Winter Walking at Taughannock Falls: Finding Connection and Quiet Along the Gorge Rim Trails

Winter distills Taughannock Gorge to stone, water, and silence, where careful footsteps along icy rim trails reveal deep connections between landscape, memory, and quiet joy.

Winter pares the world down to its essential lines, and nowhere is that more apparent than on the rim trails of Taughannock Falls State Park. On a Wednesday afternoon walk, a three-mile pilgrimage, the gorge revealed itself as a living corridor of connections—between water and stone, past and present, effort and joy. The season sharpened every sensation: the crunch and slip of ice underfoot, the hush of leafless woods, the long exhale of the falls echoing unseen below.

From the overlook, the gorge opens like a vast stone book, its pages written in shale and time. Taughannock Falls drops away in the distance, not so much seen as felt—its presence announced by scale and gravity. Even before stepping onto the trail, the walk establishes its rhythm: pause, look, breathe. Winter insists on this slower tempo. Ice dictates caution, and caution invites attention.

Heading along the Rim Trail my progress became deliberate. The path, glazed in places with solid ice, turned each step into a negotiation. Yet this was no impediment to pleasure. Slowness allowed for noticing the quiet labor of the park maintenance crew, whose careful clearing and repairs spoke of spring already anticipated. Their work stitched the present moment to the coming season, a reminder that parks, like stories, are maintained through this unseen devotion.

The gorge itself is a system of thresholds. A bridge crossing the creek marks the transition from North to South Rim, but it also frames one of the most dramatic views in the park. Standing above the chasm, one senses connection: water flowing beneath, trails diverging and rejoining, human passage layered lightly atop geological endurance. The gorge is a conversation between forces, ongoing and unresolved.

Gorge Road, early November
Gorge Road, early November
From the South Rim Trail. Taughannock Falls, New York State Park, Ulysees, Tompkins County, Finger Lakes Region.
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Ice eventually nudged my walk onto Gorge Road, which parallels the South Rim Trail like a quieter narrative strand. Here, the landscape shifts from wild drama to human memory. A curve in the road reveals a farmhouse, modest and fragile beside its outsized barn. In winter, the absence of leaves makes the scene stark and honest. The farmstead buildings do not ask for nostalgia; they simply stand, bearing witness to lives tethered to this steep land. The structures emerge gradually as I walk downhill, as if the land itself were choosing when to reveal them.

Overview of this small cemetery overlooking Cayuga Lake

A short detour leads to a small cemetery perched on a shelf above Cayuga Lake, near the Taughannock Farms Inn. In winter, cemeteries feel less like places of mourning and more like rooms of quiet conversation. Headstones rise from frozen ground, their inscriptions softened by time and distance. From this vantage point, lake and sky merge in pale bands, and the lives commemorated here feel gently folded into the larger story of the landscape. The dead, too, are part of the park’s web of connections.

Another detour brings the lower falls into view—a more intimate expression of the same water that plunges dramatically upstream. Here the sound is closer, the movement more conversational. It is easy to imagine this water traveling, moment by moment, linking ravine to lake, winter to spring, memory to presence.

One of many Rim Trail overlooks. That is the Gorge Trail, below.

Rejoining the rim trail for the final climb north, the gorge offers repeated overlooks where the Gorge Trail can be seen threading below. These moments collapse distance: walker and walker, above and below, bound by the same route at different elevations. Over the course of roughly three miles and almost 600 feet of cumulative elevation change, effort becomes its own reward. Two hours pass not as measured time but as a sustained attentiveness, a gift winter offers to those willing to meet it on its terms.

Walking these trails in winter is about entering a conversation with the land—listening to ice, stone, water, and history speak in a quieter register. The joy lies in connection: trail to trail, gorge to road, past to present, and walker to place. In winter, Taughannock invites, gently and honestly, those who are willing to walk slowly enough to see.

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Glacial Kettle Bog Wonders: Photographing Pitcher Plants at the O.D. Engeln Preserve in Freeville

Step onto Freeville’s O.D. Engeln Preserve boardwalk and meet purple pitcher plants in a glacial kettle bog—carnivorous beauty, hidden blooms, and macro-photo magic.

Seen from 1000 feet above in Google Earth, the O.D. (Von) Engeln Preserve at Malloryville Road lays itself out in two glacial “kettles,” pond and bog; a simple diagram drawn by ice and time, then complicated by everything that has happened since. In my photograph, taken from the bog observation platform on a July morning, the sky is rinsed blue, clouds billow, conifers stitch along the rim around open space. Step closer, or lower your lens, and the openness resolves into a crowded, intimate architecture of sedges and moss, twigs and standing water, sunlight and shadow.

I came here for a plant that does not announce itself the way wildflowers often do. The purple pitcher plant, Sarracenia purpurea, is a quiet scandal: a green vessel in a place where green should be satisfied simply to survive. I arrived equipped for attentiveness—an iPhone for the broad scene, and a Canon DSLR with the F2.8 100 mm macro lens for the stars of this bog. The macro lens is an instrument of humility. It forces you to admit that the important drama is often no bigger than your palm.

In earlier years, the pitchers could be found right where a visitor naturally looks—within the central cut-out of the observation deck, close enough to lean over and study. But the bog is not a museum display; it is a living negotiation. This season, highbush blueberries pressing in from the margin had crowded the pitchers out, pushing the flowering plants into the grasses eight to ten feet away. The shift is small in human terms, the kind of distance you cross without thinking. In bog terms, it is displacement—an erasure of a familiar scene, a reminder that rarity is not only about numbers but also about space.

The pitchers themselves—those “turtle socks,” as they’ve been nicknamed—sit at ground level in a rosette, their mouths open to weather. Sunlight floods the cups and turns them into something both domestic and uncanny: a set of green, veined slippers left out to air, or a cluster of small amphorae awaiting an offering. In the bog’s thin soil, nourishment is hard-won. The pitcher plant answers that poverty with invention. Instead of arguing with the chemistry of peat, it borrows from the animal world—luring and taking what the air can spare. The cup is a trap, yes, but also a reservoir: rainwater gathered and held, a miniature wetland that mirrors the preserve’s larger one.

There is a tension here that never quite resolves: the plant’s beauty, and the plant’s appetite. We admire the cup’s red veining, the glossy rim, the way the opening flares like a lip; then we remember what the lip is for. We admire the flower’s elegant sheltering forms; then we realize the shelter is also a funnel, a choreography. This is not cruelty—no more than winter is cruelty. It is adaptation made visible, a lesson in how form follows need, and how need can produce something unexpectedly lovely.

And yet the real marvel—the reason I came that day—rises above the traps on a strong stalk, lifted clear of the dangerous mouths below. The flower is not purple in the obvious way its common name promises. It is subtler and stranger: a suspended structure with the poise of a lantern and the protective logic of armor. It struck me as a flower unlike any I have experienced, resembling an insect carapace, with the reproductive element underneath a hood. That hooded design feels less like ornament than strategy—an architecture that guides a pollinator’s route, controlling entrances and exits the way the pitcher controls the fall of an insect.

Even the flower’s back side refuses to perform for the camera. From the posterior angle, “there are only bracts”—plain supporting structures, the botanical equivalent of scaffolding left in place once the facade is finished. The bog, too, shows its scaffolding everywhere: dead stems, old wood, peat-dark water, last year’s leaves. A preserve is never only what is blooming. It is what persists.

I found myself thinking about the details I wanted but could not quite capture that day: the downward facing hairs inside the pitcher—those one-way bristles that make retreat difficult once a victim has slipped in. I or my lens was not up to this challange. The shortcoming was minor, but instructive. The bog offers glimpses, not guarantees. It invites return visits, different light, different seasons, a different kind of patience.

Standing on the platform I felt the preserve’s central truth: these are landscapes shaped by constraint—by ice, by water, by nutrient scarcity, by the slow encroachment of shrubs—and yet they keep producing improbable forms. The purple pitcher plant is one of those forms: a green cup that drinks rain, a flower that wears a hood, a turtle sock that turns hunger into design. In a place where the ground itself seems to refuse abundance, the plant answers with a different kind of richness—an elegance that is also a solution.

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Bells for Christmas

The symbolic power of the numeral three, reflected in various cultural, religious, and secular contexts, underscores its universal significance. From the mystical trinities of gods to the practical applications in rhetoric and storytelling, and the fundamental structure of our physical world, the number three resonates with a sense of completeness, balance, and harmony. Its pervasive presence in different aspects of human thought and culture attests to its enduring and profound symbolism.

Continue reading “Bells for Christmas”

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.

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.

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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Distant Sapphire III

From a modest bench above Taughannock Gorge, Cayuga Lake shifts from distant glimmer to presence—a quiet invitation to pause, breathe, and follow the water down.

From the south rim of Taughannock Gorge, Cayuga Lake appears like a distant strip of sapphire, framed today by a soft veil of hemlock and oak. The overlook here is modest—a fence, a bit of open sky—but someone wisely added a comfortable bench, an invitation to pause between gorge and lake, rock and water.

I stood in front of that bench, resting the camera body on the fence, fingers braced against the wood to steady the shot. This is not the grand, sweeping vista of a postcard. Instead, it is a quieter, more human vantage point, the way a person actually encounters the lake after walking the rim: emerging from the trees, breath easing, eyes adjusting to the light on water.

From here, the trail descends toward Cayuga’s shore, each turn bringing you lower and closer, trading the lofty perspective for the intimate sounds of waves and stone. In Distant Sapphire I and II, the lake was a glimpse—caught between branches, distant beyond the gorge. Now, in this “Bench View,” the water feels nearer, almost within reach, as though the landscape itself is drawing you gently down.

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I’ve gathered the three photographs—Glimpse of Cayuga Lake, Gorge View with Oak Leaves, and this Cayuga Lake Bench View—into a small gallery, a progression of approach. Each frame is a step closer: from suggestion, to invitation, to the quiet promise of the bench, waiting for whoever needs to sit and look a little longer.

A gallery of the three Cayuga Lake photographs for comparison.

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Distant Sapphire II

Cayuga waters reflect a blue November sky.

Cayuga Lake from the south rim of Taughannock Gorge, seen through a veil of hemlock with a carpet of fallen oak leaves, foreground. This is a companion to the previous post, both were handheld. For this the foreground was included to increase interest. For added stability, I rested the camera body on the fence bracketed with my fingers.

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A gallery of the two photographs for comparison.

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Distant Sapphire I

Cayuga waters reflect a blue November sky.

Cayuga waters reflect a blue November sky.

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Photographs in Gallery

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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.

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.

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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