A Ride to Reavis Ranch

Some history and exploration

….continued from the chapter “Desert Luxuries”

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

An Invitation from The Searcher

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

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

Click any photograph for a larger image.

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

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

To Reavis Ranch on Horseback

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

Nugget in Horse Heaven

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

McLEAN BOGS has been designated a REGISTERED NATURAL LANDMARK

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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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.
Click any photograph for a larger image

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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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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“Great Blue Herons at Cocoa Beach: A Space Coast Morning on the Atlantic

Along the luminous seam of surf and sand, a heron reads the tide’s slow grammar, patience embodied, until water yields a silver secret and morning becomes ceremony.

We walk the long seam where the Atlantic writes its restless script, and our beachcombing becomes a study in attention. The shore’s edge—where foam loosens shells from sand and the wind arranges salt on the tongue—draws other walkers too: grey herons, patient and arrow-straight, patrolling the surf line as if reading a language older than tides. They halt us without trying. We stand, quieted, while they work the boundary between water and land, between hunger and satisfaction.

I pack an iPhone sometimes for beachcombing as a lightweight alternative to SLRs. This post features iPhone photographs.

Along this narrow world of sand and surf, herons keep two distinct manners. Some linger near anglers, learning the thrift of handouts and the craft of appearing inevitable. Others refuse that bargain and hunt on their own, staking the wash with a slowness that is not delay but method. These independent operators move along the ocean’s margin: high enough to let the breakers fold ahead of them, low enough that their long legs stir the small lives hidden in the cross-hatching currents. To follow one with the eye is to adopt a different clock. Sandpipers skitter and dash; the heron lengthens time.

A perfect place to stalk the surf

At first the bird seems merely spellbound by light on water. Then a shift: a narrow cant of the head, the smallest realignment of the eye to the glare. The neck—serpentine and stored with intention—uncoils quick as a strike, and the bill cleaves the surface. The world either yields or it doesn’t. Often it doesn’t. When it does, the beak lifts an impossibly large, glinting fish, as if the ocean had lent out a secret.

Success!!

What follows is ceremony. The heron stands and calibrates, turning the silver length with almost invisible nods until head and prize agree. A sharp jerk aligns the fish with beak and gullet; the upper throat swells, accepting the whole, unchewed. Two more pulses and the catch is a memory traveling inward. It is an astonishment every time, not because we do not understand what is happening but because we do, and still it exceeds us.

We carry a smart phone on these morning circuits, a slim stand-in for heavier glass, enough to witness without intruding. Backlit by the early sun, the herons are cut from bronze and shadow, working the luminous edge while the day composes itself behind them. In the afternoons we meet fewer of the solitary hunters when the strand belongs more to the opportunists near the thinning knots of anglers. Why the shift, we cannot say. The ocean has its schedule; so, it seems, do its readers.

If we keep our distance, we are permitted to watch. Cross a line we don’t perceive and the bird will rise all at once, the long body unfolding, the voice a rasping scold torn from the throat of reed beds and marsh dawns; but, grant it enough space, and the heron returns us to the lesson it keeps teaching: that patience is a kind of movement; that the boundary of things is where change is clearest; that the most astonishing acts require the courage to do very little, very well, for a long time.

We come to linger where the waves erase our tracks, apprenticed to that slow grammar, trying to learn the tide’s careful verbs before the light turns and the day becomes something else—a different text, the same shore, the heron already a thin signature against the horizon.

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