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MICHIGAN'S UPPER PENINSULA SITE OF HISTORIC MINES, MASSACRE

7/3/2026

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Dim electric lights in faux lantern casings illuminate the abandoned copper mine in Michigan’s Keweenaw Peninsula.



​“Take a trip with me in 1913, to Calumet, Michigan, in the copper country,” begins a  Woody Guthrie folk ballad retelling the massacre of striking miners and their families by hired strikebreakers in the Upper Peninsula. In the backroads of memory, I could hear his son Arlo singing it. “I’ll take you to a place called Italian Hall, where the miners are having their big Christmas ball.”

“Dianne, we need to turn in here,” I said to my wife as we approached the town of Calumet. The lyrics seeped back to the surface of my memory.

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Copper once was king of the Keweenaw Peninsula, the northernmost jut of Michigan’s Upper Peninsula into Lake Superior. The copper boom began in the 1840s, although Native Americans had mined the metal 5000 years earlier in cavities still visible on the landscape.

Annual production peaked in 1916, with nearly 270 million pounds of copper mined from the region. A slow decline set in after that, and by the 1960s most of the Keweenaw Peninsula copper mines had closed. Left behind were crumbled economies and a decreased population. Thus began the region’s gradual shift to tourism.

We engaged in some of the tourist activities. We sought out lofty views of Lake Superior. We had our pictures taken at the Keweenaw Snow Gauge, where our five-foot-something bodies were dwarfed by the average annual snowfall mark of 20 feet and the record high of 32. We visited shops in Copper Harbor, the peninsula’s northernmost town, established in 1843 as the copper industry took hold.
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But then we went deeper. Literally, fascinated by the copper mining history, we pulled in at the long-defunct 1847-established Delaware Copper Mine for a self-guided tour.

After viewing a brief, explanatory film and donning hard hats, Dianne and I descended a 110-foot stairway into the uppermost level of the abandoned mine. Alongside the stairway ran old rusted rails that once hoisted copper and waste rock up to daylight.

Seepage from recent rains glistened, dripped, and trickled into the descending shaft, then disappeared into dark passageways. Electric lights encased in faux lanterns lit the lateral vein, but they were soft, subdued, and spread far apart along the passageway, giving off a light as wan and copper-colored as the hard-sought ore. They offered just enough light to peer into subterranean rooms and into cross-cut passageways.

Shaft entrances leading to the lower levels were barely visible in the shadows. They were topped with pools of water seepage that had filled the ten lower veins—the deepest descending 1400 feet—in the century-plus since the mine’s 1887 closure.

In 2012, scuba divers explored the flooded lower levels of the Delaware Mine. Their YouTube video shows old rails, support timbers, abandoned buckets, ore carts, ladders, and tons of rubble submerged in the passageway waters.

The mine’s temperature was a constant 43 degrees Fahrenheit. Encrusted patches of white fungi grew on wooden gates, stairways, and support timbers, the result of the damp air. Pieces of discarded rail and mining equipment lay along the passage, including a long, hand-cranked drill used for boring into the rock.

Signs along the passage explained mining procedures and work hazards. Dianne digested the information and moved along the passage more quickly than I. She eventually disappeared from view.
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I was alone, then, 110 feet below ground, breathing a dark, musty air. Mildewed timbers propped up the rock ceiling above me, and water-soaked beams in the submerged chambers below held up the floor. I was haunted by the past. The silence was as profound as any I’ve ever known.

Eventually Dianne and I reunited, retraced our steps through the passage, and climbed the exit stairway back into the summer light. When we resurfaced, we passed the roofless ruins of the mining company buildings. Tall white-trunked birches growing within the abandoned structures had long since softened the memory of the brutal industry.

                                                            *                      *                      *
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Ninety-one companies tried their hand at copper mining in the Keweenaw Peninsula, most of them unsuccessful. Worker pay was often tied to the mines’ profitability, and thus wages were typically low. The work was dangerous. An estimated 2000 workers lost their lives in various Keweenaw mines in a little more than a century.

Labor strikes rocked the copper mines across the decades. Meanwhile, in 1910 mine owners introduced a lightweight drill that could be operated by one man, not two. The loss of two-man teams not only cost mining jobs but further imperiled worker safety, as a pair could no longer watch out for each other.

By summer 1913, Keweenaw miners had had enough and went on strike at the nearby Calumet mine.

The strike dragged on through the fall and winter. Violence broke out immediately. The mine owners hired strike-breakers who shot and killed two striking miners. Refusing to negotiate with the strikers’ union, the owners hired “scabs” to reopen the mines.

By Christmas, the strike was in its fifth month, and miners were running out of resources. To raise spirits, the miners’ wives organized a Christmas Eve party for the strikers and their families in the upper floor of Italian Hall, a local gathering space that had been built by and for immigrant miners.

While children received Christmas presents upstairs, someone outside the hall yelled “Fire!” A panic ensued, with parents and children dashing down the stairs to the door, which was barricaded by strike-breakers and hired thugs. Seventy-three persons—more than half of them children—were smothered on the stairs. No one was ever arrested.

                                                            *                      *                      *
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Dianne and I drove the streets of Calumet, looking for the site. 

Finally we found it. Although Italian Hall had long ago been razed, the door’s fateful archway had been preserved. Behind it, visible through the doorway, sat a granite monument emblazoned with names and ages of the seventy-three victims. The youngest had been Rafael Lesar, age 2.
The Calumet mine finally closed in 1968.
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“See what your greed for money has done,” the Woody Guthrie song concludes.
 
More information about the Keweenaw Peninsula can be found in Kevin Koch’s book, “Midwest Bedrock: The Search for Nature’s Soul in America’s Heartland.”
 
-- July 2026
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The Delaware Copper Mine self-guided tour begins with a stairway descending 110 feet into the mine.
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An encrusted gate blocks off a side vein of the copper mine.
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Ruins of the copper mine buildings are now softened by the white birch growing within their foundations.
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Rail carts with boxes attached to their frames were used to bring copper and waste rock up to the surface.
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THEODORE ROOSEVELT NATIONAL PARK - NORTH DAKOTA

5/5/2026

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Banded layers in the buttes expose geological stories in Theodore Roosevelt National Park.
The old bull eyed us suspiciously from his perch on the hillside. While the other bison slowly grazed across the meadow at Theodore Roosevelt National Park, he alone squared off to stare at us parked on the roadway snapping photos. “You got a problem?” he seemed to challenge.

Not us, we might have responded. But, indeed, Teddy Roosevelt did have a problem in 1884 when he arrived for his second visit to the North Dakota Badlands that would later bear his name as a national park.

On Valentine’s Day earlier that year, both his mother and his wife died within hours of each other — the latter in childbirth — in their shared New York home. The fledgling New York State Assembly politician was devastated, writing, “The light has gone out of my life.” He had vacationed in the Dakota Territories the prior year to hunt bison and establish a cattle ranch, but he returned in 1884 to heal his soul.

Theodore Roosevelt National Park, or TRNP, occupying 110 square miles of the vast 1,500 square miles of North Dakota Badlands, is the perfect place to delve into silent, healing reflection, whether by oneself or with like-minded souls. Unlike many national parks, TRNP isn’t overwhelmed by visitors. My wife Dianne and I could disappear by ourselves onto trails, gaze alone from overlooks or contemplate in silence the layered, down-cut canyons of the park. And the visitors we encountered were often lost in their own thoughts and observations as well.

The Missouri River divides North Dakota more than geographically. To the east, enough rainfall makes the flatlands farmable. It has a Midwest personality. West of the Missouri River, the precipitation, topography and culture transforms.

Here the West begins. The dry climate lends itself to ranching instead of farming. The land begins to dimple. Hilltops begin distancing from their valleys.

But unlike the mountains further west that thrust upward from the grasslands, here the slopes drop down from the prevailing plain instead. Behind you the prairies race off to the horizon, while in front of you the bottom falls out and the earth tumbles hundreds of feet into the Little Missouri watershed.

By the time we stopped at Painted Canyon Visitors Center on the eastern edge of Theodore 
Roosevelt National Park last summer, the earth had opened up and swallowed itself.

Occasional buttes and fingerling ridges still resisted erosion, but for the most part our hike there descended into the hot, dry remains of what once had been buried bedrock.

The exposed downcut bedrock displays colorful, banded rock formations, each layer silently speaking its story. Grey siltstones at the base hail from a muddy sea bottom 70 million years ago. Yellow sandstones formed from outwash when the Rocky Mountains began rising to the west. A thin, black band of lignite coal resulted from the compression of plant matter during an epoch of lush, swampy forests. Since then, occasional lightning strikes at exposed faces have set the coal layer burning and smoldering in underground veins, partially melting another sandstone layer above it, turning it into a brittle, burnt-orange rock layer called Clinker.

And the gray crumbly clayish rock near the surface, called Bentonite, was formed from volcanic ash wafting in from western volcanoes. Even today, heavy rains can cause the surface Bentonite to gel and slump down the inclines, creating long, gray beards across some of the cliff faces.

Wind and water have provided the final touch, sculpting the top layers into steep-sided, flat-topped buttes and capped pillars spookily called “hoodoos.”

Other curiosities include petrified wood from cypress forests buried in the volcanic ash and “cannonballs” formed when water seeped into spherical rock cavities, leaving behind mineral deposits until the cavities filled. The spherical concretions range in size from bowling balls to wrecking balls. Some lie scattered about the ground, eroded out from their places of formation. Some are still half-lodged in the bedrock cliff faces. And, quite likely, some remain hidden deep inside the bedrock waiting to be birthed sometime in the next million years.

On the Scenic Drive loop through the park’s South Unit, we frequently stopped for short hikes out to overlooks where the grasslands plummeted away to the Little Missouri, to hill tops where we scrambled amid the wind- and rain-swept hoodoos that poked up from the bedrock surface like giant toadstools, and to watch prairie dogs playing whack-a-mole from their interconnected, underground villages. A row of cars precariously parked along the roadside alerted us to wild horses sheltering in a valley.

Long before it became fully established as a national park in 1978, the remoteness of these hills soothed Teddy Roosevelt’s personal pain and helped him heal. His primitive ranch cabin, now relocated to the South Unit Visitor Center, features a simple writing desk where he confronted the curative tonic that “the farther one gets into the wilderness, the greater is the attraction of its lonely freedom.” Thus healed in the quiet badlands, Roosevelt ironically became a leader known for his bombast.

The transformative power of nature later led Roosevelt to become the “conservation President” who protected nearly 230 million acres of public land, including 150 national forests and five national parks, during his 1901-1909 administration.

The Park Service guide told us that the valley vegetation was greener than usual during our summer visit due to recent rains. But to Midwestern eyes the grasses and trees were still paler than our own Iowa cropland and forest greens. Colors at Theodore Roosevelt National Park burst, instead, from the silent rock formations.

But there was enough of everything for the Badlands’ needs. The wild horses could saunter down to the Little Missouri River to slake their thirst. Prairie dogs kept cool in their tunnels. Bison, chewing on the just-enough grasses, glided their hulks effortlessly across the prairie. Just enough loneliness to heal loneliness.

It’s mostly the wind that speaks out here.

And one bison, stopped stoically in place, staring at us, telling us, “Put away your camera. Listen.”

-- May 2026

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Capped pillars called "hoodoos" add to the mysterious landscape of Theodore Roosevelt National Park.
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Two bison stare down the author.
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In 1884, Teddy Roosevelt lived in this now-reconstructed cabin in the North Dakota Badlands while healing from the deaths of his wife and mother.
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Wild horses gather in a draw at Theodore Roosevelt National Park.
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THE CHERRY TREES

4/6/2026

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The young tree’s bark looked like it had been blasted by shrapnel. After it had survived a few winters, I had thought the tree tough enough to withstand the gnawing of our backyard critters—usually rabbits—so I’d removed its protective trunk covering. And now here it was, its bark shredded, tattered, peeled.

If I’d had a backyard surveillance camera, no doubt it would have sighted a much larger critter—probably a deer buck having wandered in from the nearby woods—scraping its velvety antlers across the newly-exposed bark of my young cherry tree, third in its line of succession.
For how long do we protect those we love? When do we tell them they’re on their own? And when do we know they’re gone?

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An old cherry tree stood in our front yard when my wife and I moved into our house thirty-six years ago. It would bloom a brilliant white each spring, and then by July ruby red cherries magically lit it up like a midsummer Christmas tree.

The recipe for preparing them was simple: there was none. I might surrender a bag or two for a cherry pie or a fruit bread, but for the most part, the menu was simply tart cherries pitted and piled atop a bowl of cereal or ice cream, or stolen directly from the tree each time I passed beneath its branches while mowing the lawn.

I would freeze at least twelve bags of pitted cherries, pulling one out on the first of each month to enjoy them year-round.

Our oldest son loved to climb into its branches and sit there for hours. “What are you doing when you’re in the tree?” my wife would ask him. “Just thinking,” he’d say. What better response need there be? Although they didn’t like the tart cherries, all three of our kids as well as my wife would help me pick them. For a while. Then the task was mine to finish off.

Within a few years of our moving in, the tree began dying. Skeletal branches claimed more of the tree each year. So we planted a second front-yard cherry tree, tart of course, and watched it grow as the old tree slipped further toward death. We cheered the new tree’s first two cherries, then a handful the following season. Meanwhile the old tree finally died. It had not been a tree of our own planting, so I was not overly pained at cutting it down. But how do you explain this to your son, for whom the tree was his place to think?
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The new tree grew quickly and soon took on almost legendary status in the neighborhood. For two weeks each summer, I’d climb the step ladder, straining to reach every last cherry.  I picked cherries for several of our elderly neighbors and invited friends to share in the harvest. We live on a popular pedestrian avenue, so friends and strangers would walk, run, or bicycle past and see me on the ladder amid the cherries. It was a conversation-starter, followed by an invitation for the passerby to pick and eat a few—with fair warning as to their tartness.

The tree kept growing and producing more cherries. Finally, I gave in and declared that the cherries at its crown—which I could no longer safely reach—were literally “for the birds.”
The kids kept growing, too. They went to high school, they went to college, they went off to their separate lives. I kept picking cherries every summer.

Then the “new” cherry tree began aging. Bits of bark loosened from the trunk. Sap stained the lower trunk from some invisible wounds. One summer it hardly produced. Was it destined to be cut down as well?

Let’s wait and see, I told my wife. The first cherry tree had come with the property; this one we’d planted ourselves, and I’d invested three decades into its fruit. We consulted an arborist and tried this and that for a while but eventually decided to leave it to its own.
Just how long can you hold onto a tree? Just when does one let go?

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A tree for which you’ve invested your sweat also serves as a marker of time. In the years since we planted that second cherry tree, I’ve had much to celebrate: wedding anniversaries, kids’ graduations, books published. But I have also lost my mother, my father-in-law, a sister, and—just last spring—a brother to death. Three of the neighbors to whom I gave cherries have passed away, one during the most recent cherry-picking season. A fourth neighbor hangs precariously on to life.

Our kids are grown, healthy, and doing fine—grafted, matured, and transplanted into their current lives. But as each one left home they left a hole behind, not unlike the empty space where the first tree once stood. I would like to freeze the joys and successes of their childhood years, and thaw just one memory once each month to re-celebrate throughout the year. But there were also worries, tears, and shredded dreams in those young years. Just the usual stuff of youth,—schoolyard problems, a spurned friendship, loss of a first girlfriend, the kind of things that bruise the heart, first of the child and then—probably more deeply—that of the parent. And their menu of present-day, young adult worries—again no different or greater than anyone else’s—remain my wife’s and my worries as well. If only we could call the arborist.

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The front-yard cherry tree, the one we planted but had begun to age, has rebounded and has had at least two banner seasons since we first began to worry about its health. Passersby on the street still comment on its abundance.

Still, when we first discovered the old tree weeping sap and shedding bark, we planted that new, third, cherry tree in the back yard just in case. I cheered its first two cherries in its second year of growth. Our hope was that it would reach maturity by the time the old tree finally gave out.

When I discovered that morning that some young buck (caught in our imaginary surveillance camera) had gored it, had made shrapnel out of its bark, had almost completely girdled it, we consulted the arborist again. Again he said to treat it and wait to see what happens.

We expected it to die, leaving us with one old cherry tree up front, that one, too, perhaps on its way out. But buds formed on the tattered young tree this past spring, followed by brilliant white flowers, and then the green nubs and red fruit of cherries.

Maybe the cuts hadn’t gone too deep and the tree has healed itself. Maybe its future is nonetheless compromised, strained, and its years will be cut short.

But it’s alive right now, and so is the old tree up front. And in this season of harvest and loss, that is something to celebrate.  
 
 
--- “The Cherry Trees” appeared in 3 Elements in their Fall 2025 issue. 
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FRANK'S HILL MOUNDS, MUSCODA, Wi

3/7/2026

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A birds-eye view of the Frank’s Hill Native American mounds near Muscoda, WI. (Photo provided by Three Eagles Foundation.)

“They’re not random,” Ho-Chunk Elite Elder Ritchie Brown said of the effigy and conical mounds at Frank’s Hill and along the Wisconsin River near Muscoda, WI. “There’s a pattern telling us a story, and we’re still trying to figure out what the story is.”

My wife Dianne and I joined with about thirty other seekers at Frank’s Hill on the Winter Solstice, having trudged up the snowy path from Highway 193. We stopped briefly at the bonfire at the base of the mounds to learn more about Frank’s Hill before pilgrimaging further up to the effigy mounds at the peak to watch the sunset. At the top, we milled about, circling the mounds, and engaging in short clips of conversation while others trained their cameras on the path of the setting sun.

Frank’s Hill actually spans two hills in the bluffs a mile inland from the Wisconsin River. Hill West is home to twelve slightly arcing “calendar earthworks” that trace sunrise locations from May to August. Hill East, where we and the other observers were watching the sun descend beyond the river, preserves five mounds thought to represent a coyote, bison, bird woman, beaver and coiled snake.

Frank’s Hill is named for its previous owner, Frank Shadewald, who died in 2013 and established the Three Eagles Foundation to preserve and maintain the mounds in perpetuity.

But Frank’s Hill doesn’t exist in isolation. Shadewald had previously helped preserve sixteen mounds along the Wisconsin River when he and his neighbors sold mound-bearing properties to the Ho-Chunk Nation, who claim descendancy from the mound builders.   

A 19th century survey map shows at least 150 mounds, including forty-some bird effigies, once existing along a two-mile river stretch and 1½ miles inland and encompassing Frank’s Hill. Most of the mounds were eventually destroyed by modern agriculture. One of the surviving valley mounds is the “Ghost Eagle” with a 1300-foot wingspan, one of the world’s largest. The mounds derive from the Late Woodland Period of indigenous history, having probably been constructed between 750 and 1050 C.E. in this area, explains Three Eagles Foundation President Mark Cupp. The preponderance of mounds suggests that a large indigenous community once prospered along the river.

After the sale of his riverfront property, Shadewald next took note of the inland mounds on what would later become known as Frank’s Hill. The hill site with its miles-wide vistas had attracted the interest of a housing developer. While the mounds themselves would have been protected by state law, a residential development at their base would have compromised the character of the mound group and perhaps cut off public access, says Cupp. With the funds derived from the sale of his farm, Shadewald stepped in to purchase the entire site.

When Frank died, he gifted Frank’s Hill and an endowment for its upkeep to Three Eagles Foundation.  “I’ve tried to continue with Frank’s vision, not only to preserve the land, but to keep it open to people from all walks of life, to the Ho-Chunk and to others,” says Cupp.

The Frank’s Hill mounds often elicit deeply spiritual responses from those who walk its grounds. The mounds have drawn attention of people throughout the western hemisphere. Three Eagles Board member Brian McGraw recalls indigenous visitors who observed a ceremony at Frank’s Hill simultaneous to the same rite being performed 4000 miles away in Peru. The participants noted that “there’s a definite spiritual energy” at Frank’s Hill, McGraw explains.

Non-indigenous visitors have commented on the mystical nature of the mounds as well. And while McGraw concedes that he himself hasn’t been privy to that same experience, “I’m not going to reject something just because I can’t understand it. That’s the attitude that Frank had, being open to everyone of all faiths, creeds, and backgrounds so that people can experience the mounds at whatever level.”

One of the biggest mysteries is what the mounds “mean,” what “story” they tell. The birdwoman mound is perhaps the most evocative on the hill. The birdwoman appears to be giving birth to the sun, with the effigy and its offspring aligned to the rising sun on the spring and fall equinoxes.

Cupp remains open to such mysteries. “The mounds are not only telling a story on the landscape—one that we don’t fully understand—but there’s also a spiritual component as long as you keep your heart and mind open.”

Ritchie Brown concurs. He had helped broker Shadewald’s and his neighbors’ sale of riverfront mounds to the Ho-Chunk and continued his close relationship on through Shadewald’s acquisition of Frank’s Hill. Over the years, Brown had come to know these mounds intimately. Brown notes, “I’m told that if you really want to connect with the mounds, take off your shoes and socks and touch it with your bare feet,” then adds with a chuckle that it’s probably best not to do so on the winter solstice!
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Gatherings at Frank’s Hill are regular occurrences on the solstice and equinox sunsets. On this particular winter solstice, the prairie-topped mounds were bathed in pink and rose-colored hues as the sun descended. But then the sun cut its magic short, disappearing into a bank of clouds just before reaching the horizon. Not everything is revealed at once.

But down at the base of the mound another sun—the bonfire—was growing in intensity as Foundation members fed its flames. We pilgrims descended Frank’s Hill to gather at the fire and listen to Elite Elder Brown speak of the long Ho-Chunk association with the land and the sacred nature of the mounds. Later, by phone, Brown observed, “There are still spirits here. You can make that connection if you just stop and be still.”

Eventually the fire burnt down and the cold closed in. We seekers trudged carefully back down the hillside in the dark toward our cars parked along the highway, guided only by small flashlights, our phones’ illumination, and a bit of the evening’s flame that we each carried away inside. 

 -- March 2026
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View of southwest Wisconsin from Frank’s Hill on the Winter Solstice. Additional mound groups and the Wisconsin River lie in the distance.
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In the spring, the Three Eagles Foundation oversees a prescribed burn on the mound effigies to keep their native grasses healthy.
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Gateway to the Frank’s Hill effigy mounds.
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Summer-time bird's-eye view of Frank's Hill Mounds. (Photo provided by Three Eagles Foundation.)
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BIG SKY RESERVE, NORTHWEST ILLINOIS

12/19/2025

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Prairie and hardwood forests share the landscape at the Valley of Eden section of the Big Sky Nature Reserve.
Austin Wachter and Ben Steffes paused with me at a roadside vista that announced itself with a young oak just beginning to flex its branches in the shortgrass prairie at the Big Sky Nature Reserve. The view then swept away to the tallgrass prairie in the distance before hurrying beyond to the forest rimming the horizon. Since the land had once been cultivated, I wondered how much of the present foliage had filled in on its own versus being restored habitat.

 “We embrace what nature wants to be here, and then help it along its way,” Ben offered, concisely explaining land management at Big Sky, where he and Austin serve as co-Directors. 

Big Sky is a 900-acre Jo Daviess Conservation Foundation (JDCF) reserve located 7½ miles southeast of Elizabeth, IL, one of nine owned by or co-partnered with the Foundation. Philanthropist and conservationist Nancy Hamill Winter donated the land to JDCF in two stages, in 2016 and 2022, respectively. The two adjoining parcels still bear separate names—Valley of Eden and Home Farm—but together they constitute, and create, Big Sky.
                                         * * *
 Fall colors were just about to pop when Austin and Ben met me with a pickup truck at the Big Sky Nature Reserve to show me about the property. “We’re here to give the VIP tour,” Ben joked, practicing what they’d say if the truck encountered hikers on the trail.

The truck bounced first along the trail at the Valley of Eden, an internationally recognized Important Bird Area (IBA). Its shortgrass prairie offers spring nesting sites for Henslow’s sparrows and bobolinks, two ecologically threatened species that hatch and rear their young in the grass from April through July. In all, the Reserve harbors 120 bird species, including several Illinois Species of Concern.

The trails wind through tallgrass prairie as well. By October, the wildflowers had given up their show colors, but back in mid-summer my wife Dianne and I had hiked among purple coneflowers, yellow compass plants, and big bluestem grass waving in the wind above eye level. That day we had also climbed onto a viewing platform at the crest of the prairie and wondered whether its star-gazing function was better suited for the night-time sky or for the galaxy of yellow and purple flowers spread out beneath us in every direction.

The Valley of Eden is also graced with a hardwood savanna where, over the past six years, Austin and Ben have been removing invasive scrub trees to re-expose 150- to 200-year-old native oaks. When we exited the truck for a short walk, we encountered two JDCF volunteers whose recent work had focused on the savanna, “giving the oaks some room to breathe,” they said. This day they were enjoying a hike amid their handiwork.

 The Valley of Eden name derives from the Eden family who had farmed there for generations and who still rent three parcels from JDCF, rotating cattle among the sites to avoid upsetting grassland birds’ spring nesting. Ben explained that a Chicago Field Museum study at the site found that the cattle manure enhances the insect population, which in turn provides food for the birds, showing that agriculture and conservation can co-exist. 

The truck then bounced over to Home Farm with its generally hillier terrain. This section is so-named because Winter had lived on the property for 25 years prior to donating it. 

After driving down a long lane and exiting the truck, Austin and Ben invited me to climb the three steps of a concrete stair stoop at the edge of the parking lot where the view put me just above eye level of the windswept prairie. The stoop had indeed once been a house’s cement entryway, but Winter had placed it here years ago to use as a horse-mount. An award-winning equestrian, Winter raised horses at Home Farm and rode the trails with friends.

JDCF honors the equestrian past by designating certain trails for horseback riding from late summer through mid-autumn, when the paths are usually dry enough to withstand the impact of hooves and the grass-nesting birds have moved on.

Dogs are allowed on the trails from October through February, likewise when grassland birds are no longer nesting. In winter, fifteen miles of hiking trails are groomed for cross-country skiing. Recreational users sometimes aid conservationists, such as when skiers have identified short-eared owls that otherwise had gone unnoticed. “I think we ended up with a well-thought-out program for wider uses co-existing with conservation,” says JDCF Executive Director Steve Barg.
 
Visitors to Big Sky can choose among four parking areas, each offering easy hiking access to different habitat types, such as woodlands, prairies, and wetlands. “There are almost always people out on the trails,” Austin said, but with the Reserve’s various entry points, “you may well not encounter anyone at your chosen spot.” 

“In May and June you can hear the grassland birds. In July the prairie flowers start blooming,” Ben added. “Every season has its own attraction.”

By noon, Austin and Ben dropped me off at my car, having enjoyed, I think, the diversion as much as I had enjoyed the tour. Now they’d get back to their work on the Reserve, which, depending on the season and the day, consists of aiding oak regeneration, removing invasive species, maintaining infrastructure, mowing trails, conducting occasional prescribed prairie burns, and more.

 “Working out here, every day is different,” Austin said. But every day’s task was directed to helping nature along its way. 
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-- December 2025
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Indian Grass paints the horizon at Big Sky Nature Reserve in northwest Illinois.
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Sky blue aster peeks through pasture grasses.
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Three enclosed cattle pastures, used in seasonal rotation, provide additional bird habitat at Big Sky Nature Reserve.
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Sunflowers speckle the prairie like day-time stars.
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MAA PII PRESERVE, NORTHWEST ILLINOIS

10/27/2025

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A restored prairie graces the former farm fields of the Mąą Pįį Preserve in Northwest Illinois.
      “It is good to come to this land and hear drums again,” said Jon Greendeer, President of the Ho-Chunk Nation. Greendeer was referring to the late September “Green Corn Dance” led by members of the Ho-Chunk nation at the Mąą Pįį Preserve in Northwest Illinois.
      Mąą Pįį, or “Good Earth,” is a 361-acre refuge located two miles southwest of Galena. Owned by the Jo Daviess Conservation Foundation (JDCF) and co-managed with the Ho-Chunk and Sac and Fox, the property attests to two strands of local and regional history. The refuge preserves the 1885 John Hess farmhouse and the Hess pioneer legacy dating to 1855. But it simultaneously pays tribute to the deep Native American past embodied by dozens of 1,000-year-old burial mounds. The Ho-Chunk Nation is generally recognized as direct descendants of the Driftless Area mound builders, and the Sac and Fox (Sauk & Meskwaki) resided in the region until the aftermath of the Black Hawk War in 1832, when they were forcibly removed.
     The Green Corn Dance brought together the cultural descendants of the pioneer past with descendants of the indigenous inhabitants of the land. The festive day included guided field trips to the mounds, a naming ceremony for the refuge, and the Green Corn Dance itself. About 120 invited attendees participated: members of the Ho-Chunk and Sac and Fox nations, JDCF staff and membership community, and several neighbors of the Preserve.
     In addition to habitat preservation on its seven public preserves and two partner preserves, the JDCF mission also includes preservation of cultural and historical artifacts on those same lands. These efforts, according to JDCF Director Steve Barg, were particularly guided by former Board President Nancy Winter and local archeologist, Phillip Millhouse, PhD, in the early 2000’s. In 2010, JDCF invited former Ho-Chunk President, Chloris Lowe, Jr., to visit some of the Foundation’s preserved effigy mounds. Since then, says Barg, Lowe has donated thousands of hours helping JDCF establish a strong relationship with the Ho-Chunk, Sac and Fox of Oklahoma, Ioway, Osage, Potawatomie and other tribal nations with heritage traceable to this region.
     In the early afternoon, JDCF staff loaded interested participants into pickup trucks and UTVs to transport them through the re-established prairie to the edge of the woods where the mounds-trail begins. The walking trail leads another quarter-mile past Woodland-Period burial mounds that stretch through the forest to an overlook of the Galena and Mississippi Rivers.
     The union of water, sky, and earth in this location made this a sacred place proper for the burial mounds, according to the Ho-Chunk tradition. JDCF staff continue to work with indigenous leaders as to the proper upkeep of the mounds. Future plans include carefully removing trees from the mounds themselves to keep their roots from damaging the burial sites, and shifting the walking path to a slight remove so the trail doesn’t impinge on the sacred mound structures.
     Walking the trail alongside the mounds serves a spiritual purpose. “Our ancestors are still alive in this earth. They are on their second journey,” said Bill Quackenbush, Ho-Chunk Tribal Historic Preservation Officer. “When we pass by their burial mounds, we are not talking about them, we’re talking with them.”
     Although the preserve became a JDCF property in 2011, it just now took on the name  of Mąą Pįį Preserve with a ceremony on the day of the Green Corn Dance. The naming marked a solidification of JDCF / Ho-Chunk collaboration.
     Clayton Winneshiek, Traditional Chief of the Ho-Chunk Nation, explained, “This was once our land to roam free. There were no boundaries. Who knows how many Green Corn dances were along the Mississippi?” But he added, collaboration with JDCF and the naming of the refuge as Mąą Pįį marks a new era. “This is something I’ve never seen before, the way the JDCF has recognized our nation.”
     Bill Quackenbush noted somberly that the Indian Removal Act of 1830 had forcibly removed Ho-Chunk ancestors from their homelands. They were loaded onto steamboats and passed beneath these ancestral burial mounds on the river bluffs. “That must have been heartbreaking,” he said. “When steamboats would pull over to the shore to refuel with wood, we would be burying our dead.”
      But, Quackenbush echoed, “We’ve encountered nothing but acceptance from the JDCF.”
      Former Board President Nancy Winter, who had helped JDCF acquire the property, then spoke of the importance of acknowledging what had been done to indigenous peoples. “My Euro-American ancestors lived in this area at the time of Galena’s booming, glorious days, which was also the period of regional Indian removal. We need to acknowledge that,” she said.
      As part of the ceremony, two Ho-Chunk legislators presented Winter with a colorful Pendleton blanket in recognition of her efforts to build new relationships with the indigenous peoples of the southern Driftless region. As they placed it on her shoulders, Jon Greendeer joked, “It will be cold tonight. You might need to wear it!”
      In return, Steve Barg presented a pair of oak saplings, one to be planted on Ho-Chunk grounds and its twin on the Mąą Pįį Preserve.
     After a meal of traditional meats cooked over an open fire and contemporary potluck foods, attention turned to the Green Corn Dance itself. So-named as an early harvest feast when the stalks might still retain a hint of green, the dance was common among the Ho-Chunk. The dance, which could go on for days, called harvesters in from the fields and hunters from the woods and plains, and told stories from the ancestral past, appropriate for the Ho-Chunk, whose name means “People of the Gifted Voice.”
     As the dance got underway, Jon Greendeer explained that the Green Corn Dance had been forbidden in the era of the 19th Century boarding schools and had dropped out of the Ho-Chunk tradition. Greendeer researched the traditional dance in Library of Congress records and then sought permission of Ho-Chunk elders to resurrect it. In the past few years, Green Corn Dances have been held throughout the Midwest.
     As the evening darkened, thirteen Ho-Chunk drummers sat in the center of a circle, beating out rhythms of ancestral songs and chanting their stories. A bonfire leapt off to the side, keeping attendees warm. A traditionally-dressed man and woman initiated the dance, and Greendeer soon invited both indigenous and non-indigenous attendees to join in by following in their footsteps
  The dancers moved in clockwise fashion around the drummers. The sideways steps accompanying the forward motion mimicked the movement of tribal women who would roll corn beneath their feet to remove kernels from the cobs, Greendeer explained.
     “The closer you get to the drums, the closer you are to the earth,” Greendeer encouraged. Before long, the procession of dancers was so numerous that the beginning of the line followed closely upon the end.
     The image seemed symbolic. For the indigenous and non-indigenous participants, a circle of unity had been achieved, for this day at least. But the pioneer descendants were still learning the dance.
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[The Jo Daviess Conservation Foundation protects and preserves seven properties along with two partner-properties in Northwest Illinois. Most are open to the public. The Mąą Pįį Preserve, however, is only open to the public on special occasions.]
 
October 2025
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Traditional meats are prepared over an open fire at the Mąą Pįį Preserve.
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Indigenous and non-Indigenous celebrants join in on the Green Corn Dance.
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The 1855 John Hess farmhouse will serve as the Preserve’s Center for Science and Culture.
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Ho-Chunk Tribal Historic Preservation Officer Bill Quackenbush (left), Jo Daviess Conservation Foundation Director Steve Barg (center), and Ho-Chunk Nation President Jon Greendeer (right) celebrate the naming of the Mąą Pįį Preserve.
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INTERSTATE PARK ON THE MINNESOTA-WISCONSIN BORDER

9/5/2025

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A series of small circular holes are called “potholes,” ground into the rock when a rush of glacial meltwater spun loose rock debris in an eddying current.
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The St. Croix Dalles at Interstate Park formed when a torrent of glacial meltwater blasted through a wall of basalt bedrock.
     The larger holes might have been witches’ cauldrons ground into the bedrock, deep enough to swallow an adult. The smaller ones could be mixing bowls and the tiny ones inverted cups for sipping rainwater with a straw. 
     Interstate Park along the Minnesota-Wisconsin border is particularly known for its geological wonders called “potholes,” circular indentations in the bedrock formed 12,000 years ago when a torrent of glacial meltwater breached Glacial Lake Duluth (near Lake Superior) and rushed down the St. Croix River. At today’s Interstate Park, the deluge burst through a wall of basalt, carving a 300-foot canyon.
    On both sides of the submerged canyon, eddying whirlpools spun rounded stones as big as bowling balls and as small as marbles that downcut over 200 circular holes into the bedrock. Many are deep enough to hide your torso while others would just cover your foot, but the largest potholes measure 60 feet deep and 26 feet across. On the day we visited, some were filled with water from the recent rains, brew pots waiting to be heated. Others were as dry as bones.
                                                     *                      *                      *
    Dianne and I had come through a bit of a torrent ourselves during the previous night’s downpour at another park that had soaked through the corners of our tent, so we laid our gear out to dry at Interstate Park before setting up camp. The delay gave us time to explore and sample the park before diving into its features.
     Interstate Park is a dual park system established along the St. Croix River on the Minnesota-Wisconsin border just south of the equally dual border towns of Taylors Falls (MN) and St. Croix (WI). The smaller 300-acre Minnesota component was established in 1895 (Minnesota’s second oldest park, after Lake Itasca) and the larger 1400-acre Wisconsin tract dates back to 1900, that state’s oldest. Together, they constitute the nation’s first two-state park.
    Although the two parks are administered by each state separately (e.g., separate state park stickers are required for each park’s entrance), they are knitted together by the St. Croix River.  We took the easy river route first, buying tickets for an excursion boat on the Minnesota side. The boat expertly navigated the narrow, swift flow between the bluffs, whose waters raced as if the glacial breach had occurred just last week.
     Tuning out the tour guide, I listened instead to the story in the angular canyon walls. The gray, igneous basalt rock that the glacial torrent had burst through formed a billion years ago when North America began to split apart during its continental drift across the tropics. Molten rock upwelled into the gap like a bad case of acid reflex and then cooled in place. While the rift arcs through several midwestern states, only here in its northern reaches did it become the exposed bedrock.
     Eons later, when the glacial meltwater torrent came rushing down the St. Croix, it nosed out cracks in the basalt and blasted its way through, creating the valley, bluffs, and potholes.
    Later, we kayaked upstream to the canyon, looking for the “cross” in the basalt walls that supposedly led French explorers to give the river the French equivalent name of Sacred Cross. We briefly debated each other’s interpretation of the cross’ location (only to find out later that the river took its name from a cross-shaped island downstream). Then we gave up the quest and let the current take us downstream to where the canyon widened. Soon, the basalt walls disappeared entirely, and the river slowed to a relaxing crawl.
     The slower river told the human story. For ten thousand years, the St. Croix served Native Americans as a food source and waterway linking the Mississippi River to Lake Superior via a 20-mile northern portage. Euro-Americans arriving in the 1700s shifted the river’s focus first to fur and then to fir, decimating the beaver population for their pelts and then, after an 1837 treaty ceded the region to U.S. settlers, decimating the forests. An 1886 log jam drew media attention when it clogged the river for seven miles.
      By 1914 the logging industry had run its course, and the St. Croix River returned to an earlier, more peaceful existence. It became popular for recreation and relaxation, but modern development still threatened to turn it into just one more polluted river. Another joint Minnesota-Wisconsin effort in the 1960s saw respective Senators Walter Mondale and Gaylord Nelson successfully propose the St. Croix National Scenic Riverway. In a National Park Service video, Senator Mondale proclaimed, “The idea that we’d let these areas be despoiled offends my idea of what America’s about.”
     The Scenic Riverway now protects 255 miles of the St. Croix and its tributary, the Namekagon (Ojibwa for “place where the sturgeon spawn”) from unfettered development and pollution.
Even so, environmental threats are never far off. A proposed nickel mine near the St. Croix headwaters in northwest Wisconsin could potentially contaminate the river.
After kayaking, we returned to the bluffs. Amid the pothole formations on the Wisconsin side, near the bluff above the St. Croix River, sits the western terminus marker for the Ice Age Trail that wends 1100 miles east and south across the state, following the end moraines—the farthest edges—of the Wisconsinan glacier, another reminder of the glacial formations that shaped this landscape.
                                                         *                      *                      *
     The North American continent once nearly split in two, and then the rift healed over. A wall of glacial meltwater once roared down the St. Croix River and blasted through a plug of thick basalt, carving bewitching potholes and a beautiful gorge. The furs and the firs were once decimated, but the creation of Interstate Park and the National Scenic Riverway designation has since offered protections to the St. Croix.
      Time can heal wounds.
      Even our wet camping gear dried out, and we set up our tent.
     In the morning, the sun came out and set the St. Croix River sparkling.
 
-- ​September 2025
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The river still rushes through the St. Croix Dalles today, offering just a glimpse of the glacial meltwater torrent that created the canyon.
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An excursion boat navigates a challenging corner of the St. Croix River at St. Croix, Wisconsin.
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A larger pothole on the blufftop is deep enough to stand in.
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Over 250 miles of the St. Croix and its upstream tributary, the Namekagon, are designated as a National Scenic Riverway.
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OZARK WILDLIFE AREA, JACKSON COUNTY, IOWA

7/17/2025

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A stand of Indian paintbrush looks like prairie fire flames.
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Ohio spiderwort adorns the Ozark Wildlife Area in purple stars.
​     The prairie had been waiting for its chance to bloom again.
                                                               *                      *                      *
    Jackson County Natural Resources Ecologist Tony Vorwald and I bounce along an abandoned low-maintenance road that winds through private corn fields. The road now serves as utility access for Jackson County Conservation Board (JCCB) personnel to reach the north side of the Ozark Wildlife Area. His truck lurches between—and occasionally into—the deep graveled ruts enroute to a restored prairie-oak savanna he wants to show me.
    The Ozark Wildlife Area, located ten miles south of Bernard, IA, became a JCCB property around 1990, thanks to former owners Raymond and Azetta Clark. Partly cultivated at the time but mostly forested, the narrow, angled 300-acre Ozark property abuts both sides of a 3½-mile zigzagging stretch of the North Fork Maquoketa River. Despite its thickly-encroached woodlands, some of Ozark’s steep ravines, riverside cliffs, and rolling uplands offered the potential of being restored to a pre-settlement landscape.
     Of Jackson County’s thirty-five parks, wildlife areas, historic sites, and trails, the Ozark Wildlife Area is “definitely my favorite,” Tony says as we exit the truck at the preserve’s gate. While Jackson County Conservation has a three-pronged mission providing for recreation, education, and habitat conservation/restoration in its various holdings, “Restoration is definitely where my passion lies,” he reveals. That is part of what has drawn him to Ozark in the seven  years and two summers he’s been with JCCB.
     The crest of the first hill—once a ridge-top cultivated field—was replanted as prairie shortly after acquisition and before Tony’s arrival. Prairie flowers take turns blooming throughout the growing season, and today Ohio spiderworts are adorning the prairie grasses with purple stars.
     Downhill from the summit, a swell of red-orange Indian paintbrush in the distance looks as if a smokeless prairie fire has ignited the plant tips. Up close, the forbs appear aptly named, as if their stems had been dipped in fire-colored paint and splashed across the hillside.
    Some of the paintbrush tips are capped with see-through, cottony bags tied with drawstrings, like tiny bonnets. Tony empties a few of the bags into a pouch he’s carrying and then ties a few more bags to the flower tips. He is collecting seedheads of the paintbrush flowers to share with fellow naturalists at the Tallgrass Prairie Center at the University of Northern Iowa, as well as gathering seed to spread on other JCCB prairies.
     Further down the narrow descending ridge, we encounter old oaks that had once been sentinels of this prairie. They had flourished when the hillside was a savanna, a prairie punctuated by occasional hardwoods. Fire-resistant oaks would survive the recurrent prairie fires that consumed lesser trees. “You can tell from their outstretched, lateral branches that some of these oaks grew when there were few other trees around,” Tony explains.
      Euro-American settlement, however, squelched prairie fires, and within a few decades the oaks were swallowed up in a tangle of intruding softwood species. And since oaks require some open canopy to regenerate, the aging giants were in danger of dying out altogether.
      Thanks to a variety of grants, the Friends of Jackson County Conservation, JCCB resources, and a ton of labor and elbow grease, about three years ago Tony led a crew of workers in “knocking the forest back to the oaks,” to the line of ancient sentinels. And true to form, with sunlight once again warming the open grasses at the foot of the trees, a nursery of baby oaks has sprung up, each vying to replace the old ones nearing the end of their lifespans.
     Near the oaks, we swing uphill again, this time onto rockier ground along the 60-foot river bluff. Due to the property’s remote ruggedness, few trails are maintained at Ozark, so we pick routes of least resistance, following deer paths and edging around outcrops where the soil is too thin to support plant growth.
    Here Tony shifts from prairie tour guide to conservationist checking up on a roster of species. The cliff hillside, with broken bits of protruding limestone bedrock, is home to rattlesnakes, and Tony wants to check if any of them are home. He pokes his hiking stick under the layered and sometimes loose limestone slabs (“You there, snake?”), but on this cool morning they’ve apparently retreated further into their dens.
     Tony examines and photographs a small stand of five-petaled prairie phlox. Abundant elsewhere on the property, it’s the first he’s found on this hillside, and he’s curious why it has taken root here. He gathers seed from wood betony, a yellow-flowered hemi-parasitic plant that powers itself from its own chlorophyll but taps into its neighbors’ roots for sustenance.
     While Tony is off looking for snakes and gathering seeds, I am perched on the cliff face, sizing up the river below for kayaking and watching turkey vultures circle overhead.
     But it is when we re-emerge from the cliff-side slope that we encounter the remnant prairie re-emerging from its long sleep. The lower half of this hillside prairie had never been tilled but had been swallowed by softwood tree encroachment over the decades. The prairie slipped into a long dormant sleep until Tony and his crew began “knocking back the forest.”
     Shorn of trees and the resultant near-constant shade and leaf litter, sun-warmed on this south-facing slope, and prodded by occasional prescribed prairie burns, the prairie plants reawakened, “began to express themselves,” as Tony puts it.
     You can tell the difference between a reawakened remnant prairie and a replanted one based on the species, he explains. “Remnant indicators” are grasses and flowers that typically don’t show up in modern prairie seed mixes, so where they appear it is because they have been reawakened from the original prairie.
    Tony points out some of the remnant indicators: Panic grass seeds out like Fourth-of-July fireworks. Pale spiked lobelia flowers are tiny, white, bed-sheeted ghosts clinging to fragile stalks. And two-flowered Cynthia adds a dash of yellow to the mix.
                                                              *                      *                      *
      We have largely altered the landscape. Much of it was necessary in order to survive. Some of it was reckless. Some unintentional.
      Still, there is some comfort in knowing that, even if only on this tiny plot of land, a prairie has reawakened and bloomed again. 

-- June 2025
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Jackson County Natural Resources Ecologist Tony Vorwald
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A small number of prairie flower tips are bagged in order to collect their seed.
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Panic grass shows off seedheads like fireworks.
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SANDHILL CRANE MIGRATION ON NEBRASKA'S PLATTE RIVER

6/16/2025

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About 750,000 sandhill cranes descend along a sixty-mile stretch of the Platte River in Nebraska each March, pausing on their northward migration.
     The annual great migration had begun. Over 750,000 sandhill cranes had descended along a sixty-mile stretch of Nebraska’s Platte River for an extended refueling stop between their winter grounds in Mexico and Texas and their summer nesting grounds in northern Canada, Alaska and Siberia. And with them came the human flock, upwards of 30,000 tourists—affectionately called “craniacs”—who land each March near Kearney, NE, to watch the birds dance, strut, and fill the sky twice daily with their silhouettes and ratchety calls.
     As a pink and orange corner of the horizon gradually spread against the cobalt blue of the pre-dawn sky, Dianne and I gathered with dozens of other curiosity-seekers at a viewing deck near Kearney, watching as the cranes prepared to take flight from their overnight roosts on the Platte. Before takeoff, the sky was already filled with the sound of their gathering excitement.
     Their commingled calls sound like a mass of happy bullfrogs in a pond. Or like ratcheting flywheels. Others call it bugling, trumpeting, rattling, or like the sound of a wooden mallet scraping across a washboard musical instrument. Put all of these together and you approach the chatter of the cranes calling to their life-long mates and yearling offspring as they prepare for liftoff.
     And then they take flight even before the sun rises, first a few brave families, then a line or two of followers, and finally great flocks (called “sedges”) that blacken the sky. They rise with  couple of twists above the river before passing over our heads en route to their daytime feeding grounds. By day they’ll break out in smaller groups of a hundred or so, feasting in area farm fields on corn dropped from last year’s harvest and bugs and worms emerging from the thawing soil.
     By day, we drove the back-country lanes for close-up views of the cranes in the fields. Occasionally we’d catch a crane dancing, strutting, or coming in for a landing with legs outstretched. The gray-colored cranes in the distance, bent over while pecking for food, looked like field stones.
     At dusk, the cranes reverse the process, blackening the sky again and returning en masse to the river for the night. Night cams capture the birds huddled in the dark by the thousands, standing less than a wingspan apart, their feet draped in an inch or two of water or roosting on small islands that rise a few inches above the river.
     Sandhill cranes stand three to four feet tall with six-foot wingspans. Life-long mates will strut, jump, and dance for each other in choreographies as individualized as snowflakes. They’ll stretch their necks together in unison. Their ratchety calls, identifiable to mate and offspring, resonate from a trachea that coils like a French horn from their throat to their sternum. Youngsters join in with a higher-pitched peep. Living about 25 years and pairing up around age three, crane-mates will lead their one or two annual offspring (called “colts”) south and then back north before chasing them out on their own at the conclusion of the colts’ first year. Over a lifetime, the paired mates will teach a couple of decades’ worth of colts what to eat, how to dance, and how to fly the hourglass route.
     With their gray feathers, sandhill cranes are less colorful than some of their cousin species from across the globe, but they often “paint” themselves a rusty orange with the residue of grasses they drag across their bodies for increased camouflage and insect repellent. Their heads bear a distinctive patch of red skin they’ll enlarge to tell others to back off.
      While some sandhill cranes’ flyways lead east of the Mississippi River through Wisconsin and Indiana, 80% of sandhills use the hourglass-shaped south-to-north route that lands them on the Platte River for three to four weeks in March to regain about 20% of their weight before resuming their journey.
      The Platte River is the key. The shallow, braided Platte—often less than a foot deep—is perfect for slurping up crustaceans and sleeping one-or-two-legged in crowded broods. But the wetlands hosting the cranes were originally wider and covered a longer swath of river.  Decades of upriver irrigation have drastically reduced the Platte’s flow by 70% from pre-settlement days. Wetland drainage has narrowed the river from a twisty mile’s width to a mere 500 feet in many locations. Only 10% of original wetland meadows remain along the river. Overhunting as well as similar habitat degradation in their winter and summer grounds drove the species nearly to extinction by the 1960s.
     Since then, however, sandhill cranes have trumpeted a remarkable comeback. Restoration efforts by area environmental groups like the Crane Trust and the Audubon Society’s Rowe Sanctuary have restored portions of the Platte to more crane-friendly conditions. Sandhill cranes once again number more than a million in North America.
     Established in 1974, The Rowe Sanctuary covers and protects 3000 acres of river bottom and surrounding habitat. In one restoration approach, for example, Sanctuary personnel strip the river’s sandbars of vegetation in the off-season. Permanent vegetation raises the sandbars higher above the river, channelizing and deepening the flow and making it harder for cranes to roost in the water come the following March. Shorn of vegetation, the bald sandbars remain low to the river and provide more available roosting space.
     The Crane Trust likewise works to restore sections of the Platte to pre-settlement standards, which includes maintaining the health of bordering prairies. Bison graze the restored grasslands along the river that provide habitat to other prairie mammals and birds as well.
     Having returned to the same viewing pavilion at dusk, Dianne and I, along with the other viewers, pivoted from our morning roost locations and watched the sun set to the west. The cranes’ bullfrog ratchets, rattles, and bugles were already filling the sky. Then came the cranes again in black droves, returning from the fields, circling overhead, and scouting out their perfect landing place in or alongside the Platte to roost for another night.
 

June 2025
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Sandhill cranes, with their signature red heads, feast on invertebrates and leftover corn in area fields by day.
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The sandhill cranes regain 20% of their body weight foraging during their month-long migration layover along the Platte River.
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Cranes set down their landing gear as they move from field to field by day.
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At sunrise the cranes depart en masse from the Platte River and return at sunset.
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Ridgeway Pine Relict State Natural Area (SW Wisconsin)

3/13/2025

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Pines cling to the sandstone bluffs and outcrops at Ridgeway Pine Relict State Natural Area near Ridgeway, WI.
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Steep sandstone bluffs have protected stands of northerly pines for thousands of years at the Ridgeway Pine Relict State Natural Area. Photo contributed by Mary Kay Baum.

On a mild January morning, about ten of us gathered at a sharp curve in the road, chatting while Jared prepared tools for us to carry back along the prairie-woods divide to our work site. There were chain saws and brush saws to lug, loppers, and long-poled herbicide dabbers.

My wife Dianne and I had joined forces with the Friends of the Ridgeway (WI) Pine Relict State Natural Area, two employees of Pheasants Forever, and State Natural Areas Volunteer Coordinator Jared Urban on their monthly workday. The task today was to clear invasive shrubs and scrub trees from a hillside oak savanna remnant.  

The Ridgeway Pine Relict State Natural Area, owned and administered by the Wisconsin Department of Natural Resources (DNR), is a 546-acre tract that harbors white, red, and jack pine. Pines had once covered the Driftless region just beyond the reach of the glaciers, but as the climate slowly warmed, these pine species had crept northward along with the retreating ice.

That said, the north-facing slopes of Pine Relict provided cool micro-climates for the pines, and their location at the edge of steep sandstone cliffs had protected them against fire prior to Euro-American settlement. In modern times, the relative absence of fire has allowed the quick-growing pines to outpace the oaks at their flanks on the upland bluffs. In this way, the pines have maintained a foothold here for 12,000 years since the end of the glacial period. 

And now the forest was being further aided by its Friends. 

The Friends group Chief Steward Bob Scheidegger worked one of the brush saws, cutting and removing small scrub trees to create more breathing room for the oaks, another cherished tree species on the property. Bob’s ties to the land ran deep. He’d grown up on a farm that had included 160 acres of today’s Pine Relict. 
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“Growing up, we didn’t realize how wonderful this land was,” he mused. As a farm kid, it was a hassle to hike down the 300-foot slopes to check on cattle in the valley, “but our cousins and friends always wanted to come out here and play, so we began to realize it was something special.” They built rock dams in the valley creeks to create swimming holes and explored caves. They’d jump onto chimney-rock towers that were partially detached from 60-80-foot cliffs. 

Bob credits Mary Kay Baum—recently moved away from Ridgeway—for energizing the Friends group in its early days. With a full and active life as a former Catholic nun, a social-justice lawyer, and an ordained Lutheran minister, Mary Kay next realized that nature and rural life provided antidotes for her health. She soon discovered the Pine Relict State Natural Area and added it to her list of passions. 

Armed with a camera instead of law briefs or a Bible, Mary Kay took to photographing wildlife and flora. With typical enthusiasm, she relates how she once spent half an hour getting a just-right photo. Hiking through a nearby prairie one day, she heard a sound and turned to find a palm-sized Ornate Box Turtle crossing the path behind her. Not wishing to scare it off, she doubled back through the grasses, lay down on the prairie floor, and waited. Eventually, she used her hiking stick to swish apart the grasses, whereupon the startled turtle emerged looking straight into the camera, “cocking its head with curiosity, as humans do.” 

Mary Kay snapped the photo. 

Mary Kay brought this same “larger-than-life” enthusiasm to Pine Relict and helped convince others to join the Friends group, says Bob. “I learned about the Friends when she walked into the cheese store I was working at and began excitedly telling me about this nearby DNR property that I soon realized had been my home farm. She was looking for volunteers; she got one that day.” The Wisconsin DNR named Mary Kay the state Volunteer of the Year in 2019. 

In working with Jared and the DNR, the Friends group is keenly aware that their goal is not to develop Wisconsin’s next state park. Jared explains, “While parks are geared towards recreational development, the State Natural Area program approach is to minimize development,” protecting sensitive plant communities and providing low impact recreation such as hiking, hunting, bird watching, and fishing.

Bob adds, “We’re trying to get the place back what it was like before settlers came through. So no trails, no little bridges, no bathrooms. We’re not doing another Governor Dodge.”
                                                                                                   * * *
While the chain saws whined away on the hilltop, Dianne and I took up positions with loppers and dabbers on the prairie hillside beneath a couple of gnarly old oaks. Wiser souls knew enough to keep me away from the chain saws. Alongside us was an experienced Friends member who schooled us on which of the winter-dried plants were invasives needing to be sheared as near to the roots as possible and dabbed with a tiny touch of herbicide on their stubs and stumps. We worked from downhill to uphill, occasionally glancing backward to view the widening swath of open grassland laid out beneath the oaks. 

After a while, the chain saws fell silent on the hilltop just as we on the loppers crew connected our prairie remnant to theirs. Then Jared offered to lead us on a short hike down to one of the pine cliff overlooks. 
Descending steeply from the uplands, we arrived on a more subtle slope that had recently benefited from a prescribed burn. The uncluttered understory was punctuated with oaks on the rolling hillside until, near the cliff face, white, red and jack pines took over. The pines popped from among sandstone and dolomite rock outcrops like mushrooms. Leaning out from the cliff face, the pines directed our gaze across the valley to the next cliff top where a swath of green marked another stand of relict pine. 
​
The pines were thriving here in the relict southwest Wisconsin forest while most of their species had retreated northward. Geography had saved them against the dual onslaught of a warming climate and human settlement. 
But now the pines, along with the upland oak savannas and prairie, were also getting by with a little help from their Friends.                                                                                                                                                       -- March 2025
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Relict pine stands have survived since the last glacial age (12,000 years ago) in southwest Wisconsin while most of their species retreated northward.
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An active Friends group also helps restore and maintain prairie at the Ridgeway Pine Relict State Natural Area. Photo contributed by Mary Kay Baum.
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An Ornate Box Turtle emerges from the grasses at a southwest Wisconsin prairie. Photo contributed by Mary Kay Baum.
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Mississippi-Missouri Rivers Confluence

12/29/2024

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North America’s two largest rivers meet as the Missouri River enters the Mississippi at the Edward “Ted” and Pat Jones Confluence Point State Park near St. Louis, MO.
I am watching a six-foot log ride the Missouri River current upon entering the Mississippi at the Edward and Pat Jones Confluence State Park north of St. Louis. The log follows the Missouri’s defiant flow halfway across the conjoined river until the Mississippi catches it, spins it, and realigns its path. 

The rivers’ convergence has long appeared as a battle of wills between the two giants. In 1673, the first European observer of the rivers’ confluence, Jacques Marquette, described “an accumulation of large and entire trees, branches, and floating islands…issuing from [the Missouri], with such impetuosity that we could not without great danger risk passing through it.” 
Judging from the log bounding halfway across the Mississippi, the two rivers haven’t yet called a truce. 

Life above the water level, though, is tranquil. Confluence Point State Park, the adjacent Riverland Migratory Bird Sanctuary along the Mississippi, and several additional parks and refuges along the Mississippi and Missouri offer 30,000 acres of wetlands, woods, and prairie a stone’s throw from St. Louis and its suburbs. 

 “Over 300 bird species use the Mississippi/Missouri corridor during the fall and spring migratory seasons,” says Ken Buchholz, Director of the Audubon Center at the Riverlands Sanctuary. In the fall, their flight patterns converge at the confluence much like the rivers’ waters, and in spring they diverge at the site as they come back north, selecting their respective paths as if from among highway exits. 

Whether in migration or living year-round, so many species gather near the confluence that the Audubon society designated the region an international Important Bird Area (IBA) in 2004. Especially during migration season, the Riverlands-Confluence region “is a birding hot spot popular among enthusiasts,” Buchholz says.

Bald eagles are among Buchholz’s favorites. Among them are a growing population of year-round residents, as well as migratory eagles who come down from the north in colder winters. Other celebrated visitors include trumpeter swans, paddler and diving ducks, and Canada geese. Residents include various species of owls, raptors, and shoreline birds. “Limits on development along the river has helped to retain habitat,” Buchholz explains.

All on the northern edge of metropolitan St. Louis. 
                                                                                    * * *
When I visited the Confluence Point State Park on a late summer afternoon, I encountered both tumult and solitude. For me, however, the confluence’s commotion was more related to the packed and swift U.S. 67 expressway traffic hustling to cross both rivers. The final exit before the Mississippi quickly transitioned me from metropolitan traffic to an isolated, five-mile road on the peninsula between the two rivers where the only other car in sight belonged to a man photographing backwater egrets. 

Immediately off the exit, the pace slows. Riverlands Way Road slips along a causeway through the Alton Slough. The Audubon Center at Riverlands is the last significant building encountered on the peninsula, aside from a handful of scattered farms and a station for conservation vehicles. Riverlands Way road soon turns to gravel as it winds along the narrowing peninsula to the confluence.

When I pulled in at the Confluence Point State Park parking lot, mine was the only car in sight. Signboards near the parking area, however, tell of this lonely site’s celebrated natural and cultural history. The Mississippi and Missouri’s combined watershed incorporates 40% of the continental U.S. and a small reach of Canada, the fourth largest watershed in the world. From ancient times the confluence—along with the nearby Illinois River to the north and the Ohio River to the south—offered indigenous peoples a trade and transportation route to vast portions of the continent. 

In 1804, William Clark and the Voyage of the Discovery crossed the Mississippi into Missouri River (Meriwether Lewis would join them upriver at St. Charles) as they embarked on their commissioned odyssey to explore the Louisiana Purchase. In a letter sent back home, Clark echoed the prevailing sentiment that the Missouri presented the stronger flow: The Missouri, he wrote, “seems to dispute the preeminence [of] the Mississippi.”

A short 1/3-mile trail leads from the parking lot to the confluence itself. The first stretch is confidently laid down in cement. From there, the trailblazers seem to have acquiesced to the fickleness of the rivers’ flow as the trail transitions to dirt. Near the convergence, the trail had disappeared entirely, its exact path having been mudded over by early summer floods. 

Now, in late summer, the rivers were limping past in time of drought. “Flood pulses are changing habitat,” says Buchholz. “More frequent high water upsets a wetland complex by bringing in non-native or invasive species.” But droughts are increasing along with the floods. “We have more roller coaster years in which flooding is quickly followed by drought, with barges tied to shore waiting for the river to come back up.” 
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If there is a bright spot, it may be that the more frequent flood-drought cycle is getting the attention of St. Louis residents and business people as they are encounter the impacts of climate change.

Another bright spot lies in some increased collaboration between conservation groups and government agencies ordinarily more geared to commercial use of the rivers. The Riverlands Migratory Bird Sanctuary, for example, was paradoxically enhanced when the shoreline was slated to receive dredge material from the nearby construction of relocated Lock and Dam #26. Wildlife biologists at the Army Corps of Engineers strategically placed the fill “to re-create and enhance some of the wetland expanses that one would have seen in earlier times,” says Buchholz. 
                                                                               * * *
When I reached the confluence point, I turned in three directions: one, upstream along the Upper Mississippi; two, upstream along the Missouri; three, to the point of merger and downstream, where the conjoined rivers take the name “Mississippi,” but the Missouri keeps up the fight. 
The log, though, finally pivoted and turned downstream. 
​
-- December 2024
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A short trail runs beside the Missouri River to its meeting point with the Mississippi at Confluence State Park.
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Greater White-Fronted Geese are among the migratory waterfowl splashing down at the Riverlands Migratory Bird Sanctuary. Photo contributed by Madi Hawn.
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The Audubon Center at Riverlands near the Missouri-Mississippi Rivers confluence. Photo contributed by Madi Hawn.
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Witkowsky Wildlife Area, Northwest Illinois

11/9/2024

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• The Prairie Point Overlook gives a clear view of Northwest Illinois’ Driftless Area landscape.

     Brad Petersburg’s UTV pitched at a hang-on angle as we descended the Walnut Trail at the Witkowsky Wildlife Area. I braced myself with the roll bar until Brad stopped to chain saw a tree limb that had fallen across the trail. Then we emerged from the upper woodlands to the prairied valley floor at the 1100-acre refuge where we encountered—of all things not expected in a prairie—the concrete remains of an abandoned satellite station.
     The Witkowsky Wildlife Area is a partner property of the Jo Daviess Conservation Foundation (JDCF) in northwest Illinois. The property is owned by the Illinois Department of Natural Resources (IDNR) and maintained in part by a Witkowsky Friends group associated with JDCF. I was fortunate to tag along on a trail clearing mission with one of the Friends. Motorized vehicles are not otherwise allowed on the property.
     The long journey to becoming a wildlife area began in 1986 when Jack and Iris Witkowsky donated 400 acres to the IDNR with the stipulation that the state add more property to the refuge and develop trails open to the public. IDNR succeeded at the first task but had not progressed on the second when concerned neighbors, led by Brad Petersburg, approached JDCF in 2012 about possibly intervening. 
     JDCF is a private conservation foundation that owns seven public preserves totaling over 1,500 acres in northwest Illinois, but its mission also includes helping landowners preserve environmentally sensitive habitat through other means. Under these auspices, JDCF completed a cooperative agreement with the IDNR in 2017 by which the local Friends would develop trails and keep them cleared of fallen trees, and the state would keep them mowed. 
The refuge fully opened to the public in 2021. 
     Brad had quickly become enamored of the nearby Witkowsky Wildlife Area after relocating to the Driftless Area. “In 2006,” Brad explains, “my wife and I purchased a cabin in the woods of Jo Daviess County as a second home. A year later, when the opportunity arose to sell our farm home in north-central Iowa, we moved to Jo Daviess full-time.” The Driftless Area, they discovered, had the perfect mix of wooded hills, open fields, and rural atmosphere. But the Witkowsky property lingered in terms of becoming open to the public with usable trails.
     Brad went into high gear when the cooperative agreement was completed. He began laying out the refuge’s ten miles of trail, conferring with the IDNR to make sure the paths didn’t impinge on fragile ecosystems. “The challenge of creating a new trail system was appealing,” Brad says. “I enjoy studying the landscape, laying out and clearing trails that highlight interesting features like rock outcroppings, large trees, and big views.” Dozens of friends and neighbors helped clear the trails over several months.
     Our first stop was about halfway down the upper portion of the Walnut Trail. Brad pulled the vehicle to the side of the trail and led me along a deer path to a small clearing in the woods. Here Brad pointed to a massive tree nearly 100 feet tall that had been verified as (tied for) the second largest red oak in Illinois. Its girth would take at least four adults to encircle. However, since that designation, its largest limb had fallen in a storm, revealing a hollowed trunk. 
    Perched on the still-freshly splintered branch, Brad worried that the tree might now be in decline. Even so, he mused, “They say oaks spend 100 years growing, 100 years living, and 100 years dying.”
     Next on the trail clearing mission was the Prairie Point Overlook. Located at the end of a wooded ridge, the Point looks out over the remainder of the woods, the prairied valley floor, and a neighboring privately owned pond. A signboard explains that the hilly and varied landscape is part of the Driftless Area, the four-state region (northwest Illinois, northeast Iowa, southwest Minnesota, and southwest and central Wisconsin) that had been spared the leveling effects of the glaciers. 
     Brad pointed to a white splotch on the prairie below, nearly tucked away beneath the view from the ledge. That, he said, was the now-abandoned shell of the telecommunications “Earth Station” that had once operated in the valley. Brad left me hanging for the moment. We’d learn more, he said, when we got there. 
     After stopping a few times to clear fallen limbs from the trail and to clean the signboards, we emerged onto the valley. In the October sun, prairie flowers had already spent their royal purples and gold for the season, and the grasses had lost their green. Still, big bluestem towered over the UTV and pulsed in the persistent breeze like ocean waves. 
   Finally, we arrived at the Earth Station. Two massive concrete hulls, partially engulfed in vegetation, sprouted from the prairie floor. An information board shows a photo of the communications facility in its glory days, topped by two massive radar dishes. The Earth Station was one of seven U.S. communications sites built in the 1970s to ferry long-distance telephone calls to upper atmosphere satellites, from which they’d be bounced back to other locations. Local newspaper photos show the facility’s interior complete with massive computers and technicians sporting 1970s hairstyles. The Earth Station was decommissioned in 1986, by which time its technology had become obsolete.
   The interior works and the massive satellite dishes were removed from the two circular structures, leaving behind just the concrete shells. Brad and others have fancied how the structures might some day be used if enough money were somehow available (and with IDNR approval). “Star-gazing on the roof? Concerts inside the buildings?” he wonders. 
     My wife Dianne and I returned the following day to explore more of the Witkowsky Wildlife Area’s scenic trails. We followed the two-mile Cedar Trail as it first led across fields still leased to local farmers before dropping into a stream valley. Tall cedars outlined the start of the wooded portion of the trail, and the late afternoon sun flooded the stream bottom deciduous woods in a gold light. The ascent treated us to limestone outcroppings hidden in plain view in the woods. We drove the remaining perimeter of the refuge, saving the Oak Trail for another visit.
     The Witkowsky Wildlife Area offers a view into what the Driftless Area landscape looked like prior to Euro-American settlement. Ironically, even its “futuristic” telecommunications Earth Station ruin is a harbinger of days gone by. 

-- October 2024

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• In autumn, prairie grasses tower over the hiking paths in the Witkowsky bottomlands.
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• Only the shell remains of the prairie valley’s “Earth Station,” which once housed two massive telecommunications satellite dishes that ushered long-distance phone calls in the 1970s-80s.
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• Asters provide autumn color after most of the season’s prairie flowers have faded.
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• Asters provide autumn color after most of the season’s prairie flowers have faded.
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• Brad Petersburg stands beside Illinois’ second largest red oak at the Witkowsky Wildlife Area in northwest Illinois.
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Pipestone National Monument, Southwest Minnesota

9/20/2024

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Winnewissa Falls is a key attraction at Pipestone National Monument in Southwest Minnesota.
​     The hand-hewn quarries at Pipestone National Monument in southwest Minnesota were underwater. The day before, Dianne and I had seen the same early-summer floods hurtling through the nearby bordering corners of South Dakota and Iowa, devastating communities and destroying infrastructure. And here at Pipestone, raging waters had wiped out a trail bridge at Winnewissa Falls and had submerged the quarries.
     Pipestone is a 300-acre National Monument protecting prairie and wildlife and assuring the right of indigenous peoples to quarry soft pipestone rock as they have for at least 700 years. For centuries, peoples of the Oneota culture and its descendent nations came from throughout the Midwest to dig out the pliable, reddish rock and carve it into ceremonial pipes, effigies, and other sacred figurines.
    The Pipestone quarries were an area for peace. No fighting occurred here when the nations came together to quarry. In pre-contact times, the pipes and figurines were traded among tribes throughout North America. Petroglyphs on the site—dating back 5000 years—indicate an even earlier sense of the sacred.
     Dianne and I were visiting Pipestone after a bit of a washed-out regional trip in which a failed car transmission scuttled one set of plans and flooding on the Big Sioux and its tributaries altered the rest. We were frustrated. It wasn’t until the morning of our final campsite in South Dakota that I sensed a change in fortune. At sunrise, I hurried down a cold, dewy trail to catch the last mists of fog rolling off our camp-side creek. It seemed like a good omen.
      When we arrived at Pipestone a short while later, the recent rains were now just a memory being carried away by the receding streams, though the quarries remained inundated.
Geology and the Creator had worked wonders here. Wedged in between layers of steel-hard quartzite formed from ancient sandy sea floors lay thin seams of pipestone molded from intermittent clays. Pressurized and uplifted, the formation offered itself to indigenous peoples.
     The sixty-some active quarries on the site today are not industrial-sized, as the term might suggest. A typical quarry might be 20 feet long, a few meters wide, and a dozen feet deep. Indigenous peoples who work the small quarries even today use only hand tools. They first remove several feet of soil and glacial gravel from their small quarry sites, then painstakingly chip through six to eight feet of hard-as-nails quartzite before reaching the 11-18-inch bands of pipestone. The back-breaking toil is part of the sacred ritual.
     The reddish rock, according to the oral tradition, has been colored by the blood of the ancestors. The place felt holy.
     Strikes-the-Ree, the Ihanktonwan (Yankton) Chief credited with saving the grounds from American encroachment, explained in 1881 how tribes “approached the sacred ground. All of us followed a three-day long purification of fasting, prayers, and sacrifices, imploring the Great Spirit to expose the holy minerals buried beneath the rocks. On the fourth day, we painted ourselves and began working.”
     The area began to draw the interest of Euro-American explorers in the early 1800s. In 1836 the famed western exploration artist George Catlin visited the quarries over Native American objections. His drawings, as well as the pipestone sample he sent back to eastern geologists, put the quarries on the White map.
      Geologists named the new (to them) formation after him, calling it Catlinite, although the term “pipestone” is more frequently used today. Soon after this, Joseph Nicollet and six other explorers visited the site and literally left their mark on the landscape by carving their names and initials into a rock at the top of Winnewissa Falls, a graffiti still visible today.
     When forced treaties signed away the surrounding landscapes from local tribes, Strikes- the-Ree in 1858 negotiated to keep Pipestone available to the Yankton tribe. Encroachments on the quarry lands eventually led to a Supreme Court decision against the U.S. government for illegal seizure.
      Although the U.S. government then purchased the land from the Yankton rather than return it, some attitudes had begun to change. In 1937 Pipestone became a national monument, with guarantees that Native Americans could continue quarrying the sacred stone.
     Dianne and I often feel cast into oppositional roles of trespasser and humble learner at such sites. As is the case among most of the 80,000 annual visitors to Pipestone National Monument, this is not our holy land, nor our sacred tradition. But we respectfully observed the “Do’s and Don’ts” advice the Park Service suggests to non-indigenous visitors, beginning with “Be open to learning” and “Listen and observe more than you speak.”
     No one was quarrying during our visit due to the flooded work pits. Inside the visitor center, a local indigenous pipestone carver described to us what he was making, why, and how. He straddled two worlds as he told us about the good medicine the mallet he was shaping would bring while also explaining the geology underlying the quarry fields. A fifth-generation quarryist, he worried that no one from his family would carry on the tradition.
     Outside we listened and observed as well. The 26- acre prairie harbors over 300 native plant species and offers habitat to 100 permanent and migratory bird species. The ¾-mile trail that winds among the prairie, quarries, quartzite cliffs, and wetlands are meant to be walked quietly and slowly, to be seen and heard rather than be talked over.
     The rushing stream speeding past the washed-out footbridge, spilling over the rapids at the lip of Lake Hiawatha, and tumbling over Winnewissa Falls told us that the catastrophic rains had dissipated and were being carried away, that the drying had begun, but that there would be more waiting before the plentifulness of summer returned. Our frustrating trip had not been for nought.
      We left nothing behind at Pipestone, and, as we returned to our car and to the road back home, took with us only the assurances given by the stream.
 
- August 2024
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3. In addition to preserving sacred Native American pipestone quarries, the national monument also protects 260 acres of prairie with over 300 native plant species.
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The small hand-hewn quarries at Pipestone National Monument were underwater due to recent rains.
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An open bluff face at Pipestone National Monument displays layered bands of quartzite and pipestone.
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Hiking With Students

7/5/2024

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Fall semester students from Mississippi River Lore & Legacy enjoy an outing to the Mines of Spain river shoreline.
“Do you have a woods eye or a prairie eye?” I would ask my Loras College students after reading Bill Holm’s essay, “Horizontal Grandeur.” “Or maybe you have some other eye—a mountain eye, an ocean eye, a river eye?”

Holm’s essay extolls the virtues of Midwest prairies. Someone with a prairie eye, he writes, “looks at a square foot and sees a universe: ten or twenty flowers and grasses, heights, heads, colors, shades,” and more. The woods eyes, he writes—not better or worse, but different—looks for mystery and a sense of the baroque.

I didn’t care so much which landscape “eye” my students claimed. I cared only that they used their eyes and ears to see, hear, and be in whatever landscape they encountered. To facilitate perception, I took students out into local landscapes several times a year.
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“We’re going to climb that?,” I overheard one student ask of another as we reached the base of a steep Mines of Spain hillside. To the left rose a sheer limestone wall, probably an old quarry not far from the river and just south of the ponds. To the right there was just enough foothold that by digging into the snow with our hiking sticks and grabbing onto tree trunks, we could pull ourselves up the incline. It may have been January Term, but after climbing the slope, we were plenty warm.

We were exercising our woods eyes. Here and there in the scraggly forest stood a few majestic burr oaks, 150-170 years old. Originally an oak savanna with a prairie carpet spread out beneath the scattered oaks, this river overlook would have been clear-cut for lead smelting furnaces in the 1800s, I explained, and the oldest oaks here today took root as lead mining came to an end. These old oaks took root in the relative absence of other trees and spread their limbs horizontal and wide. As the forest regrew, the younger trees had to stretch vertically for sunlight.

But the prize of this hike was located another hill over, down a ravine, and up another hearty climb. And there in the cover of woods and far from any summer-time trail, a simple hole dimpled the earth, then another as we curved up over the lip of the hill. And then another and another until we were in the lead-mine field, among hundreds of shallow pit mines dotting the river bluff like a crater-scape, each ranging in size from six to a dozen feet wide and four to eight feet deep.

I explained Dubuque’s lead-mining past as we zig-zagged among the pits. We playfully slid down into the larger ones and clawed our way back out. Spreading out across the woods, we searched for the widest and the deepest. After reaching the end of the mine field, we paused and looked out over the ice-caked river. I asked students to walk quietly back through the woods, imagining the miners who once roamed over this river bluff and who had tossed dirt, rock, and finally lead out of these holes.

The only other footprints in these woods besides our own belonged to deer and mice.
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Alongside Catfish Creek at the Swiss Valley Nature Preserve, we tested our prairie eyes and talked about the stream restoration project completed several years earlier that had transformed the creek’s steep-walled, muddy banks into the gentle, grassy gradients that prevailed in pre-settlement times. Before the advent of quick, massive drainage associated with modern agriculture and municipalities, prairie grasses would have sidled down to the creek-side on slopes more ambling than precipitous. Occasional high waters could glide across the creek’s grassy twists and curves instead of further downcutting into the mud walls.

Sloping down from the tree line, last year’s dried prairie stubble poked through the sagging January snow as the students and I huffed upward to the hanging marsh. Located on an embankment halfway up the hill, the marsh is fed by small springs that flow practically year-round. Groundwater filters down from the crown of the bluff through the porous limestone, then 
travels vertically on a layer of shale until it emerges in rivulets on the embankment. Warmer than the surface soil in winter, the springs encourage early season wildflowers while everything around it lies frozen. The constantly wet soil keeps the trees at bay, producing a marshy opening in the woods and boosting the warming power of the sun.
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I encouraged my students to find where the spring waters emerge. Above, they noticed, there is frozen ground; below, a soil soaked and spongy.
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In May Term and Fall, we drove to the base of Lock & Dam #11 on the Wisconsin side to exercise our river eyes. Far from a natural environment here, we talked about what the wandering river might have looked like before its harnessing. We considered the environmental impact of dams creating a narrower but deeper river and how barge engines churn up the river bottom. But we also discussed the economic benefits of barges, especially their relative fuel efficiency in comparison to rail and truck transportation of goods.

We watched the river roil and boil as it exited the gates on the downstream side of the dam, and noted the smooth upper pool surface stretching lake-like as far as the eye could see.

I told students about the habitat restoration above the dam at Sunfish Lake that protects fish breeding grounds from the swift flow of the river. Students were surprised to learn that they were standing on the shore of the Upper Mississippi River National Wildlife and Fish Refuge (now celebrating its 100-year anniversary) that lines the river for 261 miles from Wabasha, MN, to Rock Island, IL.
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After each outing I asked students to write about what they’d learned, but also what they’d reflected on or seen without my pointing it out. “I think I have a woods eye,” one student wrote, noticing the sun trickling down through the canopy. “But maybe I could have a prairie eye when the wildflowers are in bloom.”

Which eye she possessed wasn’t really the point. What mattered was that she had opened her eyes.

-- June 2024



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Students brave the snow and cold temperatures for a January-Term hike at Swiss Valley.
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Loras College January-Term students discover their woods-eyes while hiking in the Mines of Spain.
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We hike among old lead mine pits dimpling the snow at the Mines of Spain.
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Students are surprised to learn that the Upper Mississippi National Wildlife and Fish Refuge extends over 200 miles along the river and its shorelines.
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Muscatine Sand Story

5/7/2024

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Wildcat Den trails lead upward into wind- and water-sculpted sandstone glens.
​        The boy and his father were tossing bits of pea gravel past the railing of an overlook platform at Wildcat Den State Park. As Dianne and I approached, the dad laughed and explained they were aiming for the hollow in a tree trunk just a few yards beyond the railing. We picked up a few sandy bits from the trail ourselves and tried our luck: it was harder than it looked!  
       What isn’t hard is finding sand and pea gravel in southeast Iowa’s Muscatine County. From the heights of Wildcat Den to river-bottom Deep Lakes Park, Muscatine is awash in the sands of time connecting the past and present.
                                                                   *          *          *
     By the multitude of lake names alone, we might have thought we were bicycling in the lake country of northern Wisconsin or Minnesota. The bike trail slid between and among Turtle Pond, Lake Ivy, Goose Pond and Lake Chester. But one name, Haul Road Pond, offered a clue that Deep Lakes Park, with its dozens of canoeable and fishable ponds, is a 435-acre recreational site salvaged from depleted sand and pea-gravel quarries. A few short decades ago, the site was crawling with end loaders and dump trucks preparing sand and gravel for road construction sites.
        Muscatine County and surrounding areas of southeast Iowa are known for their sandy soils. But the sandy, gravelly soil that today nourishes famous Muscatine melons and is quarry-mined was laid down by glacial meltwater. During the Illinoian glacial period 100,000 years ago, an ice dam formed downstream on the Mississippi River, backing up a glacial lake across parts of southeast Iowa. At the bottom of these silent and still waters, the Mississippi dropped fine sand and gravel it had been carrying down from the north. When the ice dam broke and the backwaters subsided, today’s Muscatine County was left with a deep, sandy, gravelly, outwash bottom from the ancient lake.
      At Deep Lakes, located in the river valley about half a mile inland from the Mississippi, the spent quarry pits eventually filled with rain, snowmelt, and groundwater. With some additional sculpting and shaping, Deep Lakes became a Muscatine city park in 2013. The 435-acre park includes 120 acres of pond and lake surface, some with depths up to 30 or 35 feet. Boat ramps and access paths allow for canoes, kayaks, and small motorless boats. A handful of rental cabins sit among the lakes, and Lake Chester offers a swimming beach.
       The glacial story is ever-present. Mounds of sand and fine gravel line the bike trail, which in turn connects with the Muscatine city bike trail system. Hiking paths wind among the dunes and sand prairie. Short cedars and woody bushes tolerant of this type of soil predominate. In this early spring bike ride, we stopped at the lakes’ access points and peer through the leafless branches to more distant ponds.
       I shook my head when we reached the end of the trail. At the edges of the park today, quarrying continues. “More ‘Deep Lakes’ for the future,” I joked, and then marveled at the reclamation of an industrially scarred landscape.
                                                            *                      *                      *
           In 400 feet of climb from stream base to the heights of the park, Muscatine County’s Wildcat Den tells an even older story of sand and other layers of bedrock. At base level, Pine Creek tumbles over a mill dam in the limestone bottoms. An 1848-constructed four-storied grist mill still graces the side of the dam. From the railing of an 1878 steel bridge long retired from vehicle traffic, Dianne and I admired the brown-stained, immaculately maintained mill and watched Pine Creek spill over the dam and speed away beneath the bridge. In drought, the limestone base of the creek had been laid bare at its edges, dry and exposed to sunlight for one of its rare periods in the 375 million years since the Midwest sat at the bottom of an ancient sea.
        We set off on what we intended as a short hike that turned out to be an hour and a half of climb and descent. As we ascended, a thin band of shale, 315 million years old, crumbly and containing minutes layers of coal coated the tops of the limestone outcrops.
         But farther back and higher up in the park we encountered the sandstone glens that define the park. This is an older story of sand than lay at the Mississippi bottom. At 310 million years old, these sands were laid down where ancient rivers met the sea. The twisting, turning trail led us deeper into hidden glens and shelters naturally hewn into the sandstone that must have harbored more than a few wildcats’ dens.
        The layered, swirling, multi-colored bands in the sandstone were sculpted over time by the sea bottom itself, by the pressures of uplift, by wind whistling down through the glens, and by newer waters that still pour over the upper ledges during snowmelt and after torrential rains. The Devil’s Punchbowl—dry most of the year—fills when water cascades over its lip during such events.
       Our descent offered warning of a trail closure ahead. We’d spent more time hiking than we’d allotted, so we decided to check what the enclosure entailed. A simple downed tree had fallen across the trail where it descended from the upland glens. A few over-and-under’s and a misstep or two finally brought us tripping to the base of the sandstone bluffs. Here we encountered Devil’s Lane, a narrow squeeze-way where a slump of sandstone had broken free from the ledge, and Steamboat Rock, a hundred-foot wall of sheer bedrock rising from the trail.
        When we plied at Steamboat Rock’s sandstone ledge, our fingertips came away…with particles of sand.
       And the cycle of the sand story at Muscatine started anew.

​-- May 2024

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An 1840s four-story grist mill still graces Wildcat Den State Park's bottomland.
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A retired 1870s bridge at Wildcat Den State Park now serves pedestrians and admirers of Pine Creek.
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Depleted sand and gravel quarry pits have been transformed into more than a 100 lakes and ponds at Deep Lakes Park at the edge of Muscatine, IA.
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Good Earth State Park, South Dakota

3/14/2024

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The sun sets on the Good Earth Prairie and Visitors Center in southeast South Dakota. (Photo by Angie Mulder and provided with approval of Good Earth State Park.)
      Sometimes the good earth offers a surprise landscape. For Dianne and me, an unexpected find was South Dakota’s Good Earth State Park, located about eleven miles southeast of Sioux Falls on the hilly banks of the Big Sioux River marking the boundary with northwest Iowa. We had been travelling the eastern corridor of South Dakota and were looking for a place to stop for a short picnic lunch. We found Good Earth on the map, decided to stop for a brief visit, and stayed for several hours.
       Opened in 2013, the 600-acre Good Earth is South Dakota’s newest state park. But its story of goodwill dates back much further. From 1500 to 1700 A.D., Good Earth was the site of intertribal, interconnected villages lining both banks of the river, home to six thousand residents of the Omaha, Ponca, Ioway, and Otoe nations living together in harmony and prosperity.
       On a hot July day, we first sought relief in the sleek, new Visitor Center. Far from just being a refuge from the heat, however, the Center told the amazing story of this collaborative ground.
     Good Earth had been a prosperous trade center. Its location on both sides of the Big Sioux River, about 75 river miles north of its confluence with the Missouri, gave it trade access with Native Americans across the North American continent. Artifacts found at Good Earth include obsidian from Wyoming and Idaho, chert from southeast Nebraska, and copper artworks from the Upper Peninsula, Michigan. Local artisans made bison robes and carved pipes, decorative tablets and other objects from red pipestone mined nearby, which they in turn traded across the continent.
     Although the Good Earth village existed prior to the region’s first contact with Euro-Americans, signs of change were in the air even as Good Earth thrived, as evidenced by archaeological finds. Tribal merchants began arriving with Jesuit rings and Dutch marine shell beads called “runtees,” signaling the Eastern tribes’ increasing contact with explorers, missionaries, and colonists.
       The village’s dispersal around 1700 occurred prior to extensive Euro-American presence in the South Dakota region but was influenced by eastern contact. Like dominoes, displaced tribes pressured other tribes westward until tension with the Sioux likely caused the Omaha, Ponca, Ioway, and the Otoe to abandon Good Earth. The Ioway moved south along the Missouri River in Iowa and Missouri, the Otoe to the Platte River in Nebraska, the Omaha and Ponca to southeast and northern Nebraska, respectively. 
       But the story of Good Earth was never fully forgotten. Even early Euro-American settlers knew that something out of the ordinary had taken place here. Archaeologists drawn to the site on both sides of the river discovered 76 imprints of family and community wooden lodges ranging from 12 feet to 123 feet long. Stone circles, geoglyphs (mythical images carved into the ground) and hammer-pitted boulders, along with pottery and trade artifacts, were eventually unearthed at the site. Stone mauls, hide-scrapers made from deer antlers, and clay pots tempered with ground-up shells were among the food-preparation utensils discovered.
       Dozens of burial mounds were likewise identified. A great serpent mound, 1/8 of a mile long, is believed to have existed at the site, but was largely obliterated by an 1800s railroad line and local agricultural plowing.
       By 1970 enough modern interest had gathered around the site that it was declared the Blood Run National Historic Landmark, Blood Run being the name of a creek on the Iowa side of the village, named for the red tint its waters picked up from iron oxide during heavy rainfalls.
       But officials sought a different name as the South Dakota site moved toward becoming a state park. Park Manager Jim Henning explains there was a concern that “‘Blood Run’ would have a negative connotation, as if something bad had happened here,” when in fact the story to be told was immensely positive. Conversations with the four descendent nations coalesced around “Good Earth,” although that was probably not its literal name.
      Good Earth park personnel continue to collaborate with the Omaha, Ponca, Ioway, and Otoe nations. “We meet with them twice a year to talk about plans for the park, and to get their feedback and help on planning our programs. If we want to build a deck or even when we built the visitor center, we had tribal representation on site. We’re proud of that partnership,” Henning reports.
        Although the indigenous peoples farmed the land, their agricultural imprint was not as large scale as today. One of the goals of the park personnel is to restore the landscape to what it might have looked like in the 1500s. Henning points to timber stand improvement efforts that have helped bring back and stabilize native hardwood species and 240 acres of re-established tallgrass prairie as movement toward this goal.
       Most state parks offer RV camping and other recreational amenities, but Good Earth does not. Instead, there are 11 miles of hiking trails through the prairie, interpretive signs and overlooks, and an education-focused visitor center. The Good Earth mission, says Henning, “is concerned with preserving the area and making sure we take care of it the right way.”
                                                                              
       Dianne and I eventually ate our lunch at a pavilion overlooking the prairie and then walked the grounds. The grass paths were warm against our sandaled feet on this hot summer day. The restored prairie blazed with wildflowers on the uplands, and woods outlined the steep ravines and valleys. At an observation deck we looked out over the Big Sioux River and its wide valley across to the farms and silos on the horizon, and thought about the changes that had come across this land.
     For two hundred years, Good Earth provided well for the Omaha, Ponca, Ioway, and Otoe nations. Three hundred years later, it is enshrined as a South Dakota state park.
         But for Dianne and me, for a single July morning, Good Earth arose on the landscape like a shimmering unexpected gift.
 
                                                                                                                                                       March 2024
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The golden prairie reflects park efforts to restore the landscape as it may have looked in the 1500s. (Photo by Shawn Koch and provided with approval of Good Earth State Park.)
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The Good Earth Native American villages sat on both sides of the Big Sioux River demarking South Dakota and Northwest Iowa. Four regional tribes collaborated in this trade-center community from 1500-1700.
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A hilltop prairie at Good Earth State Park is rimmed by the forest that lines the Big Sioux River.
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BLACKHAWK WILDLIFE AREA, JACKSON COUNTY, IOWA

1/18/2024

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An upland trail affords occasional glimpse of the Maquoketa River that rims the Blackhawk Wildlife Area.
     A two-mile gravel road leads from Highway 64 to the Blackhawk Wildlife Area. I last visited the site on a mid-October day free from classes when leaves were beginning to turn, more copper than gold or red in the autumn sun. Cattle lazed in shaded groves along the road, lying or grazing among fallen trunks. It’s an unassuming road, even occasionally a bit unkempt. But at the end of the lane, Blackhawk is a grace note.
      A grace note in music is a tiny ornamental note heralding the next big, flourishing sound. In a similar way, Blackhawk Wildlife Area, is a smallish, 180-acre refuge at the southern edge of the hilly, rocky Driftless Area that spreads over 24,000 square miles north to northeast. Owned and managed by the Jackson County Conservation Board and located six miles west of Maquoketa, Blackhawk offers a Driftless preview of prairie remnants, woodland trails, river overlooks and glimpses into the local past.
    Jackson County Naturalist Tony Vorwald considers Blackhawk a little gem, even a bit of a diamond in the rough. “In spring you’ll find ephemeral flowers like snow trillium, spring beauty, and trout lily,” he says. He mentions the refuge’s tall bluffs overlooking the Maquoketa River, mature oak stands, and cool summer micro-climate rock outcrops harboring relict northern monkshood wildflowers that once flourished at the edges of the glaciers.
      But there’s a “good, the bad, and the ugly,” too, he says, as the county works at restoring habitat compromised prior to the land becoming a Jackson County Conservation property.
      The preserve’s two miles of hiking trails begin in the uplands with a few strands of remnant prairie. But prairies need occasional fire to prevent forest encroachment. Prairie fire hadn’t occurred for decades, Vorwald explains, so the Conservation staff has had to remove woody species, replant some prairie, and maintain the area through prescribed burns to bring it back to    prairie health.
      From the prairie, a trail swings down into the hardwood forest, granting occasional bluff-top glimpses across the blazing reds and yellows lining a bend of the Maquoketa River. Leaf litter along the trail and tell-tale tree bark revealed walnut, shagbark hickory, maple, and oak. During my solo hike, occasional shadows swooped overhead like raptors, but turned out to be large, swirling oak leaves, each taking its individual turn to settle on the forest floor.
      Occasional timber harvest of red oaks and walnuts provides some income for the Conservation Board, but more importantly maintains and improves habitat, Vorwald explains. Hardwood forests need occasional canopy breaks for regeneration. Too much shade will age out a healthy forest. To restore the hardwood forest after a timber harvest, the Conservation Board planted 2000 red oak and walnut trees, which at 30 years old are now coming into their prime.
      The geologist’s eye is next engaged as the trail descends steeply alongside a 50-foot limestone bluff laid down 420 million years ago in an ancient, shallow sea. Caves and indentations pock its lateral face as the bluff curves away from the trail. Sturdy boots and a hiking stick aid in the rock-strewn descent. It would be easy to leave an ankle behind on the path I’ve chosen.
     The base of the trail opens up to a Maquoketa River flood plain. At first glance the flood plain appears to be the least adorned of the Blackhawk habitats. But the flood plain provides cover for neotropical birds such as indigo buntings and scarlet tanagers migrating north in spring, says Vorwald.
     The flood plain is also where the wildlife refuge brushes up against its human past. Along the river and separated from the rest of the preserve by private property lies a parcel that housed YMCA Camp Blackhawk from 1918 till the 1950s. Little remains of the old Y camp except for a few footings and foundations. But the likewise defunct Boy Scout Camp Iten, removed a bit from the river, is more generous with its artifacts left behind from its reign from the 1930s to the 1970s. Where else in the forest will you find old dishware or a remnant chimney from a disappeared Scout camp dining hall? A 1931 Telegraph Herald / Times Journal article hailed the forty-some volunteers who descended into the valley floor to build sleeping cabins, latrines, a ranger’s cabin, and a 46 X 64-foot lodge/mess hall that eventually left only its chimney behind in the woods.
     Youthful campers left relatively little impact on what would become the Blackhawk Wildlife Area. But part of the uplands had seen a more damaging past, utilized by area industry as a dumping grounds for old machinery and parts. In preparation for the land’s transition to a wildlife area in the 1980s, the businesses cleaned up the site, covered it with fresh soil, and planted black locusts. Unfortunately, the thorny locusts are an aggressive species that the County is now working to replace.
     It was a lazy day’s solitary hike. The trail back up to the parking lot sprung a few more surprises, with rocky knolls popping out from behind the twists and bends. Winding back to where I started left me with the feeling that I was at the edge of something bigger.
     The 180-acre Blackhawk Wildlife Area is just one of 38 Jackson County Conservation properties that altogether comprise over 2500 protected acres. But even more, Blackhawk is a grace note at the edge of the Driftless, announcing ever-so-briefly and elegantly the mysterious hills and valleys that stretch far beyond.
                                                                                                                                                                                 January 2024
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A hiking trail at Jackson County’s Blackhawk Wildlife Area offers October finery.
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All that remains of a 1930s Boy Scout camp in the Blackhawk Wildlife Area is the mess hall chimney in the woods. (Photo contributed by James Varcho.)
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The uplands contain some remnant and restored prairie.
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One trail steeply descends alongside limestone bluffs to a Maquoketa River floodplain.
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South Dakota: Edge & Transition

10/30/2023

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Split Rock Creek has downcut through the pinkish quartzite at Palisades State Park in Southeast South Dakota.
     In South Dakota, the sky is vast but nature often occurs beneath you—in prairie grasses, in kettle ponds, and where the ground slices away beneath your feet.
     Anticipating prairie, Dianne and I were surprised to find that northeast South Dakota is also known as the Glacial Lakes region. The preponderance of natural ponds and lakes defies the state’s stereotype as an endless plain. Kettle ponds or “potholes,” as they are sometimes called, formed when melting glacial chunks calved off from the retreating ice 12,000 years ago and pressed into the soft, newly exposed soil. When the ice blocks melted, ponds formed in the depressions.
      Larger lakes were formed by glaciers scooping out lowlands or by meltwaters pooling behind ice dams. Regardless of origin, these blue-eyed ponds amid the farm fields and pastures keep a watch on South Dakota’s big sky.
      The largest glacial lake in South Dakota is Waubay Lake, encompassing 15,000 acres. A corner of the lake and its surrounding uplands and islands also comprise the 4600-acre Waubay National Wildlife Refuge. The lake and refuge name are derived from the Lakota “Wa-bay,” “where the birds nest,” and the combination of lake, islands, edge marshes, prairie, and woodlands harbors 100 nesting species and another 150 migrating species.
      A narrow causeway road led us to one such island where the refuge’s visitor center resides. Our hike around the island began at the water’s edge. The lake today is at a decades-long high level after years of excessive precipitation, although more recent droughts have reduced it somewhat. Drowned tree trunks line the lake about ten feet into the water, indicating an old shoreline. A distant line of immersed, decaying trunks marks an old boundary between lakes that have now fused together. Ironically, the higher lake levels threaten the island’s wetland habitat. Good wetlands need to dry out occasionally at their edges, allowing plants to take root and provide food for nesting and migrating birds.
     A boardwalk trail spans across the marshes at the edge of the lake, while a woodland trail rises upland into hardwood forest and then marches into open prairie.
Habitat variety and its eastern Dakota location make the Waubay Refuge a transitional place. Burr oaks are at their westernmost fringe. Eastern forest birds are at the extent of their range, and mingle with other birds at their southern, northern, and eastern edges. Bird chatter in the heat of midday also suggests this must be a meeting-place of sorts.
     Although still numerous today, many of the region’s lakes and ponds were drained in the early decades of mechanized agriculture to increase farming acreage. Conservation efforts to preserve the ponds began after the 1949 publication of a Field & Stream article titled “Goodbye Potholes.” Prior to that, the Soil Conservation Service subsidized the draining of the pothole ponds.
                                                             *                      *                      *
     The eastern corridor of South Dakota transitions as we drive south. The tranquility of glacial lakes and ponds gives way to streams and rivers that down-cut deeply into the landscape when glacial meltwater ran torrentially, exposing a quartzite bedrock. At Devil’s Gulch, a small but active stream still eats away at the pinkish rock, forming a narrow, deepening canyon.  Devil’s Gulch gained fame in 1876 when the outlaw Jesse James and his horse leaped twenty feet across the gorge, eluding capture after a wild pursuit following a bank robbery 170 miles away. Dianne and I chose instead a two-foot chasm to step across, then took a footbridge across the stream where the gorge is wider.
     From Devil’s Gulch, Split Rock Creek continues three miles downstream to Palisades State Park, where the quartzite pokes through the landscape again. The creek exposes and bisects 50-foot cliffs and towers of the pink, angular rock. Crevassed vertically, etched horizontally, occasionally leaning, and topped by boxy blocks of stone, the palisades look like large, precariously perched toy building blocks. Dianne and I scrambled over the rocks like salamanders, clinging from stone to stone while climbing onto ledges and descending again to creek side.
      The rock is 1.8 billion years old, originating on a sandy sea floor. Compressed and pressurized by accumulated weight and by movement of the continental plate, it formed into sandstone and then slowly metamorphized into Sioux quartzite. In places we found ripple marks on the rocks’ flat exposures, offering a glimpse into its sea bottom past.
     On the southern end of the park, a trail descends through a breach in the rock and empties onto a grassy shoreline path. Here the quartzite begins to recede from the visible landscape. Upstream lies 50 feet of exposed cliffs and towers, then 20 and 10 feet, and here—right here—the quartzite disappears back into the ground.
     The Big Sioux River takes its own turn slicing into the quartzite 26 miles further southwest in Sioux Falls. Once buried under sediment, the quartzite here became exposed at today’s Falls Park when the Big Sioux likewise carried a rush of glacial meltwater. Today the river has adopted a divide and conquer strategy, splitting right and left and nosing out the weak spots in the rock, through which it spills in numerous small and larger waterfalls in the course of a 100-foot drop. Along with a throng of other visitors, we milled about the rocks, each of us edging up to our own personal favorite falls.
     There is a “this-ness” to creation, a point at which the immensity of nature comes down to one particular patch of earth. A universe of grasses and wildflowers proliferate in a remnant prairie at our feet. An ice chunk long-ago toppled from a glacier’s edge hollowed out the pond we hike around today. Sioux quartzite that elsewhere lies buried suddenly emerges at the surface right in front of our eyes. Nature’s vastness suddenly whittles to one small waterfall where part of the Big Sioux River squeezes through a gap in the rock at the base of my feet.
     South Dakota is a state of transition and edge. Nature feels closer here when you stand on the brink.

​-- October 2023
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Waubay Lake is South Dakota’s largest glacially formed lake at 15,000 acres. Drowned trees along the shoreline show the effects of decades-long high water.
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At Sioux Falls, SD, the Big Sioux River drops 100 feet through numerous spillways at Falls Park.
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The Big Sioux River cuts through the quartzite bedrock at Falls Park, Sioux Falls, SD.
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A quartzite tower at South Dakota’s Palisades State Park appears to teeter like a stack of toy blocks.
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Shawnee National Forest & Garden of the Gods, Southern Illinois

8/24/2023

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Rain, frost, and wind have sculpted the sandstone into elegant patterns and swirls at southern Illinois’ Garden of the Gods.
     We had already crossed the railroad tracks on Highway 29, leaving Makanda, IL, behind in the rearview mirror, when Dianne spotted something interesting on her smartphone. Makanda calls itself Illinois’ “hippiest town.” Naturally, we turned around.
   Makanda, population 542, resides in the western wing of Illinois’ 289,000-acre Shawnee National Forest, which in turn sits at the southern edge of the Midwest along the Ohio River.  The forest hills’ history seems to suggest that it is good to live at the edge, so long as it’s on the mountain’s terms.
    The southern Illinois landscape changed quickly as we entered the national forest from the north earlier in the week. Successive waves of glaciers long ago flattened central Illinois, leaving behind a thick glacial till that ushered in the prairies that, in turn, gave way to the plow in the 1800s. On the long, straight stretches of road we reached often for coffee, snacks, and trivia cards to keep alert.
     South of Carbondale, however, beyond the glaciers’ ancient reach, the land began to dip and swell. The roads narrowed and swerved. Forest replaced farmland.
    Nineteenth century immigrants to southern Illinois were mostly American citizens moving on from Kentucky, Tennessee, and Carolina wooded highlands. Virgin forests fell quickly to the new arrivals, who logged the hills to supply fuel for area iron furnaces and steamboats on the Ohio and Mississippi rivers. Once deforested, the land was converted to farming.
    But the thin forest soil and the era’s erosion-prone farming practices on the hilly terrain made agriculture a short-lived enterprise. By the early 1900s, the soil’s productivity had been depleted. The population peaked and began to decline by 1910. The federal government soon began buying up distressed farms and abandoned property to re-establish the forest, and by 1939 the Shawnee National Forest was created.
     Communities adapted or died. Makanda proved a delight with its throw-back, edgy boardwalk shops. In PB & J’s Clothing and Gift shop we spied a vintage Janice Joplin concert poster, tie-died 60’s clothing, and photos from the 2017 total solar eclipse. (On April 8, 2024, a another total eclipse pass across Makanda.) At the Rainmaker Art Studio we wandered into an imaginary underwater dreamworld metal sculpture display and through a whimsical, terraced backyard sculpture garden etched into the hillside. Posters reminded us that we should return in October for Vulture Fest, a quirky celebration of artists, musicians, and fall raptors.
     People have been long attracted to the Shawnee Forest and its ancient, rocky landscape. At Giant City State Park, angular gaps in the three-story sandstone bluffs look like narrow city streets and alleyways. The rock havens have offered seasonal and personal protection across the ages. Soldiers from both sides of the Civil War took refuge here. Other people from other times have also found themselves in these stony passageways. Who was “Virdenille” who carved his name in the rock in 1933? Or E. Miller, who did the same in 1886?
      Earlier cultures occupied Giant city as well. Ashed-over rock ceilings date back 12,000 years ago to the end of the glacial era. Remnants of Woodland Period (AD 600-900) stone walls lace through the park. No one knows their ancient purpose, whether for defense, to demarcate fields, or for some other community use. In the thick of the woods, Dianne and I imagined the segments back into wholeness.
     Ancient peoples inhabited other areas of the Shawnee Forest as well. At the Millstone Bluff Archaeological Site, Mississippian-period (AD 1350-1550) Native Americans built a village 320 feet above the valley floor. Small forest depressions mark the locations of seven family dwelling sites that have been excavated from among 26 thought to have existed at the top of the bluff. A flat clearing in the woods may have served as the town plaza.
   Farther into the woods on the half-mile hiking loop we encountered other vestiges of Mississippian life…and death. With the help of an interpretive sign, we picked out petroglyph images on a mossed-over stone: pipes and axes, turkey tracks, and a thunderbird with outstretched wings and claws about to grasp its prey. In another location, rectangular rock slabs outlined a long-ago-looted stone-box burial site.
      The most literal edge of the Shawnee National Forest is the Garden of the Gods. Located in the eastern reaches of the Shawnee National Forest, about 12 miles from the Ohio River, these blufftop sandstone outcrops perch 300 feet above the surrounding valley, overlooking a 3400-acre wilderness area. The sandstone here has been shaped like pottery into graceful swirls and columns. Compressed into bedrock 320 million years ago on a sandy sea floor, the land then uplifted and the sea subsided. Rain, frost, and roiling winds have been weathering the stone back to sand ever since. 
     We ran our hands along the weathered surfaces of sandstone boulders adjacent to the hiking trails. Honeycomb indentations like tiny moon craters had been scooped from soft pockets on the rock surface. Colorful swirls and concentric rings in the sandstone walls resulted from minerals—like iron—leeching from the interior to the rock face.  At the base of every rock, small piles of sand gave evidence of the still-active erosional forces. (Remember, stone, that you are sand, and to sand you will return.)
     Wind and rain have molded the sandstone into imaginative shapes on the cliff’s edge, like Camel Rock, the Devil’s Smokestack, and Anvil Rock. Gnarled cedars perched on outcrop ledges complete the look of a land sculpted by time.
                                                                  *                      *                      *
      When the town of Makanda lured us back to take a second look, it was telling us something about the Shawnee National Forest. While there may be no such thing as a typical Midwest landscape, southern Illinois is definitely an outlier, an edge. To live here, one has to adapt to the land.
      If we return, it will be for some future October Vulture Fest. We’ll come for the artists, the musicians, and the forested hills, and to watch the raptors circling and soaring from their blufftop sandstone perches.
 
-- August 2023
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Garden of the Gods’ “Camel Rock” overlooks a 3400-acre wilderness area within the Shawnee National Forest.
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Located within the Shawnee National Forest, the town of Makanda calls itself “Illinois’ hippiest town.”
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At southern Illinois’ Giant City State Park, gaps in the sandstone bluffs appear as “city streets” and alleyways.
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A thunderbird petroglyph in the Shawnee National Forest speaks of Native American civilizations that inhabited the region.
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The Driftless Area Conservancy - SW Wisconsin

7/6/2023

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A signpost marks the way on a developed portion of the planned Driftless Trail near Dodgeville, WI.
     “Walking ferns, the way the fog settles into the valley, how cliffs arise out of nowhere,” these are among the landscape traits that drew Jennifer Filipiak to her position as Executive Director of the Driftless Area Land Conservancy (DALC) back in 2019.
     Founded in 2000, DALC is a nonprofit land trust organization centered in Dodgeville, WI. Over forty such land trusts are scattered throughout the state, Filipiak explains, but at the time there was a “donut hole” in southwest Wisconsin. Meanwhile, Driftless Area landowners were seeking to preserve beloved landscapes with steep, forested hills and valleys, rock outcrops, and spring-fed trout streams.
     The Driftless Area Land Conservancy serves both the land and the people of the unglaciated Southwest Wisconsin. DALC counsels landowners through the conservation easement process to protect designated private properties from development, manages habitat on its own preserves, and connects people to the land by providing access to nature and through volunteer restoration efforts. DALC also works with agricultural landowners to help them protect waterways.
     For Filipiak, the Driftless Area is not just about the landscape. “The culture here is defined by our geology,” she says. “We know why we have rock outcrops here and groundwater seeps there. We have smaller farm fields and more grazing with our hills. And there is a Driftless community here who connect to nature through the arts.”
     One such artist, Roland Sardeson, helped DALC secure one of its nature preserves when he donated his 12-acre wooded site near Mineral Point upon his death in 2016. Sardeson was a potter, stone mason, and beloved community theatre actor. “Everyone knew Roland,” Filipiak says, which may be why the Mineral Point community has been so helpful in building trails, an informational kiosk, and a parking area at what is now called the Sardeson Preserve.
     The Sardeson Preserve offers a one-mile wooded hiking loop among 30-foot sandstone bluffs, tumbled boulders, through a stream-bottom valley, and across a dry-bed creek bed that occasionally gifts arrowheads to passersby. “If I were someone who lived here before development, this is where I would have hung out,” Filipiak muses.
     My wife Dianne and I first visited the Sardeson Preserve in April 2023. I was quickly drawn to the sandstone bluffs. The surface of the yellow, tan, and green-streaked sandstone undulates in whorls and waves reminiscent of the primordial seashores in which it was formed. Brush your hand against the stone and you are immediately wearing remnants of this ancient sandy beach.  Wind and water have continued sculpting its pottered texture.
     Though it was a spring day, winter hadn’t yet released its hold on the forest floor, so the tumbled boulders were in easy view. Large and scattered on one slope, the boulders are plentiful though smaller across the valley. There they were stacked and layered as if waiting to be redeployed, and in fact some past landowner had built a handsome stone fence—dry-stacked, Irish-style—to mark the edge of the property.
     Winter-melt had caused some mild flooding in the valley floor on this April day, and Spring Peeper frogs ratcheted their wet delight as we hiked.
     I returned by myself in late May. In the stream bottom, just beyond the preserve, lowing cattle had replaced the Spring Peepers now that the bottomland had dried up and spring grasses were thriving. Ferns, mayapples, prairie grasses, and (yes) poison ivy had softened the tumbled boulders. Hillsides were lush with Dame’s Rocket, an invasive yet striking forest flower that had turned the woods into a sea of purple and white.
     The Sardeson Preserve is one of three properties owned by the Driftless Conservancy. But much of its work also involves collaborating with private landowners. One such privately owned property with a conservation easement overseen by the DALC is the Weaver Road trail segment of what will eventually become the Driftless Trail.
Located seven miles north of Dodgeville, the one-mile hiking trail begins along the perimeter of Seven Seeds Organic Farm and then dips down into a wooded valley. Three “Leopold benches”—a simple wooden bench design made popular by the famed conservationist Aldo Leopold who lived not far from here—announce the pathway into the forest.
     The trail glides along a hogback ridge, a landform in which a narrow spine of hard bedrock straddles above steep downward slopes on either side. At the end of the ridge, the trail switchbacks down into a valley of 90-year-old oaks and walnuts. This isn’t virgin timber. It was likely once cleared for pasture, but long-ago abandoned, its native trees are returning to glory. The return trail is more overgrown, its canopy having been decimated by a 2014 tornado. But that simply means to wear long pants and walk the trail often to better establish the path!
     For now, the trail loops back to its beginning, with about a 250-foot drop from trailhead to valley floor. Eventually it will become part of the 50-mile Driftless Trail that DALC is helping to piece together. Although it is a thirty-year vision, when completed, the Driftless Trail will take hikers across private and public lands passing through Governor Dodge State Park, Taliesin (Frank Lloyd Wright’s architectural studio and school) and Tower Hill State Park near Spring Green. The trail will provide a wildlife corridor from Military Ridge (an existing trail originating in Dodgeville) to the Wisconsin River.
   Privately-owned trail segments will be negotiated only with willing landowners. “Many landowners enjoy sharing the natural wonders of their lands,” says Filipiak, and DALC will work with them to create permanent easements for the Driftless Trail.
    Many such landowners are area farmers. Having previously worked for both the Nature Conservancy and the American Farmland Trust, Filipiak is convinced that “agriculture and conservation need to, and can, work together, not be fighting each other.”
     After all, the goal of the Driftless Area Land Conservancy is to serve people, not just the land, Filipiak insists. “We’re not protecting land from people; we’re protecting land for people.”
 
            -- June 2023
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Rain and wind-carved bluffs adorn the Driftless Conservancy’s Sardeson Preserve near Mineral Point, WI.
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Dame’s Rocket covers the valley floor at the Sardeson Preserve in late spring.
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The Weaver Road segment of the Driftless Trail dips down into a second-growth forest.
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The Flint Hills, Eastern Kansas

5/8/2023

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Canada Wild Rye frames a view of the Flint Hills landscape.
 
     “Red Buffalo is what the Plains tribes called prairie fire,” says Heather Brown, Chief of Interpretation and Visitor Services at the Tallgrass Prairie National Preserve in the Kansas’ Flint Hills region. Driving across the rolling landscape, Dianne and I could imagine bison and fire in equal measure leaping across these hills.
       The Red Buffalo keeps the prairie alive. Prescriptive burning of the prairie regenerates grasses to their nutritional best. “Prairie thatch blocks the sun from reaching the soil,” Heather explains, “squelching off new growth.” Fire puts the sun in contact with the land.
       Prairie once covered 400,000 square miles of North America from the Rocky Mountains to the Mississippi River and beyond. Before Euro-American settlement, 30% of the North American landscape was grass-covered. Less than 4% of that original prairie has remained. The Flint Hills harbors 80% of that surviving prairie, stretching for 90 miles east-west and 160 north-south through most of east-central Kansas.
                                                            *                      *                      *
      Author Willa Cather wrote, “It takes a soul to love the prairie.” At the Tallgrass Prairie National Preserve, Eric Patterson, Lead Park Ranger, is one such soul. Eric offers this advice to anyone who lacks the prairie eye: “Don’t expect things to leap out at you. The prairie isn’t one of those environments that will knock you over. It’s more subtle than that. On the other hand, it often offers a vast scenery where you can see for ten or twenty miles.”
       But once you’re done looking at the vista, look at what’s in front of you. The Flint Hills sports 70 varieties of grasses and 400 wildflowers and other forbes. Wildflowers take turns blooming from late spring through fall, each attracting their own set of pollinators.
     For those of us whose idea of grass is the lawn we mow every Saturday, it can be a steep learning curve. “Your front lawn at home is the definition of a disturbed landscape,” Eric laments,  “a monoculture of plants that have just one skill.”
      In fact, much of the skill of the prairie is unseen, underground. The root systems of prairie plants are vast, sinking ten to fifteen feet deep, enabling them to weather droughts and long, cold winters. Their thick, intertwining roots also hold the soil in place. “Three-fourths of the plants’ biomass is underground,” Eric explains. Above ground, the annual cycle of decay and regeneration of plant matter built up the Midwestern topsoil, in some places up to eight feet deep.
       “Grasses are pretty resilient,” he continues. “If it’s dry, they simply slow their growth and store their energy in their roots. In wet periods the grasses grow more full and tall.” Prairie grasses are “the meek that have inherited the earth,” he says. “They don’t necessarily blow their own horn.”  
     The Tallgrass Prairie National Preserve manages a mere 11,000 acres of the Flint Hills’ 4 million prairied acres. Most of the Flint Hills’ natural prairie lies in private ownership and is maintained by cattle doing the former work of bison, eating and trimming the prairie grasses and setting the stage for regrowth.
      The proximity of limestone bedrock to land surface is the main reason that so much of the prairie remains intact here. In the Flint Hills, limestone lies just inches below the soil and frequently protrudes, ensuring that much of the Flint Hills was never plowed, except in the stream bottoms where the soil covering was thicker.
     Instead, the Flint Hills prairie has been cattle-grazed since the arrival of Euro-American ranchers, In the absence of bison, cattle grazing protects the prairie to a reasonable degree. “Ranchers recognize that they are dependent on the long-term health of the grass,” Eric maintains. “If the grasses fail, so do they. And grasses do need to be grazed. Bison were the natural grazers, but now that task falls to cattle.”
       There are differences between the grazing habits and behaviors of bison and cattle—with cattle being rougher on the landscape. Bison, for example, might graze a section bare and then not return to it for several years, while cattle are typically confined to limited, albeit large, acreages. Ranchers simply have to “find the delicate balance between economic and ecological needs,” says Eric.
      The Tallgrass Prairie National Preserve grazes both cattle and bison. Its trails make no pretense of separating the hiker from the bison by fence or vehicle. “Keep your distance”—about 100 yards—is all the warning given on refuge signs, with no particular suggestions about how to do that should a bull decide to charge. But in the heat of our July visit, the bison had apparently retreated to some tucked away glen. One bull was visible in the distance, lounging in the sun and then rising to eat, turn around, dust him himself off, and lounge again. We kept our eyes glued on him, out of wonder and respect, and to make sure that he stayed in place. What we would’ve done if he’d bolted, I have no idea. Dianne can probably run faster than me.
     But the trail did offer evidence of bison wandering. Here and there was a “buffalo wallow” formed by bison rolling in the grass to cool and dust themselves off. Their weight in the soft prairie soil creates a hollowed-out depression that in turn becomes a tiny mud-pond in the next rainstorm, a haven to an array of smaller prairie creatures. In this totally second-hand manner, bison aid other life forms on the prairie.
     At various times throughout the growing season, the prairie bursts with coneflowers, wild bergamot, flowering splurges, showy evening primrose, and more, each taking is individual turn racing across the prairie as red, orange, yellow, and purple buffaloes. Prairie grasses include big bluestem, sideoats grama, Indian grass, hairy grama, and switchgrass.
       The Preserve’s ridge top trail makes for impressive vistas. The land stretches out for miles, with only a scattering of barns and other outbuildings visible in the vast horizon beyond the Preserve. Nothing here but wind, a prairie non-enthusiast might deduce.
       But the wind, too, was a Red Buffalo racing across the expanse, bending the grass tips in waves that rolled across the hills. You just have to stop to watch it.
 
-- April 2023

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Compass Plants reach up to the big sky in Kansas’ Tallgrass Prairie National Preserve.
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Flint rock at and near the surface hindered the plow in east-central Kansas, preserving 80% of the nation’s remaining tallgrass prairie.
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A butterfly flits amid wild bergamot.
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The Flint Hills defies the stereotype of unending Kansas plains.
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Hoosier National Forest, Indiana

3/19/2023

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The 1890s Brooks Cabin has seen southern Indiana’s old-growth forest fall to farm fields, and farm fields return again to forest.
       In a quiet Indiana woods, Dianne and I notice the slight gully intersecting the hiking trail. Wide enough for a compact car, it is overgrown with scrub trees, but its U-shaped track through the woods is still faintly visible.
       We step aside and listen, not for anything present, but for what’s long gone: hooves pounding the soil and raising a dust that strings along to the horizon. Snorts and grunts and bleats bellowing past.
       We find ourselves at a crossroads of past and present, hiking alongside the Buffalo Trace in the Hoosier National Forest in southern Indiana. When bison still roamed freely, they rushed along this path after crossing the Ohio River at a shallow ford each spring and dispersed through western Indiana and Illinois. In the fall they retraced the path back to warmer Kentucky grasslands. Their weight and numbers pummeled and pressed the pathway into the gullied depression still visible in parts of the forest.
                                                                  *                      *                      *
         The Hoosier National Forest covers 203,000 acres of south-central Indiana. In a state known for flat, sprawling corn fields and long straight roads, the forest landscape rises and dips from the Ohio River valley to just south of Bloomington.
    The forest, largely a second-growth replanting, was created out of the Depression-era heartbreak of failed farming communities. At a crossroads of broken dreams, a new course was charted.
        Mia Gilbert, Visitor Services Information Assistant, sat with us at a wooden picnic table under a grove of towering pines. She described the Hoosier National Forest’s beginnings. By the early 1770s, British-American settlers from Kentucky had begun moving into southern Indiana. The old growth forest fell quickly to farm fields.
      But the forest soil was thin, and the land was hilly and rocky. Erosion control was not yet widely practiced, and as the soils washed away, area farms lost productivity. Add in the droughts of the 1930s and Great Depression economics, and all too soon landowners were abandoning their farms. Congress empowered the National Forest Service to buy up land from owners willing to sell. By August 1935 the Forest Service was inundated with offers.
     To get a sense of the forest’s vastness, Mia suggested we drive to the nearby Hickory Ridge Lookout Tower, a 150-foot, 1936 steel structure built to watch for forest fires. The area was still transitioning from farm country in the 1930s, so at the time of construction, the tower also overlooked 80 farms, all of which have now been subsumed into the forest.
 We gave our farewells to Mia and drove off. Along the road, I noticed a nearly-hidden sign announcing the Town of Todd Cemetery. I’m attracted to old graveyards, so we pulled in. Much of the cemetery hearkened back to the farming community that pre-dated the National Forest. Small, weather-beaten tombstones poked from the ground, leaning in every direction. Many were unreadable, but a few still told their stories. There was Robert Crough, the toddler who lived from 1927-1930. The death date of Louisa E. puts her in her twenties, likely during childbirth. Private William Hicks, on the other hand, had long outlived his battle days, finally succumbing at 53 years old, his life spanning 1829-1882.
      A cemetery in the middle of the forest? This seemed odd to us. But soon enough we began seeing them all around as we drove or hiked, and we spotted even more on the maps. The cemeteries, too, suggested a crossroads between the farming past and the forested present.
                                                            *                      *                      *
        Another Indiana crossroads lies where the surface world and the underground intersect.
Marengo Cave, a National Natural Landmark just east of the forest, offered such a blurring.
Visitors tour among its nearly five miles of winding caverns through a phantasmagorical world of stalactites, stalagmites, soda straws, flowstone, and other formations. Shallow reflecting pools give the illusion of unlimited depth, their still waters perfectly mirroring the cave ceiling.
     Life forms within the cave offer their own little shop of horrors. Blind, translucent isopods scuttle along on shrimp-like legs searching for microscopic food in the cave’s streams, hiding out from equally blind, eyeless, pigment-less fish on the hunt. Millipedes and beetles explore the mud banks. Tiny, white-gray Springtails may jump when disturbed. Troglobitic spiders guard the natural entrances to the cave, catching and caching luckless insects that fumble into the openings.
       Rain and meltwater enters the Marengo Cave through sinkholes or seeps down through cracks in the limestone. Dripping interminably from the ceiling, cave water eventually forms an underground stream that emerges on the landscape five miles later.
                                                               *                      *                      *
     Back within the Hoosier National Forest, we next sought out Lick Creek, a long- disappeared Freed Black settlement. Freed Black families started coming to Lick Creek around 1811, since even the possession of “Freedom Papers” didn’t guarantee safety in nearby slave-owning states. Invited and welcomed by the Quaker Church of Lick Creek, by 1850 the Black community had expanded to 260 settlers in ownership of 2300 acres.
       By 1853, however, the state of Indiana required Black adults to register by name, place of birth and physical description. Prospects grew more ominous as the Civil War broke out. In 1862, with the war intensifying, many Black families sold their land and moved further north, some to Canada. Before long, Lick Creek was abandoned and the forest grew back.
                                                              *                      *                      *
     Indiana calls itself “the crossroads state.” Historically, this motto relates to its intersecting 1800s horse and wagon pathways as Americans and immigrants plied west and south. Today it refers equally to the maze of interstates that crisscross the state.
        The bison laid down a trail that others followed. Native Americans used the Buffalo Trace as a travelling path. French, British and American explorers followed it across the countryside. Settlers travelled the route in wagons, heading west, adding wheel ruts to the hoof prints. Stage coaches and the U.S. mail soon followed. U.S. Highway 150 was laid down parallel to parts of the Trace.
        The last bison was spotted on the Trace in 1799.
      Most of the Buffalo Trace is gone. But here in the Hoosier National Forest it runs beside us, crosses our path, and disappears again into the woods. I imagine the long line of dust that the bison must have kicked up with the weight of their hooves, a string that would have lingered long after their passing and tied together the horizons and everything beneath the dome of sky.
 
-- March 2023
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A 1930s 150-foot fire tower overlooks a portion of the 203,000-acre Hoosier National Forest.
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The Marengo Cave National Natural Landmark offers a subterranean universe of stalactites, stalagmites, flowstone, and other formations in southern Indiana.
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A faint indentation from bison hooves is still visible along the Buffalo Trace in Indiana’s Hoosier National Forest.
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A weathered tombstone reminds visitors that farming communities once thrived in today’s Hoosier National Forest.
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Hocking Hills Region, Southern Ohio

1/8/2023

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A waterfall tumbles from the overhang at Ash Cave in the Hocking Hills.

     I wish I owned windows like these. Light streams in from seven Gothic openings stretching almost from the floor to the 25-foot ceilings. The openings are irregular, curved, carved, twisted, and phantasmagoric: an ace of spades, a bowling pin, a goose taking flight, tongues of fire. From the outside they can barely be seen, but from the inside the seven windows cast light spells across the otherwise darkened room.
      Dianne and I are in the Rock House cave in southern Ohio’s Hocking Hills. Largely hidden behind a massive sandstone wall, the cave is accessible only through its seven window-like openings. This cave—running 200 feet long, 20-30 feet deep, and 25 feet tall—has been home to ancient peoples for thousands of years. The windows are water- and wind-hewn entrances to the cave interior. We use our camera flashlights to negotiate the deeper recesses and uneven floors where the light doesn’t penetrate. We bask in the coolness of the chamber, and in the perfect balance of light and earth and underworld.
      Hocking Hills is a 2000-acre state park in southern Ohio, known for its numerous waterfalls, arched cliff faces, and steep, narrow box canyons. Other features of the park, like Ash Cave, Old Man’s Cave, and Whispering Cave, are not true caves but recessed, horseshoe-shaped rock shelters wedged into the bedrock, hidden away behind waterfalls that drop 200 feet or more from overhanging ledges. People have taken refuge here for thousands of years in a delicate balance straddling the land surface and the underground.
                                                                     *                      *                      *
       An hour west of the Hocking Hills near the present-day city of Chillicothe, ancient indigenous peoples once pondered the relationship among the earth, sky, and underworld. This southern Ohio region is home to at least six different sites with conical, linear, serpentine, and elliptical burial mounds. This was the birthplace of the Hopewell culture from 200 B.C. to 400 A.D., whose trade patterns, artwork, and signature burial and ceremonial mounds spread throughout the Midwest and beyond.          
       Metalwork and carved mineral-stone from across North America have been unearthed from the mounds. Copper—perhaps from Michigan’s Upper Peninsula—was patterned into a copper headdresses, copper hands, copper stars, copper antlers, copper falcons. Mica from North Carolina mountains was thinly sliced, like onion skin, into shapes of hands and abstract swirls. Ceramics and pottery utilized designs traceable to indigenous peoples from the Appalachian mountains. Local Hopewell-based ceramic pipes were shaped as turtles, wildcats, falcons, and squirrels.
      Dianne and I walked among the burial mounds at one of the sites called Mound City. Taller than our Upper Mississippi mounds, the largest here reached 17 feet with a 90-foot circumference. No indigenous peoples lived at the earthworks, but nearby villagers and likely gathered here to trade, to marry, and, of course, to bury the dead.
      Archaeologist John P. Hancock writes that in Hopewell cosmology “the earth where we live is brought into being between the sky world and the underworld.” There was balance here: earth, sky, water, and what lay buried.
                                                                *                      *                      *
      Southeast of the Hocking Hills lies one of America’s earliest coal regions where the underworld got out of balance. Nelsonville, Athens, and a host of other local coal towns boomed in the 1870s and 80s. Sunday Creek, not far from our campground, gave its name to the second largest coal mining company worldwide. Small company towns abounded, with their tell-tale look of semi-identical homes on small lots, all in a line.
     But controversy and tragedy were hauled up alongside the wealth of coal. In 1884 striking workers set fires in numerous coal mines that burned for decades, venting from cracks in the surface ground. The largest mining disaster in Ohio history occurred in the Hocking Valley in 1930 near Sunday Creek when an explosion killed 82 workers. Mining disasters killed another 180 Ohio workers before the end of World War II.
     At the start of the 20th century 50,000 coal miners were employed in the region. But after World War II, mine shaft operations began shutting down, replaced for a while by surface strip mining. Eventually these, too, began closing. Today only a small number of coal-related jobs remain in the area.
     Meanwhile, despite some successful mitigation and restoration efforts, over three hundred miles of southeastern Ohio streams still bleed orange, white, and green where their waters emerge from abandoned underground mines.
                                                               *                      *                      *
      One early evening, we rode out from our Hocking Hills campsite to the Moonville Tunnel in the Zaleski State Forest. We turned into a muddy parking lot. One nearly-broken-down car sat amid the puddles near the access to the 16-mile Moonville Rail Trail. The trail led to an abandoned train tunnel that cut into the hills.
      Moonville was home to 100 villagers in the late 1800s, coal miners mostly. Workers walked the tracks to and from the local mines. The town dried up as the coal mines closed, with the last family departing in 1947.
      The Moonville tunnel is still part of local lore as the haunted site of six accumulated deaths until the railroad ceased operating in 1988. The 100-foot tunnel sports a handsomely bricked edifice announcing, in large letters, “MOONVILLE.” Above, below, and beside the town name, and inside the tunnel as well, layers of time-worn graffiti compete with the encroaching forest attempting to snuff out the passage.
       It was eerie, all right. There was something haunting at the Moonville Tunnel, but it wasn’t about railroad deaths. It was something from the underground itself.
                                                         *                      *                      *
       Ancient, indigenous peoples strove to keep the upper, lower, and middle worlds in balance. The Hocking Hills’ geological wonders kept the equilibrium as well, with underworld caves and rock shelters providing refuge to the middle world’s indigenous peoples. The Hocking Hills waterfalls today still bind earth and sky and underworld, plunging from the cliff faces and pattering at the stony canyon floors.
       But what happens, then, when the balance is upset? When extractive industries deplete buried ore? When boom leads to bust, and people are without jobs? When the imbalance poisons local streams?
       Maybe these are the questions that haunt the Moonville Tunnel near the edge of the Hocking Hills.

-- January 2023

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Window openings in the Hocking Hills’ Rock House Cave take a variety of fanciful shapes.
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5. Chillicothe, OH, was the birthplace of the Hopewell Culture that spread throughout the Midwest from 200 B.C. to 400 A.D. Burial and ceremonial mounds—this one 17 feet tall—were signature features of this Native American period.
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The Moonville Tunnel in southeast Ohio marks the location of a long-disappeared coal town.
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White Horse Hill, North Dakota

11/5/2022

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White Horse Hill National Game Preserve took its present name in 2019 to more accurately represent the local Native American peoples and their stories.
 
       The volunteer couple at the White Horse Hill Visitors Center told us where to look for the bison herd, except for one old bull who liked to wander off by himself and “rake you over with his stink eye” if you came upon him. So naturally that became our mission. Never mind the elk, the prairie dogs, the trumpeter swans, and the rest of the bison herd. We wanted to find old Stink Eye.
       The 1700-acre White Horse Hill National Game Preserve in northeast North Dakota dates back to 1904 when it was originally designated a national park. In 1914 it was re-classified as a Game Preserve for nesting and migratory birds. In 1917 bison and elk were introduced to the Refuge as their numbers had plummeted on the Plains. In the 1970s, prairie dogs joined the general melee.
       The Preserve sits on the southern bank of Devil’s Lake, at 330 square miles the state’s largest natural body of water. A remnant of an ancient glacial lake that once covered 4000 square miles of North Dakota, in historic times Devil’s Lake has alternately diminished and grown. In the drought-prone Depression era, it bottomed out in 1940 at a surface level some 50 feet lower than today. Then came a gradual rise through the decades, followed by a quick acceleration from the 90s to the present as regional rainfall increased. Since the lake has no natural outlets, the result has been a fisherman’s delight and a farmer’s nightmare. One farm at the former shoreline has lost 2500 acres to the swelling lake. Half-submerged barns haunt the shoreline. Roads have been swallowed up by the growing lake. It has lapped up the Preserve’s lowlands.
         Colleen Graue, Visitor Services Manager for White Horse Hill, says that despite the Preserve’s modest size, White Horse Hill harbors three distinct habitats. Wetlands at the lake’s perimeter are ideal for migratory birds. Elk love the woodlands. Bison and prairie dogs are partial to the prairie savanna.
       Hiking near the Visitor Center along the fence of the bison/elk enclosure, we saw none of the Refuge’s dozen elk, but noted their handiwork in clearing the underbrush as they ate their way through the woods. Woodlands are rare to North Dakota, where only two percent of the land is forested. But White Horse Hill’s location on the southeastern edge of Devil’s Lake helped the woods get established in pre-settlement times, Graue explains. Prairie fires that elsewhere swept across the landscape and kept tree growth at bay were snuffed out here by the big lake, allowing the forest to take hold.
      When we emerged from the woodland trail onto a prairie bluff, the trail’s descent toward the lake was blocked off. An old trail that once rimmed the lake was now underwater, and the field beyond it was flooded. Dead, drowned trees lined the old shoreline and the hiking path. The lake’s high waters have impacted the Preserve in other ways as well. The Visitors Center is new since 2006, necessitated by the rising lake waters, says Graue. The lakeside road to the old Center is now underwater.
       But the flooded lowlands have been a boon to the Preserve’s ducks, geese, pelicans, kingfishers, swans, otters, water snakes, frogs, and other wetland species.
        The Preserve’s 4.5-mile auto tour loop within the bison/elk enclosure is a favorite for visitors. Here, beyond the wetlands, the prairie rolls across the valley floor. The grasslands are home to at least two prairie dog towns. When we stopped at the edge of their burrowed city, they seemed as curious about us as we about them. Perched on hind legs while chewing stalks of grass, they sized us up, wondering perhaps whether our Honda was a big white bison. Finally, though, the small engineers nosedived back into their burrows to return to the work of interconnecting the holes with tunnels.
        In another section of Prairie Dog Town, a dozen or so of the twenty-ish bison milled about the burrows, tugging at the sod and looking bored. A few calves among them pondered the prairie dogs with curiosity and amusement.
         The bison herd is small, but the herd is prized throughout the federal Fish and Wildlife Refuge system for its genetic purity, says Graue. And because the acreage is limited, the herd has to occasionally be culled. Bison from White Horse Hill have been sent to other national wildlife refuges. At other times, excess bison are slaughtered and the meat distributed at the nearby Spirit Lake Indian Reservation.
       Near the edge of the perimeter hills, the prairie is dotted with hardwoods, mostly oaks, creating a prairie savanna. We climbed the 185-step stairway to the top of the Preserve’s namesake, White Horse Hill, overlooking the prairied valley and the surrounding upland forest. A 20-mph wind raked the hilltop grasses in wavelike pulses.
       White Horse Hill took its present name in 2019. For a century the refuge bore the name “Sully’s Hill,” referencing Army General Alfred Sully, who led several bloody campaigns against the Dakota Nation in the 1860s, including an 1863 massacre of 400 victims. Disturbed by the honor given to the massacring general within eyesight of the reservation, the Spirit Lake elders campaigned to change the Preserve’s name. The elders proposed the name White Horse Hill, or Sunka Wakan Ska Paha, to commemorate a wild white stallion that in earlier times was known to come down from the Hill to drink at the lake.
        We didn’t see a white stallion. In fact, we’d nearly given up on seeing elk until we finally heard one through our open car windows, and then spotted him, slowly mashing his way through the forest, stripping and munching leaves as if they were lettuce.
      Back at the prairie dog town, we had also looked for Old Stink Eye among the bison, but couldn’t seem to find him. So we gave the auto tour loop a second lap. We found him, finally, not far from the Visitor Center, his dark, humped shape off by his sullen self in a grassy clearing.
He seemed to hold within that eye the Preserve, the lake, the tribal history, all permanence and change.
        Don’t mess with me, he seemed to say. So we drove on.
 
-- Kevin Koch
November 2022
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The stairway to the top of White Horse Hill leads to an overlook of the forest and prairie habitats.
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Bison were introduced to the White Horse Hill National Game Preserve in 1917. Photo by Bob Christie, at White Horse Hill.
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Prairie dogs have been creating a burrowed city since their introduction in the 1970s.
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An inlet from Devil’s Lake’s decades-long high water has submerged a hiking trail and lowland trees.
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White Horse Hill National Game Preserve offers a textured landscape amid the North Dakota plains.
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Copper Harbor & the Keweenaw Peninsula, Michigan

9/5/2022

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The town of Copper Harbor on Lake Superior was an 1800s port for shipping copper ore from Michigan’s Keweenaw Peninsula.
      Hannah Rooks’ father always told his clients to listen for the “quiet full of noise” in the Northwoods. He wanted them to listen for bird song and the rustling of the leaves. Her father, Jim Rooks, ran Bear Track Eco Tours in Copper Harbor, Michigan. Before that, he had been the first Director of the E.B. Lyons Preserve in Dubuque, IA, and city Naturalist from 1974 to 1983. Born in Michigan, he felt the call to return, not just to the state, but to one of its most remote locations.
      Copper Harbor, population 136, sits near the tip of the Keweenaw Peninsula, the northernmost point of Michigan’s Upper Peninsula. The Keweenaw peninsula is a 55-mile, sickle-shaped sliver of land that slices into Lake Superior along its southern shoreline. This had once been copper country, but the mines had shut down long ago and ghosted many a town. Tourism is king now. Not the waves of visitors who favor easy-to-reach parks, but still a steady stream willing to drive to the end of the earth, or at least this portion of it.
      As Dianne and I descended the long hill into Copper Harbor on a Thursday morning in July, we found a town going about its own business. There were motels and B&B’s for visitors, but they seemed modest enough in size and décor, and all locally owned. We found a hidden bookstore, Grandpa’s Barn, that rivaled those from the cities. We found the Laughing Loon, the gift shop Jim Rooks and his wife Laurel opened in Copper Harbor and which Hannah now runs since the passing of her father in 2005 and her mother’s retirement.
     Looking down from Brockway Mountain above the town, it’s easy to see how the harbor and its lighthouse offered a protected gateway to Lake Superior for shipping 19th and early 20th century copper ore. While French and British colonialists in the 1600s and 1700s lightly mined sites first utilized by Native Americans as long as 7000 years ago, the first big U.S. copper rush gathered steam in the 1840s. Copper mines throughout the peninsula shipped their ore through Copper Harbor, giving it a bustling population of 1300 by 1887.
     Dianne and I toured the remains of the Delaware Copper Mine that had operated from 1846-1887. Properly helmeted, we descended 100 feet into the uppermost level of the long-defunct mine. Alongside the stairway ran old rails that once hoisted copper and rubble rock up to daylight.
Seepage from recent rains glistened, dripped, and trickled into the descending shaft, then disappeared into darkened passageways. Electric lights in lantern casings now lit the lateral vein, but they were soft, subdued, and spread far apart along the passageway. They gave off a dim light as copper-colored as the hard-sought ore, offering just enough light to peer into subterranean rooms and into cross-cut passageways. The tops of shafts descending to the lower levels were just barely visible, the shadows revealing the water surface of the seepage that filled the several lower levels—the deepest shaft descending 1400 feet—in the years following the mine’s closure. The topmost level was reasonably dry, as it drains through a distant adit, or horizontal vein that opens to the outside world.
      Inside, the temperature was a constant 43 degrees Fahrenheit. A white fungus grew on some of the wooden structures, the result of the damp air. Timbers still supported the bedrock roof. Other bits of timber and rail had been discarded and left at the side of the passage. A few supplies had been left behind as well, including a long, hand-cranked drill used for boring into the rock.
At least two other defunct mines on the peninsula are open to the public.
     Mining was dangerous and plagued by labor disputes. Mine owners sometimes adopted brutal tactics against striking miners, hiring violent strikebreakers. Songwriter Woody Guthrie immortalized the 1913 tragedy at Calumet, MI, 30 miles from Copper Harbor, when strikebreakers yelled “Fire!” and barred the only door at Italian Hall where striking miners and their families were celebrating Christmas Eve. Panic ensued, and 73 persons died, half of them children. No one was ever arrested.
     Dianne and I found a memorial to the massacred victims in downtown Calumet. Although Italian Hall is no longer standing, the fateful door is preserved, along with the story of what transpired.
      Copper mining began to wane after 1916, and by the 1960s was pretty much finished.
     Today, the Keweenaw Peninsula offers the great outdoors, not the insides of mines, as its chief asset. South of Copper Harbor lie the Estivant Pines, a stand of 300-year-old white pines stretching 125 feet tall. Fort Wilkins State Park, just a mile up the road from Copper Harbor, preserves the history of an 1844 U.S. fort established in the midst of the mining boom. The Keweenaw Peninsula offers numerous other beaches, parks, wildlife sanctuaries, and lighthouses along the Superior shore. Visitors can stop for a photo-op to measure themselves against a towering mast marking the average seasonal snowfall of 240 inches.
    But the highlight of our visit was finding the James Dorian Rooks Nature Sanctuary on Brockway Mountain, named for Jim Rooks by the Michigan Nature Association. The sanctuary includes a 1.2 mile hiking trail looping through a well-shaded woods with occasional overlooks of Lake Fanny Hooe on the edge of Lake Superior. Harsh winds from Superior create a microclimate here, favoring trees and wildflowers more prevalent in Canadian forests. In the valleys the oaks grow tall and sturdy, but on the exposed ridges they are small and stunted, like youthful oaks captured in old gnarled bodies. The understory is rich with ferns. On this July day orange fox-and-cub wildflowers showed off against the white trunks of downed birches.
     Hannah recalled that her father drew people to the outdoors of the Keweenaw Peninsula through his passion, his nature-based stories, and “his great, deep voice.”
      Jim Rooks used to walk the trails at this sanctuary. And Hannah was going there after we talked.
 

-- August 2022
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Copper mines like this burrowed as deep as 1400 feet below ground level on the Keweenaw Peninsula.
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The fateful doorway of Calumet, Michigan’s, Italian Hall is preserved to memorialize a massacre of striking miners that took place there in 1913. Seventy-three people were killed, half of them children.
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A marker on the Keweenaw Peninsula displays the annual average snowfall depth of 240 inches.
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Wildflowers and decaying birch at the James Dorian Rooks Wildlife Sanctuary.
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