Category: Rivers, Streams, Creeks

Fens, Bogs, and Flowing Water of Malloryville Preserve of Freeville, New York

Discover Malloryville Preserve in Freeville, New York—a hidden Finger Lakes wetland of fens, bogs, and flowing water where glacial history and rare plants meet.

MichaelStephenWills5 Comments

Water defines the O.D. von Engeln Preserve at Malloryville long before we see or hear it. At first, it is only a dampness in the air, a coolness at ankle level, a dark sheen between sedge tussocks. In the space of a half-hour walk, we pass through fen, bog, marsh, and swamp, each distinct, yet bound together by the same slow, persistent flow.

Here we are traversing a swamp, our steps buoyed along on planking made from recycled plastic. The boardwalk floats visually above pools the color of tea, edged with moss and skunk cabbage. It’s easy to imagine what this crossing would have been like before the planks were laid—boots sinking, knees splashed, delicate plants crushed. The modern walkway is a quiet compromise: we may enter this saturated world without trampling it, a human gesture that matches the preserve’s ethos of protection and restraint.

The Malloryville wetlands lie in a low pocket along Fall Creek, a landscape shaped by the last ice age. As the glacier that once covered this region melted, torrents of water tunneled through the ice, depositing braided ridges of sand and gravel known as eskers. Today, more than a mile of these ancient riverbeds winds through the preserve, narrow wooded spines rising above the surrounding wetlands. From an esker crest, the pattern of water reveals itself: dark channels of open flow, pale pools rimmed with sedge, patches of sphagnum floating like cushions, and, farther off, the straight silver of Fall Creek.

But the story of Malloryville’s water begins far from these pools. Rain falls on the uplands as cool, slightly acidic water. It sinks through glacial till—a jumble left by the ice—and begins a long, blind journey underground. As it moves, the water reacts with the minerals it encounters. Where it brushes limestone or other carbonate-rich layers, it is slowly neutralized and picks up dissolved calcium and magnesium. By the time it resurfaces in low spots, it may be transformed from sour, soft rain to mineral-rich groundwater.

Those subtle chemical shifts are written onto the land. In some hollows, where water still mainly reflects its origin as rain, the environment becomes a bog—cold, acidic, nutrient-poor. Here, sphagnum moss knits a floating carpet, and only specialists such as leatherleaf and cranberries can endure. In other pockets, where groundwater welling up from below brings minerals, we find fens: lush, lime-touched wetlands offering niches for orchids, sedges, and the carnivorous pitcher plant. Marshes and swamps round out the spectrum, their standing water and wooded shade forming still more microhabitats.

In this small preserve, all these wetland types coexist side by side, threaded by water that often moves so slowly it appears not to move at all. The stillness is deceptive. A slight difference in elevation—barely the height of your boot—can determine whether water spreads and stagnates, seeps outward in a fan, or concentrates into a narrow, unseen channel. Hydrologists studying the area have shown that a water-table mound of only a few inches can redirect the underground flow and, over time, steer the evolution from open fen to peat-filled bog.

Human history here is entwined with that quiet power. The founders of the preserve, themselves from a dairy farming family, came to understand that the springs, seeps, and wetlands feeding Fall Creek were vulnerable. Gravel pits on nearby land had already bitten into the valley; another such excavation on this side would have severed the veins of water that sustain the fen and bog. Their years-long effort to protect the property culminated in a Nature Conservancy preserve whose very purpose is to safeguard water and the uncommon communities it supports.

The boardwalk under our feet is part of that story. Its recycled-plastic planks do not rot in constant dampness, and their smooth, slightly hollow sound reminds us with each step that we are guests in a place where soil never truly dries. At the edges of the walkway, tamarack and red maple lift their trunks from hummocks, their roots anchored in peat built grain by grain from centuries of water-logged plant remains. In the open patches, we can seek out pitcher plants, their flaring, water-filled leaves digesting unwary insects to make up for the nutrient-poor conditions.

Everywhere, water moves almost invisibly. It rises as a cold trickle at the base of the esker, fans through the moss as a thin sheet, and gathers again in dark, tannin-stained channels. It rarely speaks aloud; only in spring flood or after hard rain does it murmur against roots or tap lightly at the plastic planks. Yet its influence is written in every texture and color—emerald moss, rusty sedge, the silvery bark of birch leaning over a pool.

To walk in Malloryville is to learn to read this subtle handwriting. We begin by noticing the obvious: the wetness, the boardwalk, the glimpses of standing water. By the end of the walk, we are tracing gradients—how the plants shift with elevation, how the ground feels underfoot, how the air cools or warms by a degree or two. We sense the long journey of water from sky to stone to peatland to creek, and onward to Cayuga Lake and the wider world beyond.

Water, flowing quietly, almost soundlessly, with powerful effect: Malloryville Preserve, that power is persistence. It is the power to carve a valley, to build a peatland one stem at a time, to sustain rare communities of plants and animals in a modest corner of New York. To honor such water is to move carefully, speak softly, and remember that our presence, like our boardwalk, should allow the flow beneath to continue its ancient work.

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Exploring Malloryville Preserve: A Hidden Glacial Wetland Gem in New York’s Finger Lakes

Explore the O.D. von Engeln Preserve at Malloryville, a hidden Finger Lakes wetland where glacial eskers, kettles, and springs reveal the deep story of ice and water.

MichaelStephenWills20 Comments

In the heart of upstate New York, the Finger Lakes region stretches out like a handprint left by the last great ice sheets—long, narrow lakes aligned north to south, their steep-sided valleys feeding into a lattice of creeks, waterfalls, and wetlands. It is a landscape defined by water and time: glaciers grinding south, then melting back north some 12,000 years ago, carving deep troughs, piling up ridges of gravel and sand, and leaving behind a terrain that is anything but simple.

The O.D. von Engeln Preserve at Malloryville, near the small village of Freeville, is one of the quiet places where that story is written most clearly on the land. It doesn’t shout like Taughannock Falls or Ithaca’s famous gorges. Instead, it whispers—through the curves of its hills, the softness of its ground, the unexpected appearance of a spring at the base of a gravel ridge. Here, in a relatively compact area, you can see how ice and water worked together to shape the Finger Lakes region we know today.

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

By the time the preserve officially opened in 1997, the name O.D. von Engeln was already familiar to anyone curious about local geology. His classic book on the Finger Lakes helped generations of readers understand that the scenery around them was not random, but the result of powerful, understandable processes. Reading von Engeln, the rolling hills and quiet valleys near Freeville become more than background—they become evidence: of buried ice, rushing meltwater, and the slow settling of sediments into the forms we walk on now.

Malloryville is an outdoor classroom for that lesson. The preserve is built around a cluster of glacial landforms—eskers, kames, and kettles—that create a three-dimensional mosaic of ridges and hollows. Eskers, those long, winding gravel ridges left by rivers that once flowed inside the glacier, snake through the forest like frozen currents of stone. Kames—steep, irregular hills of sand and gravel—rise suddenly from the surrounding lowlands. Kettles, the depressions left behind when buried ice blocks melted away, now cradle wetlands and pools.

Beneath and between these features, groundwater is constantly on the move. It seeps through layers of sand and gravel, emerges as cold springs at the foot of slopes, and spreads out into swamps, fens, and marshes. In the Finger Lakes, water is always telling a story; at Malloryville, it’s simply easier to hear. Follow the trail and you move through a succession of wet worlds: a seep-fed fen with delicate mosses and sedges, a shrub swamp where skunk cabbage thrusts up in early spring, a cattail marsh that hums with birds and insects in summer.

For my family, the story of Malloryville began even before the preserve had a name. We lived nearby along Fall Creek, itself a thread in the larger fabric of the Cayuga Lake watershed. My son and I camped for the first time on top of an esker just beyond our front door, our tent perched on what I would later learn was the remnant of a stream that once tunneled through the base of a glacier. At the time, it was simply a magical narrow ridge in the woods. Only later, with von Engeln’s guidance and the preserve’s interpretive signs, did that ridge become a sentence in a much older, longer narrative.

That is one of the great gifts of the Finger Lakes: the chance to move from simple admiration—“this is beautiful”—to understanding—“this is how it came to be.” The steep slopes along Cayuga, Seneca, or Skaneateles; the drumlin fields near the north ends of the lakes; the hanging valleys and waterfalls; and the quiet wetlands of places like Malloryville are all chapters in the same glacial chronicle. Once you learn to read one place, you begin to read them all.

Walking into the O.D. von Engeln Preserve, you enter that story at a small, intimate scale. The parking area and trailhead give way quickly to a world where the ground feels different—sometimes firm and gravelly, sometimes soft and yielding underfoot. Wooden walkways and narrow paths thread through shady forest and open wetland. Each bend offers a subtle shift: a new plant community, a change in water clarity or flow, a small sign explaining what lies beneath your feet.

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.

This is not grand scenery in the postcard sense; it is something quieter and deeper. Malloryville invites you to slow down and notice. To ask why a particular ridge is so narrow, why water emerges here but not there, why one hollow is filled with shrubs and another with moss and sedge. In learning those answers, you gain not only an appreciation for this modest preserve but also a richer understanding of the entire Finger Lakes region.

The Trout Lily (Erythronium americanum) is named for the mottled brown leaves resembling marking on trout.

In the end, the O.D. von Engeln Preserve at Malloryville is a lens—a way of seeing. Through it, the familiar landscapes of central New York—valleys, hills, streams, and lakes—come into sharper focus as the lasting work of ice and water. Stand on an esker, look across a kettle wetland, listen to the quiet trickle of a spring, and you are standing inside the very processes that shaped the Finger Lakes.

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Cornell Botanic Gardens’ Monkey Run: History, Geology, and Scenic Fall Creek

A contemplative walk along Monkey Run where Fall Creek writes the valley’s history—sycamores, bridges, and Devonian stone speaking across seasons in Cornell’s living classroom.

MichaelStephenWills17 Comments

On a morning in late March, when the hills about Ithaca still hold the night’s frost in their shaded folds, I took the path called Monkey Run and went to see how Fall Creek spends its winter earnings. The air had the bright sting of thaw, a kind of vernal austerity that keeps a man honest in his steps. Along the high bank the sun spilled its coin onto the water, where it broke and flickered like a school of silver minnows. A rim of snow clung to the shale ledges, and the leaves of last year’s oaks—curled, fox-red, and faithful—whispered as if to keep the woods awake until spring fully claimed them.

Sunlit bend of Fall Creek viewed from a high bank at Monkey Run in early spring.

Monkey Run is one of the outlying parcels tended by Cornell Botanic Gardens—once called the Plantations, and now, more fittingly, named for the living charge it keeps. These gardens do not end at beds and borders; they encompass the wilder rooms of the county, more than a thousand hectares of glens, pastures, and ravines where the university’s first and oldest teacher—nature herself—still holds class. Fall Creek is one of her principal lecturers. Rising beyond the high country of Cayuga Heights and slipping under stone and snow, it shoulders its way across the campus, idles a while in Beebe Lake, and turns turbines of memory at Triphammer Falls before shouldering on toward the lake that receives nearly everything here—Cayuga—long, deep, and glacial in its thinking.

Tall white-barked sycamores leafless against a blue March sky at Monkey Run.

If you would learn a valley’s mind, walk a meander. The creek here composes with easy cursive, laying down a bar of gravel, nibbling at a bank of clay, then sweeping back to consider its work from the opposite shore. The geologist says the rock is Devonian, pages laid flat and damp with time, and the ice of ten thousand winters ago scoured them into the open. A creek is a patient mason, working without rest and never in anger. I admired these sycamores—their clean bones shining through the leafless canopy like the ribs of an old cathedral. Winter reveals their whiteness; summer grants them shade. A stand of white pines keeps a dark counsel in the background; on the muddy edge, green tongues of skunk cabbage push up, pledges made by the swamp to keep faith with the sun.

Rust-stained steel pier above calm water on Fall Creek along Monkey Run trail

I came down to the water near an old steel pier, a bridge remnant, hanging on each end without purpose. It wears graffiti the way a boulder wears lichen; human wishes, briefly rooted, coloring what they can. The river accepts it all, the pilings and the scribbles, the cast limb and the bottle’s glint, and continues its one unarguable gesture downstream. That is the old instruction of Fall Creek: use, refuse, endure. Before the university drew students from every quarter, the creek turned wheels and powered the small ambitions of a frontier town. Even the name Triphammer speaks of iron struck to purpose. Now the water powers something quieter: the studies of herons, the almanacs of kingfishers, the quick arithmetic of minnows over limestone.

Looking back while climbing the steep bluff

Steps cut from logs ascend the bluff, each tread pegged with iron, each rise a short confession of breath. I climbed to the ridge, paused halfway, and through the gray lace of March branches saw the creek shining at a bend far below. A man cannot help but measure his own life against such a course. The path goes up and down in obedient red blazes, but the water keeps its own counsel. Where the bank slumps the river shoulders through; where the bottom rises it lays down a mirror. In my youth I wanted the straight run, the short work. Now the curve pleases me. To go with the current and not be carried away—that is a lesson suitable to the grey in my beard.

Clear, shallow run of Fall Creek with shale bottom and pine stand in distance
Bluff overlooking Fall Creek in summer

When I returned five months later, on August 23, the same path had forgotten the word austerity. The cathedral of sycamore was fully leafed, the white pillars now vanished behind a nave of shade. The pines perfumed the air without trying. A new footbridge—clean timber arching like a bent bow—spanned one of the wet flats. Its braces, black-bolted and handsome, looked as if they would hold the weight of an ox team or a file of schoolchildren. Such crossings are a kind of promise from the present to the future: we found a way through here; may you, too. Below, the floor was upholstered with moss, oak leaves, and a scatter of pinecones—the slow currency of the woods accumulating interest.

Arched wooden footbridge in summer forest on Cornell’s Monkey Run trail.

Summer makes a confidant of every plant. Ferns unrolled their scripture at the bridge abutment; jewelweed held its tiny lanterns along the seeps; a kingfisher rattled downstream, blue lightning with a bill. The creek, glassy over its shale pavement, showed every wrinkle of its stride. I waded a little, feeling with the sole what the eye could not—where the current took an extra thought around a stone, where it forgot itself in a warm eddy. Trout lingered in the dimmer reaches, quick as commas; a great blue heron lifted off with that surprising tidiness of wing, ungainly only in our imagination.

In all seasons the trail carries two histories: one written in rock and water, the other in the footfall of people. Cornell’s founders, Ezra and Andrew White, believed the university should place the hand near the thing studied; here that principle is plain. Botany students take their lectures in leaf and bark; geologists read the creek banks as if the pages might soon turn by themselves; children learn the oldest calculus—how long a stick will float before it catches in the weeds. The caretakers from the Botanic Gardens mark, mend, and interpret, but they do not overtalk. The woods speak enough.

Moss, grass and pinecones on an overlook of Fall Creek

As the afternoon eased toward evening, I climbed once more to the bluff. The light had gone honey-colored and the leaves of the maples, those careful accountants of September, were just beginning to weigh their green against gold. I looked down on the bend where I’d stood in March—cold, bright, expectant—and felt the year’s circle gently close. As John Burroughs wrote, “The power to see straight is the rarest of gifts… to be able to detach yourself and see the thing as it actually is, uncolored or unmodified by your own… prepossessions… that is to be an observer and to read the book of nature aright.” Monkey Run obliges that humility. The creek moves as it always has—glacially taught, mill-forged, campus-wise, and freedom-loving—and the trail, with its modest stairs and honest bridges, invites us to walk beside it, to match our breath to its turnings, and to leave, if we can, a lighter trace than we found.

References

Ways of Nature (1905), “Reading the Book of Nature,” pp. 275–276 (The Writings of John Burroughs, Riverside ed., vol. XIV, Houghton Mifflin)

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Glacial Echoes: Dryden Lake Park’s Mirror-Calm Morning in Upstate New York

Morning clouds hang over Dryden Lake as hills kindle first color; reflections hold breath while a lone walker reads the valley’s glacial and human-written past.

MichaelStephenWills11 Comments

He came to the water before the people woke, the road a still ribbon of cold tar snaking beneath the low hills. Mattocks of cloud hung over the valley and the lake took in the sky like a mirror dropped yet not broken. The trees were beginning to color. A patient fire working from within the leaves. He parked where the grass ran down to the shore and stood a long while without moving. Birds made small sounds in the reeds. Somewhere a single truck labored up the grade and was gone. The surface held the hills with a steadiness the hills themselves could not keep. He thought how the quiet of a place can be the loudest thing it owns.

He went along the margin along the damp sedges where old drift lay silvered and light as bones. A drowned trunk angled from the shallows. The lake was old in the way of things made by ice and time. A kettle in the outwash of the last glacier, some men said, a bowl left when the buried ice eased away. He pictured the ice receding into the valley heads, the meltwaters choked with gravel, a hand larger than memory scribing the floor of this country. The earth never told it plain but the lay of it was witness enough. Across later centuries men cribbed a dam across the outlet and drew the water to a shape that pleased them and served their work.

A trail ran the length of the water on the old rail bed. The ties were long gone and the iron and cinders buried under years of leaf fall and gravel. He had walked it as a boy beside his father and now he walked it alone. Benches stood at half-mile intervals like waystations in a country of small pilgrimages. The signs told what once was here and what remains. They had renamed the path for a townman who argued it into being after the railroad had passed from the world and the right-of-way grew up with sumac and rumor. It was an easy trail and he carried nothing. His hands hung at his sides as if the day might place something in them when it was ready.

In another era the lake was a workshop. Men whipsawed timber in the wet air and fed small mills with the grove’s dark boards. Winter flowed over the flats, and they built icehouses and set the blocks within like blue stone, an industry that died when cold could be called from a switch. The hills have learned to forget the noise of it, though on certain mornings the fog takes a shape and you could believe rising from the ponded sawdust and the lading of sleds. He thought of the labor of those gone hands and of how work is a scripture every place keeps in its own tongue.

Before any of that, the ground here was a summer camp. People came with the season and went with it, laying their fires in the lee of the knoll and taking fish where the cattails thin. He could feel them in the open places, not as ghosts but as the first understanding the land ever had of itself. The words used for them now are museum words, yet the wind still crosses the water as it did and empties the same smell of iron and leaf into the lungs of whoever stands to breathe.

The town took its name from a poet long dead, a scholar’s choosing in the years after the war for independence when this tract of country was parceled out to soldiers of that same war. Virgil lay to the east as if they were shelving Latin across a map. The creek that bears that name threads the villages and finds Fall Creek at Freeville, and the combined waters go their own slow way toward Cayuga where the glacial hand scooped deeper yet. He said these names under his breath and they tasted of chalk and river stone.

A kingfisher rattled across the cove. The fish rose in rings that spread and vanished like time seen from above. Out on the water an old man pushed a skiff with an electric motor that hummed like a trapped bee, for the lake allows no gas engines now. The wildlife area ran around the shore in a ragged collar of field and wetland and alder, near two hundred acres under the state’s keeping, and the lake itself a little over a hundred. He watched the man aim for the lily line and thought how rules arise from the wish that a thing endure, though nothing does. Still we make the rules and we keep them as if the earth were listening.

Wind came down the slope with a smell of rain. He turned back and the hills lay again in the water, entire, and for a moment he could not tell which world had claim to the other. He thought of the rails pulled up and the mills gone to weeds and of the icehouses fallen into their own shadows and he thought of the people before all that and of the long winter pressing its thumb into the land and lifting it away. He thought of his father walking the rail bed beside him a lifetime ago and saying nothing. There are places where the past crowds close and will not be argued with. He stood until the first drops dimpled the surface and the reflection shattered and reformed. A train no longer runs here. The only sound was the soft percussion of rain on water and the slow turning of the earth beneath both. He put his hand to the damp trunk of a fallen tree and felt the grain and the coolness and the old patient labor of rot. Then he went up from the reeds, his pockets full of acorns, and out to the road where his truck waited and the day, austere and sufficient, came along with him.

References

Geological History and Glacial Formation of the Finger Lakes

Jim Schug Trail

The Dryden Lake area in the 19th century

Indian Campsite on west side of Dryden Lake

Dryden New York (wikipedia)

Dryden Lake (New York State DEC)

Geohydrology, Water Quality, and Simulation of Groundwater Flow in the Stratified-Drift Aquifer System in Virgil Creek and Dryden Lake Valleys, Town of Dryden, Tompkins County, New York

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Autumn Reflections: The Majesty of Acer Rubrum

On a serene autumn afternoon by Beebe Lake, a solitary red maple stood out against the backdrop, showcasing its vibrant colors and resilience, symbolizing autumn’s fleeting beauty.

MichaelStephenWills25 Comments

It was one of those serene autumn afternoons that linger in memory, the kind where the sky seems impossibly clear, the air crisp and gently scented with fallen leaves. I stood at the edge of Beebe Lake, my gaze first drawn to the textured concrete dam holding back the water, its weathered facade contrasting sharply with the soft reflections shimmering across the lake’s calm surface. Beyond, the wooded hillside rose gently, a tapestry woven with the warm hues of autumn—golds, greens, oranges, and reds mingling like brush strokes on a canvas.


An October Glory, turning before all others

Yet amidst this collective beauty, one tree captured my attention, singular in its brilliance—a solitary red maple standing proudly on the lakeshore. Its leaves had turned a vivid crimson, blazing brightly as though defying the muted earth tones surrounding it. Even from a distance, framed and partially obscured by larger trees, its vibrant reflection cast a fiery echo on the water, rippling softly in the afternoon breeze.

The maple, Acer Rubrum, seemed perfectly at home here, thriving robustly at the water’s edge. I remembered reading how adaptable red maples are, able to flourish in conditions ranging from dry uplands to swampy shores. This spot, near the edge of the tranquil Beebe Lake, seemed to showcase its resilient character perfectly.

Up close, the maple’s glow was even more striking. Its leaves cascaded in fiery clusters, hues deepening from bright scarlet at the tips to a darker maroon closer to the branches. This dramatic gradient seemed symbolic of autumn itself—beautiful, fleeting, and subtly tinged with the melancholy reminder of winter’s approach.

The Red Maple (Acer Rubrum) to tolerant of diverse conditions, making it a perfect choice for this spot on the short of Beebe Lake.

A memory surfaced of early spring in the Finger Lakes region, a time when maples, including this red maple, generously share their sap. Though not traditionally tapped like its sweeter cousin, the sugar maple, this species’ sap can indeed be boiled down into syrup, a surprising sweetness hidden within its sturdy trunk. Standing in its shadow, imagining those early spring days, it seemed astonishing that the same tree could offer both the delicate sweetness of syrup and the fierce beauty now on display.

Curiously, the transformation of the tree appeared methodical yet whimsical—it changed colors from the top down, its upper branches already bare, exposing slender twigs pointing skyward. Like an artist carefully removing layers to reveal something deeper beneath, the maple unveiled its upper bare bones first, as though reminding observers of the quiet strength supporting its autumn splendor.

This Red Maple (Acer Rubrum) turns from the top down and has already bare for most top branches.

As I lingered, taking in this turning tree, joggers passed by along the path, their rhythmic footsteps a gentle percussion beneath the rustling leaves. Briefly, they glanced toward the vivid maple, perhaps drawn, like me, by its striking contrast to the surrounding foliage. It felt like we shared a secret admiration for this singular tree, recognizing in it a quiet assertion of individuality amidst conformity.

Eventually, I viewed the maple once more from afar, framed now by broader sweeps of branches and leaves, partially obscured but no less vivid. Through layers of leaves and dappled sunlight, it glowed like a distant flame, a beacon that seemed to encapsulate the entire mood of the season—warm yet cool, bright yet transient.

The Red Maple (Acer Rubrum) is the first to flower in spring and the first to turn in autumn.

Walking away, the image of that maple lingered, its reflection shimmering gently in the afternoon sun, a moment suspended between summer’s lush vitality and winter’s bare stillness. Beebe Lake had offered scenic beauty, a quiet meditation, a reflection mirrored not only on its tranquil surface but in the heart of an observer captivated by a single tree’s fleeting glory.

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Buttonbush: The Secret Geometry of Wetlands

Discover the Buttonbush (Cephalanthus occidentalis), a wetland shrub of spherical blooms, sustaining pollinators, birds, and waterfowl while reminding us of life’s enduring cycles

MichaelStephenWills9 Comments

In the quiet wetlands of late summer, when cattails lift their brown torches above the reeds and dragonflies skim the still water, there is a shrub that speaks in spheres. Its language is not the pointed spear of grass or the broad fan of lily pads, but the perfect symmetry of globes—round, intricate, and startling in their precision. This is the Buttonbush, Cephalanthus occidentalis, a native of swamps, pond margins, and the soft, yielding soils where water shapes the land.

At first glance, its clusters might be mistaken for something fashioned by human hands: spiky balls arrayed along slender stems, each one a small planet bristling with tiny cells. Only in memory can we recall their summer incarnation, when each ball was a constellation of snowy blossoms, white tubular flowers extending like delicate pins from a spherical center. Bees and butterflies crowded them then, drunk on nectar, wings glinting in the sun. Hummingbirds darted in as though drawn by an unseen magnet, their beaks fitting perfectly into the narrow blossoms, a partnership written long ago in the shared script of evolution.

Buttonbush (Cephalanthus occidentalis) at Sapsucker Woods, Cornell Lab of Ornithology

Now, in August’s waning light, those blossoms have folded back into seed, transforming into the russet orbs captured in the photograph. What was once nectar is now promise—food for ducks, shorebirds, and the small lives that depend on wetlands for sustenance. In the hands of buttonbush, time itself is circular. Flower becomes fruit, fruit becomes seed, seed becomes shrub, and the cycle spins quietly on, just as the spheres themselves suggest: complete, unbroken, eternal.

A Wetland Companion

Buttonbush is rarely alone. It thrives where cattails whisper, where pickerelweed thrusts up spikes of purple bloom, where the air holds the scent of waterlogged earth. Its roots grip the muck at the edges of ponds and rivers, holding soil against the restless tug of currents. In doing so, it becomes part of the unseen architecture that holds wetlands together, slowing erosion, filtering water, providing shelter for fish in the shade of its stems.

Pickerelweed (Pontederia cordata) at Sapsucker Woods, Cornell Lab of Ornithology

This shrub, unassuming in stature, is an engineer of stability. It creates thickets where red-winged blackbirds perch, where frogs crouch in shade, where turtles bask on half-submerged branches. The wetlands of North America would be poorer without its presence, for it provides not just beauty but the scaffolding upon which entire communities of life depend.

The Human Thread

To the human eye, the buttonbush’s spherical blooms are so striking that they demand metaphor. Some have called them pincushions, others tiny planets, others fireworks arrested in mid-burst. Native American peoples, however, looked beyond metaphor to medicine. The bark and roots were used in remedies for ailments ranging from headaches to fevers, though with caution, for the plant holds mild toxicity when consumed raw. It is a reminder that many gifts of the natural world are edged with danger, and that wisdom lies in balance.

Today, gardeners and conservationists plant buttonbush intentionally. It is welcomed into rain gardens, where its thirst for moisture makes it a perfect ally for absorbing stormwater. It is used in wetland restoration projects, where its deep roots anchor new life. And it is cherished by those who walk the edges of ponds and discover in its round blossoms a geometry that feels both wild and deliberate, a gift of design from the living earth.

Fourth of July, 2019, Stewart Park

The Sphere as Symbol

Rachel Carson once wrote that in nature, “nothing exists alone.” The buttonbush embodies this truth with clarity. Its spheres are invitations, junctions where plant and pollinator meet, where flower and bird share a moment of mutual necessity. They are offerings to the eye as well, challenging us to see patterns where we might otherwise see only happenstance.

Standing before a buttonbush in bloom, one feels an almost childlike wonder: how could such symmetry arise unbidden from soil and sunlight? Yet this is the miracle of evolution, that order may spring from chance, that beauty may serve survival, that what pleases our senses also sustains life.

A Closing Reflection

In the wetlands, where water mirrors the sky, the buttonbush offers its own reflection of completeness. Its seed heads persist through autumn and winter, small orbs clinging even when leaves fall, reminders that the cycles of life turn steadily beneath the stillness.

To linger with buttonbush is to be reminded of nature’s quiet insistence on wholeness. It speaks in forms: round, repeating, enduring. To walk away from it is to carry a sense of connection, to know that in the pattern of its blooms we glimpse a truth both humble and profound—that life is not a line but a circle, and in every turning there is renewal.

For Further Reading

USDA NRCS. Plant Guide: Buttonbush (Cephalanthus occidentalis L.). United States Department of Agriculture, Natural Resources Conservation Service. Available online: https://plants.usda.gov
– Provides detailed information on identification, habitat, and ecological role.

Lady Bird Johnson Wildflower Center. Cephalanthus occidentalis (Common Buttonbush). Native Plant Information Network. Available online: https://www.wildflower.org/plants/result.php?id_plant=ceoc2
– Covers botanical features, bloom time, wildlife value, and landscape use.

Dirr, Michael A. Manual of Woody Landscape Plants: Their Identification, Ornamental Characteristics, Culture, Propagation and Uses. 6th Edition. Stipes Publishing, 2009.
– Authoritative horticultural reference on Buttonbush and other shrubs.

Peterson, Roger Tory, and Margaret McKenny. A Field Guide to Wildflowers: Northeastern and North-central North America. Houghton Mifflin, 1968.
– Classic field guide covering buttonbush’s wetland habitat.

Carson, Rachel. Silent Spring. Houghton Mifflin, 1962.
– Source of the quoted passage: “In nature nothing exists alone.” (Chapter 2, “The Obligation to Endure”).

Moerman, Daniel E. Native American Ethnobotany. Timber Press, 1998.
– Comprehensive reference documenting traditional medicinal uses of Buttonbush among Native American peoples.

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Historical Wonders of Ashford Castle and Its Natural Surroundings

At Ashford Castle, swans glide on the Cong River’s glassy waters, weaving together myth, history, and cinema in a timeless reflection of Ireland’s enduring spirit.

MichaelStephenWills9 Comments

Headed south from Cong Village, past the venerable Cong Abbey then Saint Mary’s Church of Ireland, the road bends into the Ashford Castle estate. Time seems to shift here. The stonework of the abbey lingers in memory, only to give way to manicured parkland, ancient trees, and the shimmer of water. The road itself, aptly named Ashford Castle, carries the traveler to a place where history, nature, and imagination meet.

I do not recall passing a guard box on my first visit, though one now stands firmly on the roadside, manned and proper, as though the estate were never meant to be entered without ceremony. In truth, Ashford Castle has always carried the air of a threshold—between village and wild, past and present, myth and reality.

Soon the road brings one to the banks of the Cong River. Here the water widens, flowing calm and sure, and across it rises the battlemented silhouette of Ashford Castle itself. Its towers, turrets, and stony walls seem to grow from the riverbank like something inevitable, a fortress transformed into elegance. The castle’s mirrored reflection on the water doubles the grandeur, as though the real and imagined castle exist side by side.

It is no wonder filmmakers found inspiration here. Scenes from the classic 1952 film The Quiet Man—the tale of Sean Thornton, played by John Wayne, and the fiery Mary Kate Danaher, embodied by Maureen O’Hara—were shot on the far bank of this very river. To watch them walking by these waters is to see Ashford Castle woven into Hollywood’s Irish dreamscape, a backdrop both romantic and enduring.

Yet long before cinema, the river was already a stage. The Cong River is a natural marvel. It emerges from the same Carboniferous limestone that shapes the Burren of County Clare—an austere landscape of limestone pavements etched with fossils and caves, where rare alpine and Mediterranean plants thrive among ancient tombs. Through fissures in this ancient bedrock, the waters of Lough Mask find their way underground before rising again at Cong. This subterranean journey, through stone filters laid down some 350 million years ago, leaves the water clarified, luminous, and cold. By the time it slides past Ashford Castle, it has the purity of glass.

It is in this clarity while walking the opposite bank on a different morning I found a parent swan and its cygnet feeding. The adult glided, immaculate, its long neck bowed as drops of river fell from its beak. At its side, the cygnet paddled with earnest strokes, gray down still clinging, a fragile shadow of what it would one day become. Together they traced a quiet path across the water, ripples fanning behind them.

Few images so perfectly match their setting: a medieval castle, guardian of centuries, reflected in the same waters where these swans carried on their timeless rhythm of nurture and growth. It was as if the river itself composed the scene—a blending of stone, water, bird, and sky that belonged nowhere else but here.

The swan has long been a symbol in Irish lore. The Children of Lir, cursed to live as swans for nine hundred years, are among the most haunting figures of Celtic mythology. To see the white bird with its offspring before Ashford Castle was to glimpse that myth breathing still, alive on the Cong River.

Photographers know the difficulty of capturing water and stone without losing the life between them. On that morning, however, the river gave freely—its surface alternately smooth as glass and dappled with breeze. Stones at the water’s edge appeared like stepping-stones into history. Each frame revealed another face of the estate: the wide reach of the Cong, the castle framed by trees, the play of cloud shadows across the current.

The castle itself, though reshaped as a luxury retreat, still speaks of older times. Founded in the 13th century by the Anglo-Normans, Ashford passed through centuries of conquest and change before becoming, in the 19th century, a romantic Victorian pile. Today its battlements remain picturesque rather than defensive, but the sense of continuity—of lives unfolding along these banks—has not faded.

Standing there, camera in hand, I was struck by the layered meaning of this place. The Cong River flows from unseen caverns, purified by limestone older than memory. It nourishes swans, reeds, and trout alike. It reflects both a castle and a sky. Along its opposite bank, legends of cinema and Celtic lore alike find footing.

As the swan and cygnet drifted slowly downstream, I thought of them as part of the same enduring thread. Parent and child mirrored castle and village, past and future, permanence and change. The ripples they left widened until they touched both banks, an unbroken gesture across centuries.

Click this link to read another Ireland story “The Cloigtheach of Glendalough.”

Click this link to read another Ireland story “Killeany Bouy.”
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Carved by Time: Exploring the Virgin River and Cross-Bedded Sandstone in Zion’s Narrows

A quiet moment along the Virgin River reveals the artistry of nature—where water, stone, and time shape Zion’s majestic Narrows in subtle, surprising ways.

MichaelStephenWills

In Zion National Park, where towering sandstone cliffs rise from the desert floor, the Virgin River weaves a persistent and graceful thread through deep canyons carved over millennia. The river is the creative force behind Zion’s signature landscape, sculpting stone with a patient hand. Among its greatest achievements is the Narrows—a sinuous gorge where water and light perform a timeless duet. The two photographs shown here draw us into an intimate corner of that realm, where water flows past a rock face marked by both subtlety and drama.

At first glance, what stands out is the unusual structure on the wall behind the river—a feature that at a distance could easily be mistaken for a man-made stairway. But closer observation reveals this to be a natural element, the result of erosion acting upon cross-bedded Navajo Sandstone. The texture and linearity of these formations are remnants of ancient sand dunes hardened into rock nearly 190 million years ago, during the Jurassic period. What looks like precision carving is, in fact, the legacy of sedimentation, lithification, and the scouring action of water over time.

In the first photograph, the scene is bathed in soft, diffused light, lending a quiet tone to the flowing water and the weathered rock face. The surface of the Virgin River becomes a silky sheet, its motion captured with long exposure so that it seems to glide effortlessly past the cluster of smooth stones in the foreground. Here is a deep calm—the kind that can be heard in the hush of water over stone and felt in the breathless silence of a canyon morning.

Click each photo for a larger view
Taken using the Kodak DCS Pro SLR/c mounted with a Canon EF 50mm f/1.4 USM lens

The second photograph, taken under brighter conditions, reveals the same scene with different character. The increase in light clarifies the water’s transparency, the greens of moss and lichen on the wall, and the golden tones of the sandstone. What you see is a pattern formed by layers of wind-blown sand, once part of vast dunes, now standing as a stone ledger of time. The river, its bed visible beneath the shallow flow, seems to read this text as it passes—century by century, pebble by pebble.

The Virgin River begins high in Southwestern Utah, at the Navajo Reservoir in the Dixie National Forest north of Zion National Park and travels over 160 miles to join the Colorado River, carving through layers of sedimentary rock as it descends. In the Narrows, the canyon walls rise up to a thousand feet while the corridor narrows to just 20–30 feet across in places. The intimacy of the Narrows contrasts with the vast openness elsewhere in Zion, enclosing the traveler in a world of water and stone, shadow and echo.

Walking the Narrows means walking in the river itself—an experience that engages body and spirit alike. The water is rarely still, and neither is the trail. Slippery rocks and ever-shifting current demand attention and balance. Yet, this very immersion invites a deeper kind of awareness. You are observing nature from within it, shaped by nature, and held by nature.

What the photos capture so eloquently is that Zion is a place where the work of nature can appear deliberate, even architectural. The illusion of stairways in the sandstone, carved not by hands but by wind, gravity, and time, is a reminder of how little separates the human sense of design from the forms nature produces. We recognize rhythm and repetition, elevation and flow, and are drawn to interpret meaning from these patterns.

But perhaps the meaning lies not in what we impose, but in what we receive. The Virgin River’s passage through this sculpted corridor teaches patience, resilience, and the beauty of gradual transformation. Its waters do not fight the rock; they yield, swirl, and persist—until the rock, by degrees, gives way. What results is a landscape both eternal and ever-changing.

Zion’s grandeur is easy to admire its many amazing overlooks, but its soul is found in quiet places like this—where sandstone walls, smoothed by water and time, speak not in shouts but in whispers. Here, beside a seeming stairway that leads nowhere and everywhere, we come face to face with the artistry of the Earth.

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Exploring Sims-Jennings Preserve: A Nature Lover’s Delight

A walk through Sims-Jennings Preserve unveils ancient cliffs, vibrant bird calls, and the quiet wisdom of maples and waterfalls along Cayuga Lake’s forested edge.

MichaelStephenWills15 Comments

I arrive early, the sun still climbing its slow arc, brushing the eastern sky in pastels as I step into the Sims-Jennings Preserve at Cayuga Cliffs. The trailhead, tucked neatly along NYS Route 34B, is a doorway into an ancient chapter of the Finger Lakes—one rich with the scent of moss, the hush of leaf-dappled silence, and the layered echoes of stone and birdsong.

The first thing that strikes me is the expanse of mowed meadow, rimmed with goldenrod and patches of milkweed. From here, the land rolled gently westward until it ends abruptly in cliffs that plummeted toward Cayuga Lake. A map at the entrance speaks of the Sherburne and Renwick Formations, shale and siltstone laid down when the land was covered in warm Devonian seas. The cliffs themselves stand like watchmen over time, protecting 4,000 feet of lakeshore from erosion, whispering tales older than mammals.

A side trail leads to this mowed meadow and Cayuga Lake overlook

On the meadow edge is this Carya ovata, or shagbark hickory, unmistakable from its elongated leaflets and distinctive bark that peeled in long, curled strips. The leaves shimmered in the breeze, their green etched with pale speckles of recent rain, as if nature herself had hand-painted them.

Shagbark Hickory on the edge of meadow.
Leaves of the Shagbark Hickory
Shagbark Hickory bark / trunk

I follow the yellow-blazed trail into a thicket where tall sugar maples—Acer saccharum—arched overhead. Their leaves caught the morning light, each palm-sized blade glowing like a shard of stained glass.



Throughout the preserve I find large holes like these in a pine tree snag, the work of a Pileated Woodpecker.

A sudden fluting note from the trees stops me in my tracks. “Ee-oh-lay,” the Wood Thrush sang, its call cascading through the forest like water over stone. Moments later, the rapid, accelerating trill of an Ovenbird joins in—a sound like “teacher-teacher-teacher” echoing from the understory. The forest is alive.

Watch on YouTube for the best experience.

I descend into the shade. A narrow stream runs over the flat gray ledges of the Ludlowville Formation, forming delicate waterfalls no taller than a man but intricate as lace. One fall, framed by a colonnade of black cherry and beech trees, poured over stone like a ribbon of silk. The water’s voice changed with each ledge—first a murmur, then a chuckle, then quiet confidence as it wound through the woods.

Here, a Scarlet Tanager flashes like flame through the canopy, its red feathers shocking against the sea of green. Above, the Eastern Wood-Pewee calles its own name from a high perch—“pee-a-wee”—a humble herald of summer. Lower down, a Tufted Titmouse flits from branch to branch, a gray blur with a whistle like curiosity incarnate.

Further along, a looping vine coils around a pair of trees like an ancient signature. Possibly a native bittersweet, its woody stem thick as a child’s arm. It reminds me of how all life here is entangled—flora, fauna, stone, and stream woven into one vast web.

I pause at the overlook, where the trail skirts the cliffs. From this height, the view opened to Cayuga Lake, vast and gleaming in the morning light. Across the water, the hills of the western shore softened into a watercolor horizon.

Crowbar Point on the west lake shore is visible, partially hidden by trees. Sims-Jennings Preserve at Cayuga Cliffs, Finger Lakes Land Trust on a May morning 2025, Lansing, Tompkins County, Finger Lakes Region

On the walk back, a robin sings its measured phrases from a nearby hawthorn, and I think how common birds often hold the deepest solace. The robin’s voice rises above the silence, not grand, not rare, but reassuring in its familiarity—like a good friend’s greeting.

A shale ledge, Renwick Formation (?)

I leave the preserve changed gently, like the soft indent of a footstep in moss. The Sims-Jennings Preserve at Cayuga Cliffs is a place that reminds you to listen. To the birds, to the trees, to your own breath. And in listening, you remember what it means to be wholly present in the world.

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On The Edge of Time Above Taughannock Gorge

Perched above Taughannock Gorge, a moss-covered ledge and cascading falls reveal ancient stories—where Devonian seas once flowed and time’s layers whisper through stone and water.

MichaelStephenWills5 Comments

The morning sun had only just breached the rim of the gorge, sending long slants of golden light across the forest floor. Walking the South Rim Trail of Taughannock Falls State Park, I came upon a quiet, unassuming spot—just a few paces off the path—where the forest seemed to pause in reverence. What greeted me was a small marvel of persistence and time.

There, rooted precariously atop a slab of brittle shale, was a tenacious shrub rising from a bed of moss, its spindly frame etched in sharp contrast to the soft, green sprawl beneath it. The moss had taken hold on a shelf of rock cantilevered over the gorge like a green tongue of earth defying gravity. Cracks traced the shale’s surface like veins, silent records of the forces that shaped this place—heat, ice, pressure, time. Together, the moss and the bush formed an improbable community, surviving against odds, bound together by the thin soil cradled in stone.

This ledge, suspended over the abyss, seemed less a part of the earth than a question it asked—how much life can cling to the edge before the edge itself gives way?

Beneath this living fragment, the gorge dropped away. Layers upon layers of shale revealed themselves, stacked like a collapsed library of time. Here, the Devonian Period lies exposed to wind and rain, and to those willing to pause and wonder. Each stratum holds the fossil whisper of ancient seas, where trilobites scuttled and coral reefs once stood. This gorge was not carved quickly. It was not born of a moment, but of many—countless raindrops, millennia of ice melt, the slow, sure work of water over stone.

From this natural balcony, I looked out and down to the gorge floor where the creek shaped the land with an artist’s patient hand. The falls, seen from above, no longer thundered—they danced. Spread like the folds of a fan, water curled over smooth stone in steps of white silk. From here, the cascade looked deliberate, choreographed—an elemental performance halfway between gravity and grace.

How many times had this water flowed, reshaped, receded? How often had it carved these grooves, smoothed those ridges, erased the footprints of what came before? Looking at the exposed rock, one could trace the signature of ancient glaciers, feel the memory of long-gone floods. It was humbling—this intersection of change and continuity.

Above it all, the trees stood still. Pine and oak, rooted well back from the edge, offered a kind of sentinel presence. Their shadows stretched long and angled, tracing the contours of both earth and memory. For a moment, I let go of all thought and simply listened—to the murmur of wind through leaves, the faint rush of water far below, and the silence that presses in when the land itself seems to be remembering.

This spot—so easily missed by a hurried hiker—offered a parable of resilience and impermanence. The moss did not grow with certainty, nor the shrub reach with confidence. They survived on the edge because they adapted. They made do with less. They took root where others could not. There was no security in that place, only presence. Only the now.

And isn’t that a lesson worth carrying?

We so often seek stability, firm ground, a clear path. Yet, some of the most beautiful things live just beyond comfort—on ledges, in cracks, in the margins of the known. To pause here was to acknowledge that life thrives not only in sheltered valleys but also at the edge of what seems possible.

As I stepped back onto the trail and continued along the South Rim, the image of that mossy outcrop stayed with me. I carried it in my thoughts like a talisman—proof that even on the brink, life finds a way. And that from above, the most chaotic falls can appear as ordered motion, as a flow toward something larger.

Later, when the sun climbed higher and the light lost its slant, I would look back on this moment not as a spectacular highlight but as something more intimate: a quiet encounter with nature’s subtle artistry, its layered truths, and its enduring invitation to look closely, feel deeply, and walk softly.

For here, above the gorge, at the edge of earth and time, even a whisper leaves a mark.

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