Desert Stones and Ancient Walls: A Meditation on Rocks I Have Known

I have known rocks as obstacles, as shelter, and finally as memory. These ten photographs gather these moods: cliff, wall, ruin, creek-bed, boulder, altar, shadow screen, old page. They are not inert. They keep their own weather, their own grammar.

At Mesa Verde, in Montezuma County near Cortez, Colorado, there are cliff dwellings within and of the sandstone, as if a thought withheld. I am reminded those “windows” were doors, and that access to them depended on a toe-trail: a sequence of small depressions in the rock, secure only if begun with the correct hand and foot. These details stay with me, a place understood in the body. The rock was architecture, ladder, lock, and covenant.

House of Many Windows, Mesa Verde

In another photograph, the sandstone rises in immense vertical folds, scored and varnished, with ancient rooms tucked low against the wall. The scale is most moral. Human work appears small, but not trivial. A few stacked stones become a claim: we were here, we learned the wall, we lived under its patience.

The White House, Canyon de Chelly

Elsewhere along Canyon de Chelly a different intimacy is offered as petroglyph horses move across desert varnish on red sandstone, their bodies made by removing darkness. Since horses arrived with Europeans, the image carries a date without numbers. History appears as a pale incision. The rock remembers contact, disruption, motion, and the brief confidence of riders, a page that is best read by subtraction.

Then Reavis Creek, below Reavis Falls in the eastern Superstition Wilderness, softens the meditation. A smooth pale boulder receives branch shadows. Stone becomes a screen for passing light. The marks are temporary, the surface makes them visible. I like that reversal: permanence serving the fleeting. The rock does not need the shadow, but it receives it completely.

Reavis Creek originates in the eastern Superstition Wilderness. This photograph was captured below Reavis Falls.

At Reavis Falls where water thins into veils over basalt cliff, water teaches stone the art of yielding without surrender. Nearby, boulders lie piled below the falls, carried down Reavis Creek in flood time or broken from the cliff face. They are the aftermath of force, the creek’s heavy language.

Reavis Falls is nestled in mountain ridges of the remote eastern Superstition Wilderness of Arizona. Captured during a four day solo expedition to this site visited by few people.
These are large boulders carried down Reavis Creek and washed over the falls at flood time as well as blocks fractured from the cliff face.

I rested during water gathering in East Boulder Canyon. The pool is narrow, reflective, held among pale stone. Water gathering is one of the oldest errands. In such places, thirst makes geology personal.

Taking a break from morning water gatheringin East Boulder Canyon near where the Peralta Trail where meets Dutchman Trail between Black Top Mesa and Palamino Mountain. Superstition Wilderness, Tonto National Forest, Arizona

The Flatiron, glowing at sunset above Lost Dutchman State Park, expands the timescale: volcanic eruptions between 20.5 and 18 million years ago, dacite lava, rhyolitic tuff, caldera collapse, uplift, differential weathering. The science does not diminish the wonder; it gives wonder a skeleton. The mountain is long-solidified fire, a flame that learned stillness.

The setting sun’s glow on the end point of Upper Siphon Draw trail, The Flatiron. The mountain was formed by a series of volcanic eruptions between 20.5 and 18 million years ago. The west face of the mountain is composed of dacite lava and rhyolitic tuff. The overlying tuff was deposited during an eruption which created a collapse caldera bounded by faults. Dome resurgence reactivated these faults, causing uplift of the caldera floor which juxtaposed the softer tuff and more resistant dacite. Differential weathering caused the outer tuff to erode faster, leaving the dacite cliffs exposed and creating the prominent mountain visible today. The Flatiron, the mesa-like projection above us in this view, is long solidified dacite lava. The word dacite comes from Dacia, a province of the Roman Empire which lay between the Danube River and Carpathian Mountains (now modern Romania and Moldova) where the rock was first described. Lost Dutchman State Park, Apache Junction, Maricopa County, Arizona

These hikers on red slickrock seem almost ceremonial, crossing a surface grooved by time and runoff. They stand small, not diminished but correctly sized. That may be one gift of rocks: they return us to proportion.

And finally Canyon de Chelly again, the risen gibbous moon beside the red southern canyon wall on the trail to White House. Moon, cliff, brush, evening light: all of it held in a copper quiet. After so many stones, the moon is a far away, familiar rock.

The risen gibbon moon against the red rock of the southern canyon wall from the trail to the White House, Canyon de Chelly National Monument.

Rocks I have known have not answered me, exactly. They have done something better. They have outlasted my questions until the questions changed.

Click me to visit Michael Stephen Wills Online Arizona Gallery.

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5 thoughts on “Desert Stones and Ancient Walls: A Meditation on Rocks I Have Known

  1. What a beautiful meditation in both words and images. Your photographs breathe a deep sense of peace, as if the stones remain silent while telling their stories to those willing to truly look and listen. Thank you for yet another remarkable glimpse into your world.

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