Two Nature Abstracts, macros of Reavis Creek below the falls
The light of a early spring desert afternoon on a broad rock shelves along the creek.
I spent a day hiking in, two days hiking out and a day of canyoneering to the foot of Reavis Falls. The featured (i.e. “header”) photograph is a view of the inner canyon, the raw material for these abstracts.
I received notice of IStock acceptance of select photographs from my last posting, “Wilderness Textures”, was accepted. Click to view my IStock Portfolio, including photographs from today’s posting included in the acceptance notice.
In this post I move up the Reavis Creek canyon from where the last posting, “Wilderness Textures”, was sited to the foot of Reavis Falls. With the first photograph you look up at the falls from the head of the canyon carved by the creek over eons. The rock wall, the canyon “head”, is thick with microorganisms, fungi, mosses.
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In the foreground is a jumble of boulders, some washed down at flood time, spread wide at the bottom of the falls, piled to a jumbled height of 15 feet.
Talus is the geological term for this formation. Derived from the Latin word for slope (talutum) the definition, from the Oxford English Dictionary, is “A sloping mass of detritus lying at the base of a cliff or the like consisting of material fallen from its face.”
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The ankle bone is also called talus, from the French word for heel, I bring it up because climbing this chaotic, unstable jumble is a way to break your ankle. The route to Reavis Falls, a climb up one side of Lime Mountain then down the other on a non-existent (lightly marked) trail, is rated difficult and impossible with a broken leg or ankle. I was alone and very careful to check each rock for stability before putting my weight on it.
A climb of the talus pile was necessary to view the pool at the waterfall base, for this photograph.
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A more artistic vertical format version, below, captured with the Canon EF 100mm “macro” lens. All shots are using the Kodak DCS pro SLR-c (the “c” designated Canon lens compatibility) and a Manfrotto studio tripod with a hydrostatic ball head. The horizontal format shot was captured with a Canon EF 50mm f/1.4 USM lens. I prefer the vertical version, artistically, because the talus jumble is all but cropped out while the upper corner of the angular basalt boulder is left as an interesting focal point. The boulder, not being in the spray, is in focus to contrast with the basalt wall behind the water.
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I captured a series of shots from this precarious vantage point, working up from the pool to the brim of the waterfall.
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My goals was a composite photo of the falls. I have yet to succeed with this project. Maybe I will give it one more shot in spite of having learned the hard lesson the best photographs are a single moment captured in a single frame.
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I find in this series the vertical aspect is more artistic. The water volume, of the falls, at this time of year offers only the finest of sprays with most of the basalt rock wall only moist. The 100mm “macro” lens allowed me to include only the falling water with a bit of the moist wall for contrast.
In the following version I experimented with color, moving from the narrow range of hues, to more contrast.
These abstracts are some of my photographic output from four days and nights spent alone in the remote eastern Superstition Wilderness. For the first three days I met not a soul, all these images were captured on a single afternoon spent in the canyon below Reavis Falls, a jumble of landslides, flood debris and boulders. There is no trail. The few people who enter the canyon must negotiate around boulders, crossing Reavis Creek many times.
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My backpack kit included a full sized Manfrotto studio tripod with hydrostatic ball head. The benefits more than outweighed the effort (I was a lot younger in 2008) when the Canon EF 100mm (macro) lens is mounted on a Kodak dSLR body, allowing me to take crisp shots. The tripod legs can be adjusted to precise positions for stability.
I can feel the bright afternoon desert spring sunshine in this photos. It was after the spring floods, the flow of Reavis Creek and ample still but slow. Gathering in pools over the rough stones of the creek bed, the water absolutely clear.
I held the shot over many minutes, capturing ever changing diffraction patterns.
We see in all these photos, not a homogenous blend of stones from a shared geology. Reavis Creek washes over diverse geologies: volcanic, ancient igneous extrusions, sedimentary and metamorphic are jumbled together.
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This is a series of photographs of smooth, white igneous boulders with shadows of still leafless sycamore and cottonwood trees.
Graceful shadows
Strong, demonstrative shadows.
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A leaning cairn, not a trail marker….
A 15 foot high jumble of stones piled at the bottom of Reavis Falls, carried over by the floods.
In this post we start the day of my posting “Family Trek“, July 19, 2008, when, well before the sun rose at 6:23 am Mountain Daylight Time (the Navajo Reservation observes daylight savings, the rest of Arizona does not), Pam and I were at the Spider Rock Overlook.
Most visitors to the canyon make use of a system of roads and parking lots next to strategic views. There is the White House Overlook we visited our first day, July 18, to hike from the trailhead into the canyon. There are also, on the south side of the canyon:
Tsegi Overlook, taken from a Navajo word that translates directly to “between the rocks” and usually refers to a deep canyon with steep cliffs.
Junction Overlook above the point where Canyon Del Muerto (see my posting “Sun and Shade, Canyon Del Muerto”, and Canyon De Chelly intersect. There is an Anasazi ruin in the south-facing cliff across the canyon.
Sliding House Overlook, another Anasazi run across the canyon.
Face Rock Overlook, to view the eponymous formation.
Spider Rock Overlook, the most stunning rock formation.
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Looking east from the Spider Rock overlook, Canyon De Chelly.
While getting ready I scoped out the location for interesting visual tropes. Utah Junipers are exceptionally hardy shrubs, stressed individual plants grow into compelling forms shaped by hardship. As the sun rose, this specimen emerged from the gloom and caught the first sun rays.
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A distressed Utah Juniper on the edge of Canyon De Chelly overlooking Needle Rock a few moments after sunrise.
In my post Canyon of Music, Wind, Light I shared a different photograph of this beetle crawling on sandstone, naming it as a “dung beetle”. I had assumed it was one from once having seen a beetle in an Arizona desert pushing a ball of dung around. This morning, to confirm my assumption, I searched for images of “Arizona Dung Beetle” and was dismayed to find this beetle shares no characteristics with the photographs. Absent smoking gun evidence, sadly lacking in this photograph, I have to admit my “dung beetle” attribution is in error.
Supporting the beetle, the luminous surface of the red sandstone named “de Chelly,” sunlight reflects from durable remnants of the ancestral Rocky Mountains wore to these bits of rock, piled to mountainous dunes by the winds of tens of thousands years, polished to smoothness each against the others.
Mysterious abrasion and grooves in a de Chelly sandstone cliff, Canyon de Chelly.
The above photograph is a detail from the brightly lit cliff of the following photograph. The desert varnish and underlying rock was weathered over thousands of years, the sand grains falling to the canyon floor.
The soil of the canyon is composed of these bits of the ancestral Rocky Mountains. What appears to be a white road in the above photograph is not man-made, it is the dried bed of a stream. When a waterway is dry like this, only flowing with rains, it is called a wash. When water fills the wash of the Canyon Del Muerto, the polished sand granules become a dangerous morass, sucking down horses, people, anything unlucky enough to step into it. Every movement, struggling for freedom, pulls the victim deeper down until the wet sand closes over the head and suffocation and death ensues.
Stairs cut into the sandstone cliff of Canyon de Chelly
The waters Canyon De Chelly National Monument naturally form a vast Y into the Defiance Plateau, naturally because two major streams merge into one canyon a few miles above Chinle. On both our guided trips, heading east from Chinle there is a branch. On the right De Chelly canyon continues. On the left is Canyon Del Muerto. The photos in this post are all from “The Canyon of the Dead”, what the name means translated into English.
No, it is not named this because of the quicksand. Conditions for quicksand are present throughout canyons of the southwest. It is history of human occupation for which this canyon was named. I will cover it in a future posting. For now, I will say the above views are from the spot featured in “Family Trek.”
My first visit, in 2003, while my son Sean climbed the rocks with our guide, I was left to document the wondrous surroundings. The above shallow cave is reached by that stairway carved into the precipitous ledge. The access to the cave is via those naturally occurring ridges of the cross bedded sandstone. It is another example of De Chelly sandstone formed from the windblown edge of a monstrous ancient sand dune.
A solid block of De Chelly sandstone formed from the central bulk of a sand dune.
Here is another example of rock formed from the solid body of the sand dune, that unbroken and un-striated cliff. Below is the cross-bedded, windblown sand.
Autumn lights up the floor of Canyon De Chelly, the foliage rivals the cliffs for wonder at this time.
As we proceeded generally east from the climbing spot of “Family Trek”, driving by the golden cottonwood foliage I asked the guide to stop for these photographs.
Canyon walls
Soon the cliffs hid the sun.
Notice the modern water distribution system (pipe) at the foot of cliff on right. These vast tracks of shadow adjacent to bright sunlight are a fact of life for canyon dwellers, a source of joy and wonder.
The canyon here is rather like the Narrows of Zion, without the water.
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