Back to StoriesThe Winterkeeper's Great Chasm—As You've Never Known It Before
The Grand Canyon of the
Yellowstone is a geyser basin like none other in the park. Yes, geyser basin. On cool mornings plumes of
steam from geysers, hot springs, and fumaroles rise from the canyon walls and
along the river’s edge a 10,000 feet below.
A member of an early
scientific expedition in 1869 turned in his saddle to sort out some pack
animals while his horse continued on the way as a trusted horse would, when the
animal suddenly stopped. He turned back
around to see that the horse had halted on the very rim of the abyss.
February 11, 2008
The Winterkeeper's Great Chasm—As You've Never Known It BeforeBesides being jaw dropping, the Grand Canyon of the Yellowstone has geysers, hidden spectacles and a mountain of volcanic rhyolite
February 11, 2018—Plunging Into The Abyss
The Grand Canyon of the Yellowstone, a wonder of the world and not well understood even by those who visit America's first national park often. One of the most widely photographed scenes in Yellowstone, Fuller strives to avoid cliches with his interpretation of the Lower Falls. Photo by Steven Fuller
Its edge begins a little more
than a quarter of a mile away from where I am writing these words.
The canyon is a river-eroded
transected geyser basin and cut into a mountain of volcanic ash leftover from
Supervolcano. The rocks at the head of the canyon down river from the Lower
Falls have long been and continue to be hydrothermally altered by hot acidic
water that rises through the networks of fractures that reach down to the
volcanic magma mass that underlies central Yellowstone.
This corrosive chemistry has
weakened and degraded the rhyolite lava bed rock so that it is more easily
eroded by the river than the harder unaltered rock at the Lower Falls, the
upriver boundary of the geyser basin.
In addition, the extreme
hydrothermal chemistry acts as a catalyst that alters the elemental components
of nature’s pallet of pigments, or more simply said, this is why the canyon is
so spectacularly colorful. The canyon continues today to be an alchemical
crucible of chromatic chemistry in action.
Mechanically, the Kodachrome canyon gash we adore is
the child of the raging melt water born of the very rapid final
wasting of the ice of the last glaciation that occurred about 12,500 years ago
that flushed the debris from the ancestral canyon and rapidly deepened the
canyon we know today.
In some places the upper end
of the canyon is almost as deep as it is wide, and since the rims are heavily
timbered the forest conceals the chasm until you come right up on it.
The photo here was taken from behind Fuller's cabin. "In the background, a plume of steam, water vapor, rises up and out of the canyon," he writes. "This ephemeral jewel of a light catcher is generated by the fall of the Yellowstone River over the 308 foot cliff at the head of the Grand Canyon of the Yellowstone."
A threesome of waterfalls is
closely associated with the Canyon: first the post card famous Lower Falls at the head of the
canyon. Second, a half mile up river,
the109-feet-high Upper Falls.
"On a subzero morning shortly after sunrise floating frost crystals born of hot springs deep in the Canyon fill the air," Fuller writes. "There are two shapes of crystals. One acts as a prisim that separates white light into the spectrum of colors visible to us and a second form that reflects white light like a mirror. A photo cannot convey this nuance, but if you have the good fortune to see this in the real world, and take the time to look deeply, you can see the light show of both crystals dancing."
Between the two the river
follows a sweeping “J” (“hockey stick”) course where, midway the parent
creek of the close-by Crystal Falls, a 129 feet high triple cascade, joins the
river. Isolated from these three a fourth, Silver Cord Cascade, descends 1200
feet down a vertical wall on the south side of the Canyon three miles downriver
from the Lower Falls.
My house sits about two New
York city blocks distant from but directly overlooking the Lower Falls which is
hidden from view situated as it is deep in the narrow chasm at the head of the
canyon. The Lower Falls’ location is usually obvious because of the plume of
water vapor that rises from it for hundreds or even for a thousand feet or more
into the sky.
I wish I could appropriate
the African name for Victoria Falls, which would be as appropriate here as it
is there: “the smoke that thunders.”
The house faces south
south-east so the plume is backlighted at sunrise and whenever a cold clear
night is coincident with the rise of a full moon the plume appears luminescent,
as magical as a towering genie.
In the spring, at the end of
hot sunny days when rapid snow melt has swollen the river, the roar of the
falls fills the night. Surprisingly the
noise doesn’t come from the Lower Falls directly below me where the river
crashes over a 300 feet high cliff but from the Upper Falls, almost exactly
twice as far, .08 of a mile away.
The reason is obvious when
you stand at the brink of the Upper Falls looking down river where the
spreading canyon walls form a megaphone that points directly at the house.
"Beautiful and seductive, the Canyon is a widow maker. The Canyon is hungry, its hydrothermally degraded walls are often crumby or clay slicked. I have thought of the canyon as an ambush predator, like the sand trap of a giant ant lion."
When low clouds hang over the
Upper Falls and the acoustics are just so I can hear the sounds of the riffles
in the river below the falls…some evening I expect to hear the song of a water
ouzel (American Dipper)—“the bird that flies underwater,” splashing around
down there, almost a mile away.
Beautiful and seductive, the
Canyon is a widow maker. The Canyon is hungry, its hydrothermally degraded
walls are often crumby or clay slicked.
I have thought of the canyon as an ambush predator, like the sand trap
of a giant ant lion, where the unstable materials around its’ perimeter invite
a fatal fall into its maw.
"A winter snowstorm embellishes this old pine snag that has extended a formidable root in an attempt to belay the itself from being drawn into the maw of the canyon," Fuller notes. "Think of clawing your fingernails in slow motion into the top edge of a cliff with a 1,200-foot exposure. Eventually the pull of gravity over-whelmes the life force in all of us." Photo by Steven Fuller
People do fall into the
canyon. A motorist backed his car off
the north rim until gravity irresistibly captured them, killing him and his
wife. A sundry have slipped to their
deaths. Others have been killed by rocks
falling or thrown into the canyon.
One young man committed
suicide with a spectacularly romantic leap onto the brink edge of the lower
falls. The father of a longtime Yellowstone friend of mine recalled the time he
encountered the corpse of a female, “her buttocks partially emergent, white as
ivory” at rest in a favorite fly fishing hole where she had washed down from
the upper Yellowstone.
Two men died when climbing
the 1,000-foot Silver Cord stalactite of ice attached, until they descended it,
to the south wall of the canyon late in May. In the early 1950’s several
visitors reported witnessing a bear fall fatally into the canyon, so it is not
just us tourists that mis-step.
In winter the Lower Falls is
mostly sheathed in ice while a pile of snow and ice accumulates at its’ foot
which in some years is massive. The top of the mass may reach near to the brink
of the falls, other years it assumes the form of an asymmetrical, but pleasing
cone, or it may evolve as a low slung ridge of ice.
“Tom Thumb,” a small geyser near the foot of the Lower Falls was historically accessible at the terminus of Uncle Tom’s Trail near the base of the cataract. Tom, an early private tourism purveyor, created the trail in the decades after Yellowstone was created. Subsequently, much having to do with resource protection and liability reasons, the National Park Service shortened and reconfigured the primitive trail as an iron stairway that no longer terminated at the river level. A new trail will make its debut in 2018. Photo by Steven Fuller
Every winter its form is
different, reflecting variables in temperature, wind, precipitation, water
flow, and other less obvious mysteries of the morphology of ice cone formation.
Then, some warm mid-March day or night, the whole mass collapses, an event I
have never witnessed. Yesterday it was there, this morning it is gone.
In any season the canyon and
falls are an irresistible attraction for the aerially empowered. Every few years
several jet fighters do a couple of low wide turns around the falls
overwhelming everything else with their mega- thunder, vastly louder than the
falls can muster even at spring tide. The whop-whop of a single helicopter
indicates a rescue or recovery operation or sometimes an inspection by a
politician, or a film crew capturing a view unprecedented until now, late in
the Anthropocene. One afternoon a half dozen Hueys in formation paid an aerial
visit, ‘twere Ride of the Valkyries redux.
The canyon and lower falls
are a spectacle immortalized for more than a century on countless millions of
postcards, mega miles of film, petabytes of digital memory rendering most of us
numb to the reality of what an extraordinary space this place is. Most of us are more focused on bagging it
than absorbing it. Check it off the bucket list and hurry on to Old Faithful,
the Tetons, or back to wherever.
I have lived closely
proximate to this canyon and its’ trinity of waterfalls for many years but it
remains an elusive icon, like meeting a movie star in the flesh, how do you
connect with the person behind the famous mask, how do you see into a landscape
become a national cliché?
In one of various intimate
forays with this place I once attempted to walk at river level from Seven Mile
hole (7 miles below the Lower Falls) to Tower Junction, a further fifteen miles
downstream. Along the way trout were
abundant and naïve and easily caught in the deep clear pools. On the sylvan bench of a side canyon I found
the undisturbed bones of a venerable bull bison and a cast iron griddle and a
rusted out frying pan. Who, why, and when remained unanswered.
With increasing frequency
sheer cliffs reached down into the river forcing me to climb high in order to
by-pass them. Game trails, mostly mule deer, showed the best routes, though in
places were so precipitous I wondered if there were goats locally resident.
Once past the cliff I dropped
back down to the river until around the next bend I encountered the next cliff
and again and again the whole strenuous process was repeated. The trout weren’t
the only naif in the canyon, call me Candide.
Having budgeted only three
days for the jaunt I climbed out of the canyon on the third day and proceeded
along the rim trail the rest of the way to Tower and my pick-up at the
appointed time. Pleased, I had experienced a bit of the canyon seldom seen.
Undoubtedly the most
successful visionary of the Canyon was the great American painter Thomas Moran.
During two of the forty days he first spent in Yellowstone in 1871, in company
with the Hayden Geological Survey, he sketched many details of the canyon and
falls which, upon his return to his studio, he incorporated into his 7 X 14-foot opus, “The Grand Canon of the Yellowstone 1872." (See at bottom.) This magnificent work
was instrumental in inducing Congress to create Yellowstone as a national park.
The canvas is not a literal
portrays of the Canyon, rather it is a faithful composite of the whole, a
montage of elements based on the details sketches he made on site. As I walk or
ski the canyon I sometimes experience a mild epiphany when I recognize some of
those details that he rearranged and incorporated in a true rendering of a
sense of this place that transcends the photographic.
The painting is a movable
feast of saturated colors and shifting illuminating light cast on the canyon
walls via drifting mottled translucent clouds after a summer rain. His
rendering of this synergy is one I attempt to re-experience each summer when,
on rare occasions, all of the right conditions harmonize and confirm the
palette of canyon colors and the play of light Moran faithfully portrayed in
this wonderful work.
The details: within the canyon the perfect sweep of a
mount Fuji curve (very Hokusai) that defines the mound in the middle distance, the
scattering of pines throughout the canyon that have pioneered the unlikely but
live-able niches on the canyon walls (“bloom where you are planted”), the
desiccated twisted snags, those tortured skeletal Yellowstone bonsai.
On the wall of the canyon he
portrays the familiar creep of a dark vegetative mat below a hot spring, in
another the multi colored aqueous abstract patterns that recall the ancient art
of marbled paper
And the peripheral details,
small, but they convey the landscape context in which the Canyon exists. The
speck of an eagle high in the sky, small plumes of steam that mark hot springs
on the walls of the canyon. In the far
middle distance he acknowledges Hayden Valley. And, most appropriately, the
plumes of hot springs and mud pots at Mud Volcano eight miles to the south.
Every February for a short time in Yosemite National Park, sunshine strikes Horsetail Falls and creates a visual effect that resembles a waterfall on fire. Similar kinds of phenomena happen in the Grand Canyon of the Yellowstone depending upon the seasonal arc of the sun, weather and steam pouring out of the ground. "What marvelous hot springs lies hidden in this canyon cliff cleft revealed on this cool morning by an ephemeral tease of steam," Fuller writes of this image. " Photo by Steven Fuller
On the far southern rim of
the Yellowstone plateau, way beyond the canyon focus of the work, he portrays a
suggestion of snowy mountains, or be they clouds?...or both? Ambiguity is
rampant up here on the Yellowstone Plateau, one of its’ many charms.
The painting is “psychedelic”
in the sense that it “creates an elevated sense of awareness” of the wondrous
nature of this “scenic climax”, a term in the lexicon of the modern scientific
formulaic criteria used to quantify the aesthetic values of scenery, usually as
a means to monetize the place. Master
artists, conflicted poets, and the simple minded recognize the canyon’s
numinous nature on first sight, no spreadsheet required.
Moran was first a master of
observation, seeing the whole in the mélange of the details, then on the canvas
he was a master colorist with the technical skills to convey his poet’s minds’
eye.
Osborne Russell, the first
and the last of the literate mountain men who knew Yellowstone in the late
1830s, put it well, “For my own part I almost wished I could spend the
remainder of my days in a place like this where happiness and contentment
seemed to sing in wild romantic splendor”.
Moran said something similar and so do I.
Of course, it was viewed for
the first time by humans long, long before that. Native people frequented the
interior of the park since at least 9,000 years ago, though I am not aware that
any evidence as old as that has been found in the canyon area.
The first evidence of a person
with European ancestry visiting the Canyon were the initials “J.O.R. and the
date “Aug 19, 1819” near the Upper Falls. The graffiti was last reported in the
1890s when it had naturally grown over and was nearly indecipherable. Thereafter
it was lost.
In the 1890s there was a
serious proposal to build an elevator to the base of the lower falls, an
amenity attractive to the less robust amongst the visitors of the time and a
revenue generator for the more entrepreneurial/savvy among us. Opponents of the
idea were disparaged as elitists. Such thinking more broadly about nature still
echoes today.
EDITOR'S NOTE: Click here to read all of Steven Fuller's journal entries for "A Life In Wonderland" and this Mountain Journal profile of Fuller, "Twilight of the Winterkeepers". Enjoy Thomas Moran's painting, below.
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