Pacific Northwest High Desert, Oregon
Cinder Cone in High Desert Forest, Pacific Northwest, 1950s — Archive & Atlas
AA-2026-2313E6
Pacific Northwest High Desert, Oregon
AA-2026-2313E6
On the image
A young cinder cone rises from a sagebrush and lodgepole pine forest, the kind of volcanic geography that covers vast stretches of Oregon and central Oregon high country where the Cascade Range gives way to semi-arid plateau. The cone itself is barren except for a sparse scattering of small conifers on its slopes, its dark volcanic stone still plainly visible beneath decades of weathering and sparse vegetation. Someone in the 1950s drove or hiked to a vantage point to photograph this landscape, probably because the geological clarity interested them, or because they were documenting the region for a government survey or educational purpose.
The surrounding forest shows the aftermath of the region's logging history and fire cycles—a mix of dense younger growth and scattered mature trees, the patchwork mosaic of a landscape humans had been actively managing for half a century. The clear sky and the color saturation suggest summer, when such high-country roads would be reliably passable. This is the kind of record that made sense to someone at the time: evidence of the land's underlying structure, the bones of the West still visible if you knew where to look.
The historian's note
Cinder cones are small volcanic features formed by accumulated cinder and ash from relatively recent eruptions—in the case of Pacific Northwest examples, typically from the Holocene epoch. The Newberry Volcanic Field in central Oregon contains dozens of such cones, as do areas surrounding the Cascade Range. The lodgepole pine and sagebrush environment visible here is characteristic of the Oregon high desert and the transition zone between the Cascades and the Basin and Range provinces, elevations typically between 4,000 and 6,500 feet.
Photography of geological features became routine for the U.S. Geological Survey and the U.S. Bureau of Land Management during the 1950s as part of systematic resource surveys and educational outreach. The color transparency process and the composition suggest official or semi-official documentation, though attribution cannot be determined from the image alone. Such photographs served both scientific and public purposes: mapping volcanic history and promoting public understanding of the region's geology.
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Visually related — by likeness
Cinder Cone in High Desert Forest, Pacific Northwest, 1950s. 1950–1959. Archive & Atlas, Historical Image Library, AA-2026-2313E6. https://thearchive.archiveandatlas.com/library/cinder-cone-in-high-desert-forest-pacific-northwest-1950s.
@misc{aaAA20262313E6,
title = {Cinder Cone in High Desert Forest, Pacific Northwest, 1950s},
year = {1950–1959},
howpublished = {Archive \& Atlas, Historical Image Library},
note = {Accession AA-2026-2313E6},
url = {https://thearchive.archiveandatlas.com/library/cinder-cone-in-high-desert-forest-pacific-northwest-1950s}
}TY - ART TI - Cinder Cone in High Desert Forest, Pacific Northwest, 1950s PY - 1950–1959 PB - Archive & Atlas, Historical Image Library AN - AA-2026-2313E6 UR - https://thearchive.archiveandatlas.com/library/cinder-cone-in-high-desert-forest-pacific-northwest-1950s ER -
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