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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

Click Me for the first post of this series.

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Atkinson Hall and the Quiet Confidence of Good Design

A new Cornell building settles into its hillside, glass and weathered metal catching sky and trees—less a declaration than an invitation to pause, wander, and think together.

Learning the Shape of a New Building

I first noticed the building from above.

Not in person—on my screen, late at night, when I should have been revising a draft and instead opened Google Earth the way some people open a window. There it was, just off Tower Road, close to Stocking Hall, pale and newly settled into the slope. From that height it looked careful rather than confident, as if it had arrived recently and was still deciding how much of itself to show.

Atkinson Hall, Google Earth from August 2023, 350 Tower Rd, Ithaca, NY 14850

I remember thinking: good placement on a former triangular parking lot. Enough distance from the older buildings to breathe, close enough to feel included. The hill does most of the work. You can see that even from an overhead height.

The next morning I walked there.

Atkinson Hall as viewed from the open field south of the Nevin Welcome Center of Cornell Botanic Gardens

Across the open field the building didn’t announce itself. Trees intervened—pines, bare hardwoods—so that it came into view in pieces: a curve of metal, a long line of glass, brick holding the ground. It felt less like approaching a destination than like gradually realizing you were already there. I liked that. Buildings that reveal themselves all at once tend to exhaust me.

The slope matters. You feel it in your legs as you walk, and the building seems to acknowledge it, stretching rather than standing tall. It does not pretend the land is flat. It follows the descent toward the creek, toward the older geological story underneath all of us.

Up close, the materials settle my attention.

North Side of Atkinson Hall, 350 Tower Rd, Ithaca, NY 14850

Brick at the base—solid, Cornell-familiar, not trying to reinvent anything. Above it, bands of weathered metal curve gently, already carrying the muted browns of fallen leaves, old stone, and stream-worn shale—colors long familiar to the slopes and ravines that shape this campus. They look as though they have agreed to age, which feels like an underrated design choice. The glass holds the sky without insisting on transparency. Some days it reflects trees so clearly that the building nearly disappears into them.

Compare the facade brickwork of Warren Hall, one of the earliest buildings on the Cornell University campus, completed 1868. This is the southwest corner with facade signage, Cornell University, Ithaca, New York

I stop near the windows longer than I intend to. The view steadies me. The hillside, the trees, the quiet persistence of winter light. My notebook stays closed for a few minutes. No one seems to mind.

View near Atkinson, Nevin Welcome Center, Cornell Botanical Gardens, 124 Comstock Knoll Dr, Ithaca, NY 14850

Inside, the building does not behave like a department.

That is the first thing I notice once I begin using it regularly. No single discipline claims the space. Offices and meeting rooms feel provisional, lightly held. Conversations drift. Someone from engineering crosses paths with someone from policy. A food systems researcher borrows a chair from a planner. No one looks lost.

It helps to remember who gathers here. The building hosts people from many parts of the university, each arriving with partial expertise, incomplete questions.

Cornell College / UnitAreas of Engagement
College of Agriculture and Life Sciences (CALS)Food systems, agroecology, climate resilience
College of EngineeringEnergy systems, materials, infrastructure
College of Arts and SciencesEarth systems, ecology, human dimensions
SC Johnson College of BusinessSustainable enterprise, supply chains
College of Architecture, Art, and Planning (AAP)Urban resilience, adaptive design
Cornell Law SchoolEnvironmental law and governance
Public & Global AffairsClimate policy, diplomacy

I keep this list taped inside my notebook. It reminds me that no one here is meant to arrive fully formed. The building expects us to be unfinished.

Cobblestones with fallen oak leaves along Feeny Way, Cornell University, Ithaca, New York

There is a quiet confidence in how the place is run. Systems hum discreetly. Heat holds steady even when the weather rips. Somewhere nearby, unseen, a generator waits, a reassurance. Work continues. Conversations do not end mid-sentence. I think about this more than I expected to. Stability has become a form of generosity.

On certain afternoons I walk the exterior again before heading home.

The curves soften what could have been institutional. Corners ease into one another. Nothing feels sharp. The building does not posture or instruct. It listens. It seems content to let weather, foot traffic, and time finish the job.

I have overheard visitors describe it as “restrained.” I think that is right. It does not wear sustainability as an emblem. It does not ask to be admired. It offers something quieter: space to think without being hurried, to talk without being territorial.

From some angles it nearly disappears into the hillside. From others it asserts itself just enough to be useful. That balance feels intentional, and also rare.

When I sit near the glass and look out, I sometimes imagine the building learning us in return—our habits, our pauses, the way we linger in doorways when a conversation matters. It seems designed for that kind of noticing.

If I were forced to describe it the way a realtor might, I would say it is well built in all the ways that matter. The structure is sound. The site is excellent. The materials will age well. But what I would mean is something less technical.

It is a building willing to wait.

Seen from above, it is still new.
Seen from the field, it is already settled.
Seen from inside, it feels patient.

That patience makes room—for uncertainty, for collaboration, for the long work that does not resolve quickly. I think that is why I keep returning, even on days when I do not strictly need to be there.

The building does not ask what I am producing.
It asks only that I stay awhile.

And for now, that is enough.

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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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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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Climbing Piestewa Peak: Multicultural Pilgrimage to a Phoenix Desert Dawn

In the cool predawn, strangers from every background climb a stone stairway above Phoenix, trading city lights for desert silence as sunrise spills gold across Piestewa Peak.

Arriving at 5 am there is a line of trucks and cars and Piestewa Peak parking almost full when I grab a spot in the predawn darkness. The desert air has that deep, merciful coolness it offers before sunrise, edged with the long-remembered scent of creosote. Car doors close with soft thuds, headlamps blink on, and a loose procession of strangers begins to funnel toward the trailhead like pilgrims, even now white and red headlamps sprinkle the upper slopes.

At first the climb exists only in a narrow cone of light, my lamp illuminates the scant gravel, uneven steps, and each scuff of boot or shoe sounds loud in the hush. Somewhere below, the city hums, but here the conversation is mostly breath and the occasional murmur of greeting as we fall into the rhythm of the climb.

My beam catches a young couple just ahead, their hands knotted together. They speak Spanish, laughing quietly as they miss a step and bump shoulders. Behind me an older man in a Veterans cap leans heavily on trekking poles, his companion—maybe daughter, maybe friend—matching her shorter stride to his with patient care. A group of women in bright leggings and braided hair moves past us in a burst of energy, their languages overlapping—English, maybe Vietnamese, something I cannot place—like the weaving of a rug. A man passes me, a drum on his back. Piestewa draws them all, before dawn, to this rib of stone in the center of the Phoenix basin.

As I stop to rest myself and turn off my headlamp, ahead the trail tilts steeper the steps fade to rock, irregular and unforgiving: a stairway carved from ancient volcanic bones. With my dark adaptation, surfaces reflect star and city light, leading the eye down the ridge toward the dark quilt of neighborhoods below. Later, captured in the photograph, those steps will twist away like a stone dragon’s spine, the city waking beyond in soft pastels. Now they are simply work for legs and lungs.

The desert plants materialize around us as shapes before they acquire color. Saguaros stand like sentinels along the slopes; their arms lifted in silhouette. Ocotillo rise as witchy bundles of sticks, each spine leafed out from October rains the leaves catching a little light. On a small plateau a family has paused; the father adjusts a tiny headlamp on his son, no more than six, who is insisting, with fierce determination, that he can carry his own water. “Almost there, campeón,” his father says, and the child straightens like a soldier.

The dark begins to soften at the edges. Over the eastern horizon a thin band of orange appears, a delicate seam between night and day. In one direction, the city stretches out in a glittering net of streetlights, the squares of parking lots and subdivisions catching the last of the darkness. In the other, the mountains are still black cutouts, their profiles sharp as paper against a gradually brightening sky. One of my images will hold that moment: the jagged ridge of Piestewa in shadow, the valley below already spangled with light, a single towering saguaro rooted at the cliff’s edge like a punctuation mark.

November 2025 while visiting Pam’s family in Phoenix

Higher up, the trail narrows and the rock turns rougher. We fall into single file, strangers linked by a line of effort. A runner comes flying down, feet barely touching stone, breath steady and controlled. “On your left,” he calls, and we part for him like water. A woman with a hijab tucked neatly under her ball cap leans against the retaining wall, stretching a calf muscle, her friend counting in accented English: “Ten more seconds, you can do it.” Near one bend a hiker pauses to press a hand against the rock face, whispering a quiet prayer in a language I do not recognize. It is a small, intimate moment, gone almost before I register it.

The last push to the saddle is steep, the steps uneven, the sky now a cascade of colors—copper, rose, faint lavender melting into a high dome of blue. The silhouettes of distant ranges sharpen: the Estrellas?, the Superstitions?, low ridges whose names I do not know. On the horizon, the first thin line of sun breaks free, setting fire to the edges of clouds. In another photograph, framed by dark rock and desert trees, that sunrise becomes a golden portal at the end of a shadowed corridor of stone.

We reach a broad ledge just shy of the summit as the light finally spills over us. People are already gathered there: a trio of college students taking selfies, a pair of retirees sharing thermos coffee, a solitary man sitting cross-legged with eyes closed, face open to the warmth. The city below is suddenly transformed. The carpet of lights dims, replaced by the clear geometry of streets and rooftops, golf courses and parking lots, all laid out like a model at our feet. The mountains that hem the basin—once anonymous shapes—now reveal their ridges and ravines in sharp relief.

For a few minutes conversation dies away. Everyone seems to feel the same thing: that fragile instant when the sun clears the horizon and the desert shifts from silver-blue to gold. The rocks around us, sharp and broken in the photographs, glow honey-colored. Saguaros catch light on their spines, each thorn a tiny ember. Even the dusty air seems to shimmer.

Down below, a new wave of hikers starts up the trail, latecomers walking into full daylight. We, the predawn climbers, share a small, quiet complicity. We have seen the city from the backside of night, watched the day arrive from a perch of jagged stone. Piestewa Peak has turned us, for an hour or two, into a single, breathing organism: many hearts, one climb, all of us stitched together by the steep path and the slow unveiling of the sun.

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The Dún Aonghasa cheval de fries field

…this defensive structure evokes the enormous scale of the struggles around this place of defense. 

A span of 10,000 years spreads between now and the first possibility of settlement on the island of Eire, then swept clean to bare rock by the weight of ice.  Current scholarship of the Dún Aonghasa ruins, Inishmore, County Galway, the Irish Republic place a settlement within the inner of the four dry stone rings after 6,500 years (1,500 BC or 3,500 years ago).  By way of scale, the first settlement took about 30 times the duration of the U.S. Constitution ratification through 2025: the last state, Rhode Island, ratified the Constitution 1789.

By 700 BC, 2,700 years ago, a series of upright, closely placed stones, were erected between the second and third rings called a cheval de fries field (“Frisian horses” in English) today, this defensive structure evokes the enormous scale of the struggles around this place of defense.  

This is a portion of that field, I believe, taken as Pam and I approach the inner ring entrance, walking a wide path cleared of barriers.  Click the photograph for a larger image with caption.

Click the link for my Getty IStock photography of the Aran Islands
Click me for the first post of this series, “Horse Trap on Inishmore.”

References: search wikipedia for “Dún Aonghasa” and Google “cheval de fries definition” and “Dún Aonghasa.”

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University of Arizona Homecoming 2003: Cheerleading, Tradition, and Tucson

At my first UA Homecoming since ’75, I stepped back into the parade, camera in hand, capturing three airborne moments that felt like returning home.

In November 2003, at fifty and traveling Arizona with my son Sean, I returned to the University of Arizona for my first Homecoming since graduating in 1975. I’d made the freshman cheerleading squad my first year in Tucson, and when the alumni invitation arrived, I couldn’t resist.

ArizonaCheer2003
ArizonaCheer2003

At the cheer alumni reception on November 7, the room felt instantly familiar—handshakes, stories, and a current squad packed with scholars as well as athletes. I mentioned to advisor Phoebe Chalk that I hoped to photograph the parade. “The squad already had photographers”, she said, so I planned to work from the sidelines.

ArizonaCheer2003
ArizonaCheer2003

I came prepared the next day with a Sony Cybershot F828. It was “Sony’s flagship prosumer digital camera” at the time. It worked well that day, the variable lens was especially helpful.

ArizonaCheer2003

At the staging site, I solved access with a simple ask. I approached UA President Peter Likins, explained I wanted to photograph the cheerleaders, and he nodded, made a quick call, and waved me on. The team recognized me from the evening before, and I fell in step with them at the head of the procession

ArizonaCheer2003
ArizonaCheer2003

As we passed the Flandrau Science Center and crossed Cherry Avenue, a stunt group set quickly: bases J. Justin VandenBerg, Ricardo Abud (captain), and Robert Scoby with flyer Taylor Hendrickson. They launched her high for a full flip and clean catch. I caught the moment of collective focus—an image I call Mind.

ArizonaCheer2003

We progressed until the stunt group reset. This time I framed the instant of takeoff—limbs aligned like clockwork—I call this image Aerialists.

ArizonaCheer2003

The next flyer to launch was Kristen Ortega, here standing on the shoulders of her partner.

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In front of the review stand, flyer Kristen Ortega rose into a poised extension and flight returned safely to the same three pairs of hands. Grace is the image title. 

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The rest of the parade streamed past in a blur of alumni, bands, and banners. Afterward, a squad member took a picture of me with the team—two eras in one frame. The cheers change; the spirit doesn’t.

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ArizonaCheer2003-1
ArizonaCheer2003-1
ArizonaCheer2003-1
ArizonaCheer2003-1
ArizonaCheer2003-1

Click link for another posting about Arizonians, “Portrait of a Navajo Guide.”

Click link for another posting about Arizonians, “History and Ghosts of the Triangle T Ranch.”

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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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