AA-2026-09DAAB
On the image
Someone in the early postwar era travelled into the high desert Southwest to photograph a landscape that looks like it was organised by a sculptor with too much time and a taste for the surreal. The pale hoodoos—those columnar rock formations that stand like half-finished statues—rise in a neat row along what appears to be a seasonal stream bed, the kind of geological accident that seems designed to make geologists talk for hours and civilians nod politely. The water pooling in the foreground carries the reddish tint of mineral-rich runoff, evidence that the land here is not inert but actively dissolving and rearranging itself, a process the photographer's era found endlessly worthy of documentation. The composition suggests someone who knew the light would be good and the formations photogenic—this is not casual tourism but the kind of deliberate expedition America's mid-century landscape photographers conducted with a camera mounted in a vehicle and a plan folded on the passenger seat.
What makes the image historically specific is not just the geological formations but the evident assumption that wilderness worth recording was wilderness where you could still drive to it, photograph it with available light, and use colour film to prove the colours were real. The hoodoos have the slightly uncanny perfection that American photographers of that decade seemed to find everywhere—the sense that nature, given half a chance and good light, resembled nothing so much as landscape painting, and that capturing it on film was a way of confirming the continent's inheritance of natural splendour.
The historian's note
The high desert Southwest of the United States contains numerous hoodoo fields, columnar rock formations created by differential erosion of layered sedimentary deposits. The most prominent and accessible examples occur in Utah, Arizona, and parts of New Mexico, with Goblin Valley State Park in Utah and the Bisti/De-Na-Zin Wilderness in New Mexico amongst the most visually distinctive. This scene, shot in colour transparency film (likely Kodachrome or Ektachrome stock), reflects the mid-twentieth-century surge in colour landscape photography enabled by improved colour film availability and the expansion of automotive tourism through the Southwest. The reddish water and mineral coloration visible in the stream bed are consistent with alkali or iron-oxide-bearing waters common to arid basin drainage systems. The photographic documentation of such formations became increasingly common during the 1940s–1950s as highway infrastructure improved and colour photography made natural landscape colour verifiable to the general public, transforming geological formations from subjects for geological survey documentation into elements of American scenic tourism.
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Hoodoo Formation with Stream, High Desert Southwest, circa 1940s–1950s. 1940–1955. Archive & Atlas, Historical Image Library, AA-2026-09DAAB. https://thearchive.archiveandatlas.com/library/hoodoo-formation-with-stream-high-desert-southwest-circa-1940s-1950s.
@misc{aaAA202609DAAB,
title = {Hoodoo Formation with Stream, High Desert Southwest, circa 1940s–1950s},
year = {1940–1955},
howpublished = {Archive \& Atlas, Historical Image Library},
note = {Accession AA-2026-09DAAB},
url = {https://thearchive.archiveandatlas.com/library/hoodoo-formation-with-stream-high-desert-southwest-circa-1940s-1950s}
}TY - ART TI - Hoodoo Formation with Stream, High Desert Southwest, circa 1940s–1950s PY - 1940–1955 PB - Archive & Atlas, Historical Image Library AN - AA-2026-09DAAB UR - https://thearchive.archiveandatlas.com/library/hoodoo-formation-with-stream-high-desert-southwest-circa-1940s-1950s ER -
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