Category: Landscape

A June Meditation at Houston Pond in Cornell’s F.R. Newman Arboretum

A June meditation at Houston Pond in Cornell’s F.R. Newman Arboretum, where water lilies, turtles, cattails, and summer light gather into green silence.

MichaelStephenWills8 Comments

On June 21, 2026, just after noon, Houston Pond of the F.R. Newman Arboretum held the day in a green, breathing stillness. The sun stood high over Ithaca, bright enough to polish every lily pad, every cattail blade, every glossy fold of leaf. This light of the first summer day entered the scene, becoming part of the water, part of the trees, part of the quiet intelligence of the pond.

Houston Pond

The pond was nearly covered with lily pads, a floating mosaic of green circles, some fresh and whole, others freckled, torn, yellowing. Between them, dark water opened in irregular channels, deep blue-black, mirroring trees and sky. These openings felt like pauses in a long sentence, small places where the pond allowed itself to breathe. Around the margins, cattails stood in dense ranks, upright and watchful, like a congregation listening to the sermon of light.

At the center of this water-world, white lilies opened with calm authority. Their petals rose cleanly from the surrounding abundance, white against green, flame-hearted with yellow. Each flower seemed impossible and inevitable at once: born from mud, rooted in darkness, arriving as a cup of light. A water lily is one of nature’s great acts of persuasion. It asks us to believe that beauty can rise without apology from what is hidden, tangled, and submerged.

American White Water Lily (Nymphaea odorate)

One blossom carried an unexpected visitor. A small turtle had climbed onto the flower, its dark shell resting against the white petals, one leg extended in complete confidence. The scene was both comic and profound. The lily was a raft, a chapel, a sun-warmed throne. The turtle seemed to understand what people often forget: beauty is not diminished by being used. It is completed by being entered. The flower did not become less beautiful because the turtle climbed aboard. It became more of the world.

Painted Turtle (Chrysemys picta).

Nearby, new lily leaves still held their rolled shapes, brown and burnished, rising like curled scrolls from the water. They had not yet flattened into the broad green plates surrounding them. In their tight forms was the promise of unfolding, the secret grammar of growth. Around them, older leaves floated with scars and stains, reminders that even in June’s fullness the season carries time within it. Summer is not a fixed paradise. It is motion disguised as abundance.

Beyond the pond, the arboretum rose in layers: meadow, shrubs, cattails, dark trees, open sky. A path climbed away through the greenery, pale and narrow, inviting without insisting. The woods stood dense and generous, every tree leafed out in the opulence of early summer. Clouds drifted over the blue, white and soft, their reflections briefly caught in the pond’s darker openings. The whole place seemed balanced between cultivation and surrender. Human hands had shaped the arboretum, named its paths, protected its plantings, opened it to walkers and watchers. Yet the pond itself answered in its own language: water, root, wing, shell, blossom, shadow.

Away from the broad view, the smaller flowers made their quieter claims. Tiny yellow blooms lifted themselves on fine stems among the leaves, little sparks in a green hush. White blossoms hovered behind them, half blurred, like memories of spring still lingering in the understory. A single white flower opened over sharply cut leaves, its petals simple, its center delicate with stamens. It had none of the dramatic presence of the water lilies, but it possessed a different power: the power of being almost missed.

Nipplewort (Lapsana coounis)
Canada Anemone (Anemonastrum canadense)

That is one of the arboretum’s gifts. It teaches scale. First the eye takes in the pond, the sweep of trees, the blue sky, the mass of cattails. Then attention narrows. A petal. A turtle’s foot. A torn leaf edge. A yellow flower no larger than a thought. The place asks us to look widely, then closely, then widely again. It trains the mind away from haste. It reminds us that wonder is not always a thunderclap. Sometimes it is a small white bloom waiting at ankle height.

Northern Bush Honeysuckle (Diervilla lonicera)

The yellow honeysuckle-like blossoms tucked among broad leaves offered another kind of intimacy. Their pale tubes and slender filaments seemed made for visitors more delicate than us. They belonged to the hidden commerce of June: pollinators, fragrance, pollen, fruit-to-come. Much of what matters in a place like Houston Pond happens below notice. Roots thicken. Insects navigate. Turtles choose their sunning places. Flowers open and close according to laws older than memory. The pond is never still, only patient.

Northern Bush Honeysuckle (Diervilla lonicera)

Standing there, I felt the day gather itself into one phrase: green silence, golden heart. The white lilies held the light. The cattails guarded the edges. The turtle rested without concern for symbolism. And all around, the arboretum offered its deep reassurance: life does not need to announce itself loudly to be complete.

June in the F.R. Newman Arboretum is a state of attention within a season. Houston Pond receives the sky, feeds the lilies, shelters the small dark bodies of turtles, and gives back a vision of the world refreshed by reflection. To walk there at midday is to be reminded that the ordinary is only ordinary until we stop long enough to see it. Then the pond becomes a mirror with roots, the lily a white flame on dark water, and the whole green world a quiet invitation to belong.

Click me to visit Michael Stephen Wills Online Finger Lakes Gallery.

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The Wonder of Purple-Flowered Raspberry: Nature’s Thornless Native Treasure

The purple-flowered raspberry is a native shrub that confounds expectations, combining rose-like blossoms, maple-shaped leaves, edible fruit, and thornless stems into one of eastern North America’s most enchanting woodland plants.

MichaelStephenWills10 Comments

I first encountered the purple-flowered raspberry while walking the Gorge Trail at Fillmore Glen State Park. Dry Creek murmured below, working patiently within ancient shale walls that confine its course. Waterfalls spilled from ledges overhead, cool mist drifted through the narrow passage, and sunlight filtered down in shifting patches through the summer canopy. It was a landscape dramatic enough to command all of one’s attention.

Yet it was a flower growing quietly beside the trail that stopped me in my tracks.

Purple-flowered Raspberry Growing Within Treman Gorge by the South Rim Trail

At first glance, I thought I had stumbled upon an escaped garden plant. The blossoms were  impossible to ignore—large, open, and an exuberant shade of rose-purple that glowed against the surrounding green. They seemed too extravagant for the subdued palette of a northeastern woodland. The petals had the simple elegance of wild roses, but there was something else about the plant that resisted easy identification.

The purple-flowered raspberry, Rubus odoratus, is a plant of delightful contradictions. Its blossoms are among the largest in the raspberry family, often two inches across. They appear over an extended season, beginning in early summer and continuing well toward autumn. Unlike the brief fireworks of many woodland wildflowers, this plant stages an encore performance, offering fresh blooms long after others have taken their final bow.

Over the years, I returned often to Fillmore Glen. Dry Creek became an old acquaintance, its voice changing with the seasons—boisterous after spring rains, subdued during the heat of late summer. And almost every year, somewhere along the Gorge Trail, I would encounter those same remarkable shrubs. Familiarity deepened into appreciation, and appreciation eventually became affection.

The flowers also serve a practical purpose beyond their beauty. Native bees and other pollinating insects visit them regularly, gathering nectar and pollen throughout the season. The plant has become part of an intricate ecological conversation that has been unfolding for thousands of years.

Then there are the leaves. The first time I noticed them closely, they triggered another moment of confusion. Broad and softly textured, divided into five lobes, they looked uncannily like oversized maple leaves. Some can grow nearly ten inches across, creating islands of lush greenery along shaded streambanks and woodland edges.

It is as though nature, in one of her playful moods, decided to combine the leaf of a maple, the flower of a rose, and the fruit of a raspberry.

Most raspberries and blackberries demand respect from a distance. Their prickles and thorns snag clothing and skin with equal enthusiasm. Purple-flowered raspberry breaks that expectation as well. Its stems are fuzzy rather than fierce. There are no hooked defenses waiting to punish curiosity. The plant invites close examination.

By late summer, the blossoms yield to flattened red fruits. Technically, they are raspberries, though they lack the sugary richness of their cultivated cousins. I have sampled them occasionally, appreciating them more for the experience than the flavor. Birds, however, are less discriminating. The fruits provide nourishment for wildlife, becoming another thread in the web of life that surrounds Dry Creek and countless other woodland habitats.

Native to eastern North America, purple-flowered raspberry ranges from Nova Scotia westward into Ontario and Wisconsin, extending south through the Appalachian Mountains. It thrives along forest margins, rocky slopes, stream corridors, and disturbed areas where sunlight penetrates the canopy. Through underground shoots, it gradually forms colonies that stabilize soil and provide shelter for small creatures.

It belongs exactly where I first found it. There is a temptation, especially among gardeners, to seek novelty elsewhere—to import the exotic, the unusual, the unfamiliar. Yet some of the most extraordinary plants are those that have quietly shared our landscapes all along.

The purple-flowered raspberry reminds me of this truth each time I encounter it. It teaches the value of paying attention. A hurried walk through Fillmore Glen might focus exclusively on the waterfalls, the sculpted rock formations, or the cool refuge of the gorge itself. All are worthy of admiration. But along the margins of the trail stand these shrubs, offering their own quieter marvels.

My photograph captures all flowering forms of this member of the Rose family. This specimen was blooming in August within the shade of Fillmore Glen in the Finger Lakes of New York State.

A rose-colored flower where one expects white. Maple leaves on a raspberry cane. Soft stems where thorns should be. Fruit that feeds the forest. A native plant that asks for nothing more than the chance to flourish where it has always belonged. Years after that first encounter beside Dry Creek, the sight of those blossoms still stops me as I find them in all the Finger Lakes gorges.

Certain plants become landmarks in our personal geography. They root themselves not only in the soil but in memory. The purple-flowered raspberry has become one of those companions for me—a recurring presence marking the passage of summers, a familiar face in a beloved landscape.

Dry Creek continues its patient work of carving stone. The waterfalls continue to descend in silver ribbons through the gorge. And each year, as if renewing an old friendship, the purple-flowered raspberries lift their improbable blossoms toward the filtered light. In their presence, wonder becomes less an emotion than a habit of attention.

Sometimes the greatest discoveries are not rare because they are hidden. They are rare because we have not yet learned to see them. The purple-flowered raspberry taught me to look more closely. Along a trail I thought I knew by heart, it revealed that nature still keeps delightful surprises in reserve.

Click me to visit Michael Stephen Wills Online Finger Lakes Gallery.

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From Limestone to Pasture: How the People of Inis Mór Created Soil on this Aran Island

Beneath the green fields of Inis Mór lies a remarkable story of persistence as generations of islanders created fertile soil atop bare limestone.

MichaelStephenWills17 Comments

Standing atop the cliffs of Dún Aonghasa on Inis Mór (Inishmore), one is struck by contradiction. Beneath your feet lies a landscape of exposed limestone, fractured and weathered into the unmistakable geometry of karst. These unworked, barren slopes have a pale green covering growing seemingly on air. The Atlantic crashes hundreds of feet below, while inland the island stretches toward Galway Bay in shades of gray and pale green. It seems an improbable place for agriculture.

Yet there they are: fields enclosed by dry stone walls, dotted with cattle and thick enough with grass to sustain them. Looking out across this island, a question naturally arises. Where did the soil come from?

Click the link for my Getty IStock photography of the Aran Islands

The answer is simple to describe and astonishing to contemplate. The soil of Inis Mór was, in large measure, made by human hands.

The Aran Islands are composed primarily of limestone deposited some 350 million years ago when this part of the world lay beneath warm tropical seas. The shells and skeletal remains of ancient marine organisms accumulated on the seabed and, through immense pressure and time, became stone. Today, limestone accounts for the overwhelming majority of the islands’ bedrock.

Limestone landscapes possess a severe beauty. Rainwater, slightly acidic from dissolved carbon dioxide, which in turn slowly dissolves the rock, creating fissures known as grykes separated by flat blocks called clints. Soil drains rapidly through these cracks. Left to natural processes alone, only thin accumulations of organic material develop and much of the landscape will resemble a stony pavement.

For generations, survival on Inis Mór required transforming that pavement into productive land.

Islanders gathered seaweed from the shoreline, hauling it inland by cart and hand. The seaweed provided organic matter and nutrients, particularly potassium and trace minerals. Sand from the beaches added texture and volume. Mixed together atop the limestone surface, these materials slowly decomposed into something capable of supporting plant life. Over decades—and in some places centuries—layers accumulated.

The process demanded persistence. Storms could strip away exposed earth. Atlantic winds threatened erosion. Each year required renewal: more seaweed, more organic matter, more labor. Roots from grasses and crops helped bind the developing soil together. Animal manure returned nutrients to the ground. What had begun as an artificial growing medium gradually became a living soil ecosystem.

As understood by modern soil science, soil formation is often explained through five factors: climate, organisms, relief, parent material, and time. On Inis Mór, all five are present, but there is a sixth factor impossible to ignore: culture.

Without human intervention, much of the island would likely remain dominated by exposed limestone and sparse vegetation. Instead, generations of residents imposed patience upon geology. Their work transformed an inhospitable environment into a functioning agricultural landscape.

The dry stone walls that divide the island tell the same story. Built from limestone cleared from the fields, they required no mortar. Each stone was carefully selected and placed, creating boundaries that controlled livestock, sheltered plants from relentless winds, and marked family holdings. The walls themselves became part of the ecological fabric, providing habitat for insects, mosses, lichens, and wildflowers.

Visitors often admire these walls for their picturesque quality. They are indeed beautiful and are also evidence of necessity. Every stone removed from a field made space for soil to deepen and grasses to spread. The very act of creating pasture simultaneously generated the material for the island’s defining architecture.

There is poetry in this relationship between hardship and abundance.

In many places, fertile soil is taken for granted. Deep glacial deposits or river sediments create agricultural wealth with little awareness of the thousands of years involved in their formation. On Inis Mór, however, the origins of fertility remain visible. The limestone still protrudes through the fields. The seaweed-strewn shore lies only a short distance away. The walls reveal the labor embedded in the land.

To walk these fields is to encounter a collaboration between people and place extending across centuries. The islanders did not conquer the landscape so much as negotiate with it. They worked within its constraints, borrowing from the sea to enrich the stone and relying upon time to complete what effort had begun.

The resulting landscape offers a quiet lesson. Soil, the foundation of civilization, is created through intricate interactions among rock, water, organisms, and time. On Inis Mór, soil also represents inheritance: the accumulated labor of countless individuals who refused to accept barrenness as destiny.

Viewed from the heights of Dún Aonghasa, the green fields scattered across the gray limestone are miraculous.

Not a miracle of sudden transformation, but one measured in generations—made from seaweed and sand, from patience and persistence, and from the enduring belief that even the most unpromising ground can, with enough care, be coaxed into life. 

The answer is simple hard work, hundreds, a thousand years of hauling seaweed and sand, mixing it on the barren limestone, allowing the rot of time to work. Hold it down with roots, till and refresh.

Click me for the first post of this series, “Horse Trap on Inishmore.”

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A Ride to Reavis Ranch

Some history and exploration

MichaelStephenWills16 Comments

….continued from the chapter “Desert Luxuries”

After hitching the saddled buckskin, named “Nugget,” and lightly packed pinto to trees beside the trail, The Searcher climbed up to my camp for a visit. I started water for tea and soon we were chatting. Right from the start The Searcher asked for privacy. Devoted to searching the Superstitions for the gold of the “Lost Dutchman Mine,” he organized his expeditions from a staging point near Phoenix and spent nearly sixty days each year in the wilderness. Part of his preparation was a desert survival course provided by the Reavis Mountain School, conducted by Peter Bigfoot.

An Invitation from The Searcher

The Searcher described a place near Pine Creek, he called it “Circlestone,” a large, almost perfect circle of precisely fitted stone walls, on the slopes of Mound Mountain above the headwaters of Pine Creek. My sister, Diane, and I found Circlestone on backpack expeditions March and November 2006. WThe site exceeded our expectations, the walls appeared less built than patiently persuaded from the mountain itself.

Here is a panorama from March 2006, southwest from the forests of juniper and pinion on the slopes of Mound Mountain.. The southern tip of Reavis Valley is to the right, from there Arizona Trail lead to White Mountain in the distance. It was taken on a later trip, in November of 2006 when my sister, Diane, and I visited Circlestone.

Click any photograph for a larger image.

The Searcher also told of Elisha Marcus Reavis, who settled the Valley west of Pine Creek in 1874. At one point, a band of Apaches planned to kill Reavis, but were respectful of his reputation as a rifle shot. They were waiting him out across from the his dugout, when Reavis stripped naked and, with wild hair and a flaming red beard, charged their camp, knives in both hands. The Apaches rode off, wary of his insane behavior, and never bothered him again.

We talked about my prospects and plans when The Searcher offered to take me to the Reavis Valley the next day, on horseback. There is a large apple orchard there and, this being April, we’d be treated to masses of apple blossoms. The day after Reavis Ranch, I could pack out with him down the Arizona Trail, past the Reavis Mountain School, over Campaign Creek and drive back to the Lost Dutchman Park. I readily agreed.

To Reavis Ranch on Horseback

The following morning rose slowly from colorless darkness, accompanied by thin birdsong and the whitening glow of high clouds. When the Searcher arrived around 8 am he was leading the pinto, introduced as Colorado, equipped with a western saddle instead of a pack. As an absolute novice trail rider, I rode while The Searcher held Colorado’s lead rope. The reins were wrapped around the saddle horn, leaving me to hang on and enjoy the view and the swishing tail of Nugget, the buckskin.

The 2.5 mile trail to Reavis from Pine Creek is typical of the eastern Superstitions, minimally improved, dramatically uneven, littered with boulders polished smooth by decades of hooves, floodwater, and erosion. From Pine Creek there’s a climb of a 631 feet to a 5,278 foot elevation, where the trail meanders beneath a dramatic red cliff with a view of the pinyon/juniper forests on the slopes of Mound Mountain. As he picked our way, The Searcher pointed out the sights. “Circlestone is somewhere over there, a ring of stones overgrown with Alligator Juniper.” I could do little more than observe; photography was entirely out of the question. The trail twisted around the mountain like a dry stream remembering water.

A cliff along the trail to Reavis Ranch offered the ledges and shadowed cover preferred by cougars. In daylight it posed little danger to mounted riders, and attacks against horses were rare. In all our years in Arizona, neither of us had seen more than the tip of a tail slipping behind brush.

This had been a lush April after a wet winter, and small game was plentiful. Only a sick cat would have been desperate enough to stalk horses. The darker possibility—a cougar infected with rabies after encountering a diseased animal at a water source—was a thought neither of us lingered on for long.

Eventually, the path descended steeply to Reavis Creek, the valley floor and intersected with the Reavis Ranch trail. Heading south the Reavis Ranch trail passes the site of a long abandoned ranch. What remained of the adobe and stone ranch house stood on a level bench overlooking what had once been the corral and a broad open meadow.

Open field at near the juncture of the trail from Pine Creek with the Reavis Ranch trail.

Apple trees in bloom sween from the former site of the ranch house. There used to be a pond near this spot. With a little imagination, the trail from Pine Creek can be seen on the far ridge.

Reavis Ranch Trail, foreground, traverses the valley length north to south. The Arizona Trail from Pine Creek following below the red rock cliffs in the distance.

The US Forest Service razed the building after it “burned to the ground” Thanksgiving 1991. I would not call what is left “a foundation,” it is a platform where the house stood. In the photograph, the surviving tiles still suggest the modest warmth of a lived-in home. I’ve seen old photographs of the structure with a large pond to the left of this view, a door and simple porch face east and the pond used to hold irrigation water. The leveled ruin possessed the melancholy geometry of abandoned human hope.

Turning from the ruin, another structure came into view. Built into the western slope above the valley floor was a hexagonal adobe foundation overlooking the remains of the ranch house across the trail.

My interpretation rests partly on the surrounding terrain. South of the structure runs the shallow trace of an excavated canal, suggesting that water from upper Reavis Creek—or one of its tributaries—was diverted into a catchment basin before being stored or directed toward irrigation.

Whatever its exact purpose, the site commands sweeping views of the central valley and is a beautiful place to watch evening settle over the orchard.

Turning from the ruin, another structure came into view. Built into the western slope above the valley floor was a hexagonal adobe foundation overlooking the remains of the ranch house across the trail.

The Searcher led me to a place a few hundred yards south, in a narrowing of the valley, where he let Colorado and Nugget roam free. The horses appreciated the level, open spaces and I enjoyed the Ponderosa pines on the west valley slope. We sat on the smooth trunks of fallen trees, 4 feet in diameter, near Reavis Creek.

Colorado took this opportunity to bolt, headed south. We took off after him into and through a thicket of locust trees where The Searcher cornered Colorado to regain control. “He was abused by a previous owner and can be difficult at times” was how The Searcher put it.

We were close to the end of Reavis Valley where Reavis Creek originates from the drainage of White Mountain, to the west.

We headed north here, back to the ranch house site, to the lush new grass of the apple orchard.

Nugget in Horse Heaven

Nugget grazed, tethered with plenty of slack, with the calm assurance of an animal that knew it had arrived in horse heaven. This photograph of the pair shows their personalities, Colorado edgy, Nugget content to feast while the grass is available. The orchard grass rolled in waves around their legs like green water beneath anchored boats.

Colorado on the alert while Nugget grazes, typical of their personalities.

Click me for the next post for photographs and more history of this Apple Orchard in the Superstition Wilderness.

Click me to visit Michael Stephen Wills Online Finger Lakes Gallery.

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McLean Bogs in Early Spring: Pitcher Plants, Skunk Cabbage, a Quiet Walk with Grandchildren

A quiet early spring walk through McLean Bogs reveals pitcher plants, skunk cabbage, and the subtle beauty of glacial wetlands shared with grandchildren.

MichaelStephenWills14 Comments

The path into McLean Bogs begins without ceremony, a narrowing of the world. The road falls away, the trees gather closer, and the ground softens underfoot, remembering water. You arrive at a threshold. The air seems altered, quieter, carrying a faint mineral stillness, as though the glacier that shaped this place has not entirely withdrawn its presence.

McLean Bog, Tompkins County, New York State part of Cornell Botanical Gardens

The pond holds the sky with patient fidelity. Its surface is dark, reflective, contemplative—mirroring a band of bare trees and the pale sweep of early-spring cloud. Nothing disturbs it. No wind, no bird, no ripple of urgency. It is the kind of water that asks nothing of you except attention. And in giving it, you feel the pace of your own thoughts begin to slow, as if they too must match the bog’s ancient tempo.

At the edge, grasses stand in muted gold, last year’s growth bowed but not broken. They frame the water as do an unfinished sentence. You can imagine how, in another month, this quiet will be interrupted by green—by the rising insistence of life. But today, the landscape is held in suspension, between endings and beginnings.

On the boardwalk, my grandsons, Sam and Rory, find what the place offers most readily: evidence. A small gray pellet of fur and bone delicately assembled and then discarded. Nearby, a twisting length of scat, marked with the unmistakable language of survival. These are not the symbols we teach in books, but they are legible all the same. The boys lean close, curious, unbothered by what adults might turn away from. To them, this is not unpleasant—it is a clue, a message left behind by an unseen life moving through the same narrow corridors of forest and marsh.

There is something honest in that exchange. The bog does not disguise itself. It offers no curated beauty, no ornamental flourish. What it gives instead is continuity—the quiet assurance that life persists in forms both delicate and stark. And the children, without pretense, receive it as it is.

Deeper in the woods, a small structure of branches rises against the trunk of a tree, a lean-to, improvised and incomplete. Its architecture is simple, almost instinctive, a tentative answer to the question of shelter. Sam and Rory stand before it, boots sunk slightly in the soft ground, their bodies close together in that unconscious gesture of kinship. One leans into the other, not for support exactly, but for connection.

Behind them, the forest extends in gray and brown, a lattice of trunks and fallen limbs. It is not the lush abundance of summer, but something more revealing—a stripped-down anatomy of place. Here you see the bones of the landscape, the structure beneath the surface. And in that exposure, there is a different kind of beauty, one relies on form, on persistence, on time itself.

The boardwalk carries you out into the open bog, where the ground gives way to water and moss. It is a narrow path, elevated just enough to allow passage, and it bends gently, as though respecting the terrain rather than imposing upon it. Rory walks ahead, small against the expanse, following the curve without question. There is trust in that movement—the simple faith that the path will hold, that it leads somewhere worth going.

The path is flooded
Your task: find pitcher plants in the middle distance

Around you, the bog stretches in subtle variation. Patches of standing water reflect a green that seems almost improbable in this season, the work of mosses and algae that thrive where others cannot. The vegetation is low, dense, textured—a mosaic rather than a meadow. And here and there, like small embers against the muted field, the pitchers rise.

The pitcher plants are both beautiful and unsettling. Their deep red forms, veined with intricate patterns, hold themselves open to the world. They are vessels, yes, and thresholds, invitations with consequence. Insects, drawn by color or scent, enter and do not leave. It is easy to think of them as passive, but they are anything but. They are active participants in the exchange of life, taking what the poor soil cannot provide.

You kneel to look more closely, drawn in despite yourself. The interior of the pitcher is a map of intention—every line, every curve serving a purpose. And yet, there is an elegance to it, a precision that feels almost artistic. It is not cruelty, exactly, but necessity rendered with a kind of quiet grace.

McLean Bog, Tompkins County, New York State part of Cornell Botanical Gardens

Elsewhere, the first signs of skunk cabbage emerge, their dark, curved forms pushing through saturated ground. They are early risers, indifferent to cold, generating their own heat to break through frost. They do not wait for spring; they create their own version of it. Scattered across the forest floor, they resemble a field of small, listening shapes—each one a declaration that life does not always arrive gently.

And so you move through the bog as a participant in its slow unfolding. Sam and Rory run ahead, then return, their boots muddy, their hands full of nothing in particular. They do not need to name what they have seen. The experience is enough.

As we return to the preserve edge, this sign stands—formal, declarative, assigning significance in the language of designation: Registered Natural Landmark. This place is important, rare, worthy of protection. But the words feel almost secondary after what you have just walked through.

McLEAN BOGS has been designated a REGISTERED NATURAL LANDMARK

This site possesses exceptional value as an illustration of the nation’s natural heritage and contributes to a better understanding of man’s environment.
National Park Service, United States Department of the Interior 1973.

Because the true measure of McLean Bogs is not in its classification, but in its effect. It changes the rhythm of your thinking. It draws your attention downward—to the ground beneath your feet, to the subtle movements of water and growth, to the quiet negotiations of life that continues with or without witnesses.

And perhaps that is what Thoreau meant, though he said it more simply: that heaven is not only above us, distant and abstract, but also here, immediate and tangible, woven into the fabric of the earth itself.

In the bog, that idea does not feel like metaphor. It feels like observation.

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Where Winter Yields: Skunk Cabbage, Pitcher Plants, and Milky Ice at Malloryville Preserve

A late winter walk through Malloryville Preserve reveals milky ice, emerging skunk cabbage, and hidden wetland life—seen through the curious eyes of grandchildren.

MichaelStephenWills9 Comments

The morning began in that quiet register peculiar to late winter in the Finger Lakes—when the calendar insists on spring, yet the land, still half-claimed by frost, speaks in a more cautious dialect. At the O.D. von Engeln Preserve at Malloryville, the woods held both seasons in tension. Snow lingered in shaded hollows, while the exposed ground, damp and rust-colored, breathed with thaw.

Sam and Rory—boots muddied almost immediately—climbed atop a great, weathered stump, its cut face fanned with the geometry of years. There is something about a stump that invites children upward, as though it were not a remnant but a stage. From their perch they surveyed a kingdom of bare trunks and quiet trails, their laughter momentarily lifting the stillness. Behind them, the forest rose in gray-brown columns, and beneath them, the history of a tree—rings like a clock no one can wind backward.

We moved downslope toward the seepage-fed lowlands that give this preserve its particular character. Here, the ground softens, water gathers, and winter lingers longer in pockets of ice that seem reluctant to relinquish their hold. The ice itself told a story—not clear and crystalline, but cloudy, milky, almost opalescent. This opacity is the signature of trapped air, minute bubbles frozen in suspension as water repeatedly melts and refreezes. Each cycle interrupts the orderly lattice of ice, scattering light and transforming transparency into a pale, diffused glow. It is ice that remembers its instability.

Threading through this ice were narrow rivulets of meltwater, tracing paths around moss-covered hummocks. These islands—bright green even in winter—rose like miniature continents in a frozen sea. On one such hummock, we found this skunk cabbage. Its mottled spathe, deep maroon flecked with yellow, pushed upward through the cold, its form both alien and ancient. I pointed out to the boys that this plant generates its own heat—a metabolic furnace capable of melting the surrounding snow. It is one of the earliest heralds of spring, though it announces itself not with color alone, but with scent—a pungency that walked with us that day.

Nearby, nestled in the sphagnum, were the pitcher plants—Sarracenia purpurea—their tubular leaves tinged with winter’s reds and greens. Even in dormancy, they held their form, each pitcher a small reservoir. I explained how these plants supplement the nutrient-poor conditions of the bog by capturing insects, their modified leaves forming a subtle trap. The boys leaned in, curious, perhaps imagining the unseen dramas that would unfold here in warmer months.

The North American genus Sarracenia are the trumpet pitchers, which have a more complex trap than Heliamphora, with an operculum, which prevents excess accumulation of rainwater in most of the species.

The wetland was a place of plants and textures. The ice thinned near the edges, revealing water beneath that reflected the vertical lines of trees above. Droplets fell intermittently from branches, punctuating the quiet with soft, irregular taps. It was a landscape in transition, each element negotiating its passage from one state to another.

Along a tangle of shrubs, I noticed an unusual growth—a dense, broom-like cluster of twigs protruding from what appeared to be a highbush blueberry. This “witches’ broom” is often the result of fungal infection or other physiological stress, causing the plant to produce a profusion of shoots from a single point. To a child’s eye, it might seem like a bird’s nest or some deliberate construction, but it is, in fact, the plant’s own altered architecture—a distortion that nonetheless becomes part of the ecosystem, offering shelter to small creatures.

Further along, a fallen log bore the layered forms of shelf fungi, each bracket extending outward like a series of pages half-opened. Their colors—muted tans and browns—blended with the wood, yet their structure was unmistakable. These polypores are the quiet recyclers of the forest, breaking down lignin and cellulose, returning the substance of the tree to the soil. I ran my fingers lightly along their surface, feeling the fine texture, while the boys, less cautious, tapped them as though testing their solidity.

On the bark of a nearby tree, we encountered a patch of what looked like pale, fuzzy insulation—the egg mass of the spongy moth. I explained that each of these masses could contain hundreds of eggs, waiting for the warmth of spring to hatch. It was a reminder that even in this subdued season, the next wave of life was already prepared, concealed in plain sight.

As we made our way back, the boys’ boots squelched in the soft ground, their earlier perch on the stump now a distant memory. Yet the morning had offered them—and me—something more enduring than a climb. It had revealed a landscape in flux, where ice is not merely frozen water but a record of change, where plants defy cold through chemistry, and where even decay participates in renewal.

Late winter, in a place like Malloryville, is not an absence of life but a study in persistence. It asks for attention, for patience, and for a willingness to see beauty in transition. Walking with Sam and Rory, I was reminded that discovery does not wait for spring. It is already here, written in ice, moss, and the quiet industry of the forest.

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The Science and Poetry of Melting Ice: Cayuga Lake During a Winter Thaw

Under a blue February sky, Cayuga Lake keeps its icy grip, revealing how light, time, and physics conspire to make winter’s farewell a slow, luminous negotiation.

MichaelStephenWills8 Comments

These photographs, made along the frozen margin of Cayuga Lake at Cass Park in mid-February 2026, carry a quiet paradox. The sky is a lucid blue, the light has that late-winter clarity that hints at spring, and yet the lake remains locked under a pale, glassy skin. A few geese stitch the air. A bench waits. Red and white beacons stand where water should be moving. The moment is fixed: late afternoon light in February, Finger Lakes winter—but the deeper story is written in physics, not pixels: why does lake ice linger so stubbornly during a thaw?

The short answer is that water is a hoarder of heat and ice is a keeper of promises. The long answer is the reason these scenes feel suspended between seasons.

Start with the cost of melting itself. Ice does not simply warm into water; it must first be converted, and that conversion demands a large, fixed payment of energy known as the latent heat of fusion. To melt just one kilogram of ice takes about 334,000 joules—and that energy raises the temperature not at all. It is spent entirely on changing solid to liquid.

Scale that up to a lake surface and the numbers become sobering. Even a modest sheet of ice—say ten centimeters thick—contains roughly ninety kilograms of ice per square meter. Melting that much requires on the order of thirty million joules per square meter. To put this in a human context, in 1 kcal there are 4,184 joules. Melting a square meter of ice requres 7,170 kilocalories (kcals) or 3.6 days for a person expending 2,000 kcals per day. Spread across square kilometers of lake, the energy bill climbs into the tens of terajoules. That is the hidden arithmetic behind the familiar disappointment of a February thaw: a few warm days feel dramatic to us, but to a lake they are only a small down payment.

This leads to the second, more subtle constraint: melting ice keeps itself cold. As long as ice is present, the surface of the lake is pinned near 0 °C (32 °F). Incoming heat does not make the surface warmer; it simply converts more ice into water at the same temperature. The thin layer of meltwater that forms on top is also near freezing, so the entire interface remains locked at winter’s threshold. There is no “warming momentum” here—no quick rise in temperature to accelerate the process. The system quietly consumes energy without changing its outward thermal expression.

That is why the lake in these images can look bright and almost springlike while remaining physically winterbound. Sunlight is being spent on erasure, not on warming.

A third rule of water deepens the delay. Freshwater is densest not at freezing, but at about 4 °C (39 °F). In early spring conditions, the coldest water—near 0 °C—floats. The slightly warmer, denser water below tends to stay below. This creates a stable stratification: a cold, near-freezing surface layer sitting like a lid on the lake.

The consequence is crucial. The lake cannot easily mix warmer subsurface water upward to attack the ice from below. The thaw must work mainly from the top and the edges—where sunlight, mild air, rain, and shoreline heat can do their work—rather than through a coordinated, whole-lake turnover. In practical terms, the ice is dismantled by margins and seams, not by a sudden, uniform collapse.

Add to this the reflective nature of ice and snow. The pale surface in these photographs is not merely beautiful; it is also defensive. Bright ice and snow reflect a significant fraction of incoming sunlight back into the sky. Dark, open water would absorb that energy eagerly and warm quickly. As long as the lake remains light-toned, it is actively rejecting some of the very energy that could hasten its release.

Thickness and structure matter too. Winter does not lay down a single, simple sheet. It builds layers: clear black ice, milky refrozen crusts, snow-ice composites, trapped bubbles—each a page in winter’s ledger. A brief thaw may soften the surface, open a lead near shore, or trace fine cracks across the sheet, but the bulk remains. In the closer views—the lighthouse and the red beacon standing in frozen sheen—you can see subtle tonal shifts and faint stress lines, the calligraphy of slow change. These are signs of negotiation, not surrender.

Scale, finally, is destiny. Cayuga is long and deep; it behaves more like a small inland sea than a pond. Small waters can change their minds quickly. Large waters are conservative. They remember. The heat they lost in autumn must be repaid, carefully and in full, before winter loosens its hold. This is why harbors and shallows darken first, why the margins in these scenes show hints of movement while the center keeps its pale composure.

Put together, these rules explain the peculiar patience of February ice. The thaw is not a switch but an accounting. Enormous quantities of energy must be delivered just to accomplish the phase change. While that work is underway, the surface temperature barely moves. The cold meltwater stays on top, limiting mixing. The bright surface reflects sunlight. The lake, in effect, resists haste through the ordinary, unromantic laws of physics.

There is an austere beauty in this. Ice is a temporary architecture built by the loss of heat, and its demolition requires an equally disciplined repayment. The quiet in these images is the quiet of bookkeeping—joules being transferred, layers being undone, thresholds being approached but not yet crossed. When the change finally comes, it often feels sudden: a windy day that breaks the sheet into plates, a warm rain that darkens the surface, a week when the margins retreat visibly. But that drama is only the visible last act of a long, invisible exchange.

So the lake lingers. Not out of stubbornness, but out of fidelity to the rules that govern it. Under a sky that already looks like April, Cayuga is still paying winter’s invoice. The ice remains until the account is settled—and when it finally goes, the benches will no longer face a mirror of light, but a moving field of dark water, ready once again to begin the long work of storing heat for another year.

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Stones That Traveled: Glacial Erratics, Deep Time, and the Stories They Leave Behind

Glacial erratics are immigrant stones—carried south by ice, dropped without explanation, and left behind to challenge our sense of permanence, place, and deep time.

MichaelStephenWills22 Comments

There are rocks that merely sit where gravity has placed them, and then there are rocks that arrive with stories already embedded—foreign syllables carried south on ice, dropped without explanation, and left for us to puzzle over. Glacial erratics belong to the second category. They are migrants with no passports, refugees of deep time, whose presence quietly contradicts the landscape that hosts them.

Long before anyone reached for a hand lens or an ice-flow diagram, people answered such contradictions with imagination. In Ireland, a boulder perched just so on a mountain side is not a geologic problem but a resting place. Leprechauns, we are told, favor such stones—high enough to observe human intrusion, solid enough to outlast it. Skepticism, as folklore reminds us, is not always a stable position. Kevin Woods—better known as McCoillte—found that out the hard way when doubt collided with experience on the slopes of Slieve Foye. What followed was not merely a conversion story, but an act of modern mythmaking: folklore translated into bureaucracy, imagination petitioning regulation, and “The Last Leprechauns” entering the unlikely language of conservation. Stone, story, and belief hardened together into something oddly durable.

Rocks such as this are a favorite perch for leprechauns to rest and contemplate the works of man who have invaded their world. Inhabitants of Carlingford who wander Slieve Foye have come upon them often enough, their stories and certitude in the existence of the Little People are resistant to manifold doubters with their reasons and arguments. Kevin Woods, aka McCoillte, was a doubter until worked on a stone wall on property he owned on Ghan Road, Carlingford. His belief did not arise on the discovery of the leather purse, covered with ages of dust and lime, nor with the gold coins inside. McCoillte pocketed the coins for luck. As luck would have it, McCoillte loved to walk on Slieve Foye. It was on one such walk he and his dog encountered Little People who paralyzed them to escape. His unexplained absence led to troubles with the wife. This experience brought McCoillte around to enough of a belief that he, with lots of help, succeeded in petitioning the E.U. European Habitats directive to recognize leprechauns a protected species. A reserve was establish on Slieve Foye to protect the “Last Leprechauns” and you can google this phrase to learn more about McCoillte’s stories.

Back in the Finger Lakes, we tend to use a different grammar when confronted by an out-of-place rock. We name it, classify it, and trace its lineage northward. Erratics scattered across Tompkins County are geological sentences that begin somewhere else entirely. The bedrock beneath Ithaca—Devonian shale and sandstone—cannot account for crystalline intruders left behind like forgotten punctuation marks. These stones speak of ice sheets thick enough to erase valleys and decisive enough to transport mountains in fragments.

Some of those fragments have been domesticated. Cornell, for example, has never been shy about rearranging its stones. An unremarked erratic along the Allen Trail may once have been shrugged off as inconvenient rubble, while another—dragged from the Sixmile Creek valley—was carved into a seat and made eloquent. The Tarr memorial boulder, resting near McGraw Hall, transforms erratic stone into deliberate monument. It invites rest, contemplation, and perhaps gratitude for those who taught us how to read landscapes written by glaciers.

We find boulders of crystalline rock, commonly derived from Adirondack sources, left behind on the surface of ablation moraine, in the Finger Lakes Region. Cornell finds some and move them, maybe the case for this unremarked erratic found along the Allen Trail of FR Newman Arboretum. Another enormous erratic, brought in from the Sixmile Creek valley, was carved into a seat as a memorial to Professor R.S. Tarr who deciphered much of the glacial history of the Finger Lakes Region. Find it at the southwest corner of McCraw Hall on the Cornell University Campus. Reference: “The Finger Lakes Region: Its Origin and Nature,” O.D. von Engeln, Cornell University Press, 1961 page 106

Glacial Erratic, Fillmore Glen

Elsewhere, erratics remain defiantly themselves. In winter, one along Fall Creek alternates between anonymity and revelation, depending on whether snow smooths its surface or retreats to expose lichen constellations. Bridges pass overhead, traffic flows, semesters turn over, yet the rock remains unimpressed. It has already endured pressure sufficient to rearrange its crystals; a passing academic calendar is not likely to trouble it.

Glacial erratic with and without a snow covver and spotted by lichen along Fall Creek in a winter afternoon as seen from Cornell Botanic Gardens. That is the bridge over Fall Creek on Forest Home Drive. Cornell University, Ithaca, Tompkins County, New York State

Closeup of the same boulder

This boulder, a glacial erratic, was found near Fall Creek and the Cornell Botanic Gardens Horticulture Building. Cornell University, Ithaca, Tompkins County, New York State

This rock, a glacial erratic, was found near Fall Creek and the Cornell Botanic Gardens Horticulture Building. Cornell University, Ithaca, Tompkins County, New York State

Then there are the stones that confront us most directly—those we stumble upon in fields, pulled from soil by plow or frost, demanding explanation. A white, iron-stained marble boulder in a Tompkins County field is not subtle about its foreignness. It does not belong to the local vocabulary of shale and sandstone. Its pale surface, crystalline texture, and mineral scars point insistently north, toward the Grenville terrane of the Adirondack Lowlands. The Balmat–Edwards–Gouverneur marble belt offers the most persuasive origin story: metamorphosed carbonate rock carried south by Laurentide ice, released when climate and physics finally lost patience with one another.

I found this white marble erratic in a Tompkins County field. The highest-probability source is Grenville marble from the NW Adirondack Lowlands / St. Lawrence County (Gouverneur/Balmat–Edwards marble belt), delivered by southward-flowing Laurentide ice. I say the most probable source is metamorphosed carbonate (marble) from the Grenville terrane to the north—especially the northwest Adirondack Lowlands / St. Lawrence County marble belt (the “Gouverneur Marble” and related Grenville marbles), transported south by the last Laurentide ice sheet. Why that’s the best bet: Ice-flow geometry favors a northern source. In the Finger Lakes, glacial ice advanced with a flow direction that was very close to due south, guided by the north–south bedrock valleys. Tompkins County erratics are “exotic” imports. Local bedrock around Ithaca/Tompkins is Devonian shale/sandstone, but the region contains many nonlocal (“exotic”) glacial erratics carried in from much farther north (including southern Canada and beyond). Marble isn’t local to the Ithaca area, but it is abundant in the NW Adirondack Lowlands. The Balmat–Edwards/Gouverneur area in St. Lawrence County is a classic Grenville Lowlands district with marble belts (the same province that yields cream/white building marble around Gouverneur).

What makes this particular erratic compelling is not just its provenance, but the improbability of its journey. Ice moved with purpose here, flowing south along bedrock valleys like Fall Creek and Cayuga troughs, turning the Finger Lakes region into a conveyor belt for distant geology. When the ice melted, it left behind evidence that refuses to blend in. Erratics are geological truth-tellers. They announce that this place was once unrecognizable, that what seems permanent is merely provisional.

Perhaps that is why folklore clings so naturally to stone. Whether leprechauns or Laurentide ice are credited, erratics insist on a larger frame of reference. They ask us to imagine landscapes in motion and beliefs under revision. A boulder can be a seat, a marker, a perch, or a puzzle—but never merely background. It waits, quietly confident, for us to catch up to its story.

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Lucifer Falls in Winter: Traversing Ice Chutes Along Ithaca’s South Rim Trail

A careful winter walk along the South Rim reveals Lucifer Falls transformed—ice chutes, frozen veils, and flowing water beneath stone, inviting patience, attention, and quiet awe.

MichaelStephenWills15 Comments

January pares the gorge to essentials. Color withdraws, sound sharpens, and the land reveals its underlying grammar—stone, water, cold, and time. Reaching Lucifer Falls by the South Rim Trail on a winter morning feels less like an initiation, a careful passage through ice-chutes and shadowed ledges where the creek rehearses its ancient work in a new key.

Wintertime scene along the South Rim Trail of Robert H. Treman State park. The trail is solid ice. Ithaca, Tompkins County New York State

The trail begins quietly, a soft crunch underfoot where snow thins to leaf litter. Hemlocks hold their breath. The gorge opens in increments, not all at once, and the creek’s voice arrives in fragments—first a whisper, then a steady insistence. Winter edits the landscape with a clean hand. The clutter of summer understory is gone; what remains is structure: stratified shale stacked like a book left open to a single, patient chapter. Every footfall demands attention. Ice slicks the stone where seeps cross the path, and the trail teaches a winter gait—short steps, weight centered, the quiet confidence of traction earned rather than assumed.

As the rim narrows, the air cools perceptibly. The gorge walls rise higher, their layered faces stippled with frost and snow. Icicles form a punctuation along ledges, commas and exclamation points caught mid-sentence. In places, the trail descends into ice chutes—steep, polished corridors where meltwater has glazed the rock. Here, the body listens more closely. Boots test, then commit. Hands brush the cold bark of a leaning tree, a borrowed handrail. There is pleasure in this concentration, the way winter insists on presence. You cannot hurry. You cannot drift.

Below, the creek widens into a quiet pool, its surface a muted mirror. Thin plates of ice drift and collide, sounding a faint porcelain clink. The sound carries upward, amplified by the gorge’s acoustics, a delicate counterpoint to the deeper hush of falling water. The trail curves, and suddenly the falls announce themselves—not in full view, but as a white presence beyond the bend, a brightness lodged between walls of stone.

The trails this day were solid ice. I arrived via the South Rim Trail, the only way to access this site. Robert H. Treman State Park, Ithaca, Tompkins County, New York State

Approaching from the South Rim offers a measured reveal. First the upper cascades appear, water fanning across rock that has become a winter canvas. Ice has claimed the margins, building ribs and curtains that thicken day by day. The falls do not stop in January; they change. Water threads through ice, slips behind it, emerges again in translucent veils. Gravity persists, but its expression is altered—slower, more deliberate, sculptural.

At the base, Lucifer Falls stands transformed. The familiar plunge has become a tiered architecture of frozen flow, a stepped amphitheater where icicles hang like organ pipes and snow pillows settle into hollows. The water still moves, a silver ribbon finding its way down the left flank, while the right side has grown into a cathedral of ice. The gorge walls close in, amplifying the sound—a low, resonant murmur that feels as much felt as heard.

The cold sharpens every sense. Breath fogs, then clears. Fingers tingle through gloves as the camera comes out, metal biting through insulation. Framing becomes an act of translation: how to honor motion when much of it has paused; how to suggest the hidden currents beneath the frozen skin. A short video will later catch what stillness cannot—the soft shiver of water behind ice, the way the falls breathe even in winter—but for now, the eye lingers on texture and line. Shale layers echo the ice’s striations. Time repeats itself in different materials.

Standing there, it’s impossible not to feel the weight of deep history. These rocks remember glaciers and warmer seas; this creek has been at work since before memory had a word. January merely adds a chapter. Snow feathers the ledges. A stray sunbeam slips into the gorge, briefly igniting the ice, and then is gone. The falls return to their monochrome palette, as dignified as an old photograph.

The return along the rim is lighter, the path now familiar, confidence earned. The ice chutes yield more easily on the way back, as if acknowledging the careful passage. Above the gorge, the forest resumes its quiet, and the trail leads out into the open day. What lingers is the sense of having witnessed something intimate and exacting—a winter conversation between stone and water, conducted without haste, inviting those willing to slow down and listen.

January asks little and gives much. Reaching Lucifer Falls by the South Rim is a reminder that beauty is not diminished by cold; it is clarified.

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Where Fall Creek Turns: An Esker’s Quiet Authority in Malloryville Preserve, New York

An ancient esker redirects Fall Creek at Malloryville Preserve, revealing how Ice Age meltwater shaped the land and still quietly governs water and wandering feet.

MichaelStephenWills16 Comments

The esker rises like a glacier’s spine, a long-backed remnant left behind where an ice mountain learned how to leave quietly. It is not loud geology—no cliffs shouting their age, no cataracts announcing force—but a patient, sinuous fact. A frozen river’s footprint, pressed into the land and then abandoned, it lies there still, grading itself gently on both sides, as if unwilling to offend gravity or time.

At first glance, it could pass for a human thing: a railroad berm, a raised roadbed, an engineer’s solution. Yet this ice-scribe ridge was shaped without blueprints, drafted by meltwater racing beneath a retreating glacier, carrying gravel like a hoard of stories. The stones settled where the ice allowed them, stacked by pressure and patience, forming a ridge long enough—nine-tenths of a mile—to tell a stream where it must turn.

Fall Creek meanders through the esker fields of the Malloryville Preserve. Here is the view from an abandoned railroad bridge. The preserve is near Freeville in the Finger Lakes Region of New York State.

Fall Creek arrives with purpose, confident in its descent, until it meets the esker and must reconsider. Here the water performs bows, an abrupt acknowledgment of authority. The creek becomes a liquid negotiator, redirected by the ridge’s quiet insistence. This is the esker’s work: not domination, but persuasion. Land teaching water a new sentence.

This video provides a better feeling for the esker. To do this from WordPress Reader, you need to first click the title of this post to open a new page.

Standing at the foot of the esker, the slope to the right reveals itself slowly. It does not announce, I am important. Instead, it waits to be noticed. A swamp settles nearby, the water-mirror lowland, collecting what seeps and lingers. Together, ridge and wetland form a conversation: height and hollow, drain and gather, spine and lung.

Before there was signage, before placards translated glacial grammar into public language, the land already knew itself. Knowledge preceded explanation. My son and I pitched a tent atop a kame at our front door — another ice-left hill, a deposit of ancient momentum. That night, the ground beneath us was older than memory and younger than myth. Camping there was not recreation so much as apprenticeship.

A kame is a meltwater’s knuckle, rounded and abrupt, shaped by collapse rather than flow. To sleep upon it is to rest on uncertainty made solid. The tent fabric whispered in the breeze, a thin membrane between human breath and glacial aftermath. Fireflies stitched brief constellations above the grass, while the earth held fast, remembering ice that no longer needed remembering.

Walking along Fall Creek later, watching it turn west where the kame insists upon geometry, one begins to sense the land’s authorship. This is not random scenery. It is edited terrain. Each ridge, each bend, each saturated hollow is a sentence left behind by ice that once covered everything and then, mercifully, withdrew.

The esker itself is a time-ladder, inviting slow ascent. Step by step, gravel shifts underfoot—rounded stones, carried far from their origins, now loyal to this place. Each stone is a traveler without a passport, naturalized by pressure and pause. Together they hold their line, resisting erosion not by hardness alone, but by collective agreement.

From above, the ridge reveals its length, its deliberate curve. It does not hurry. It does not apologize. It simply is, a memory ridge, reminding the present that absence can be as powerful as presence. The glacier is gone, yet its handwriting remains legible.

Overflow from a Kettle Pond threads through a meadow before feeding Fall Creek. The O.D.von Engeln Preserve at Malloryville.

In the nearby swamp, water pools in dark reflection. Frogs tune their throats. Sedges write vertical poetry. This is the after-ice sanctuary, where meltwater’s descendants linger and life reclaims the margins. The esker drains; the swamp receives. Between them flows a balance older than names.

To walk here is to practice a different kind of attention. The land does not reward speed. It rewards listening. The ridge asks you to follow its curve, to feel how it shapes movement, how it choreographs water, wildlife, and wandering humans alike. It is a path-without-intention, yet it guides all who encounter it.

Long after the tent is folded, after the creek continues its bent course, after the placards fade and are replaced, the esker will remain. It will continue directing water, lifting footsteps, and teaching geometry to anyone willing to notice.

Eskers and kames are the glacier’s farewell letter, written in gravel, signed by time, and left open for reading.

Click Me for the first post of this series.

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