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Stream Cobbles Oregon

Ultramafic cobbles in Rough and Ready Creek, drained from the Smith River Terrane of the Western Klamath Belt, Cave Junction, Oregon. (ID: 140119-12t2)
Download ImageFountain Formation, Colorado. (vertical

Pennsylvanian-Permian sandstone of Fountain Formation, Colorado (131024-6)
Download ImageHogbacks of Fountain Formation, Colorado.

Strike valley and hogback eroded into Pennsylvanian-Permian sandstone and conglomerate of Fountain Formation, Colorado (131024-19)
Download ImageFountain Formation, Colorado.

Pennsylvanian-Permian sandstone of Fountain Formation, Colorado (131024-7)
Download ImageMazama Ash overlying basalt, Oregon

Ash from the cataclysmic eruption of Mt. Mazama 7700 years ago (which formed Crater Lake) overlies basalt. (130922-108)
Download ImageLake Abert, Oregon –a pluvial lake

Pluvial lakes are those left from the Pleistocene epoch when the climate was wetter. They are now mostly playa lakes. (130922-16)
Download ImageQuarried Cinder Cone, Oregon

LIttle Nash Crater, quarried for its cinders. (130901-9)
Download ImageBelknap Shield Volcano, Oregon

2000 year old Yapoah basalt lava flow and Belknap shield volcano, near McKenzie Pass, Oregon. (130825-6)
Download ImageGabbro outcrop, Mary’s Peak, Oregon (vertical)

Gabbro outcrop at top of Mary’s Peak, highest peak in Oregon’s Coast Range. (130914-12)
Download ImageGabbro on Mary’s Peak, Orgon

Gabbro outcrop at top of Mary’s Peak, highest peak in Oregon’s Coast Range. (130914-14)
Download ImageGlacial till and volcanic ash, Oregon

Glacial till and overlying volcanic ash erupted from Mount Mazama, 7700 years ago, Oregon. (130901-17)
Download ImageSea Arch, Oregon

A small sea arch produced by wave erosion along the Oregon Coast. (130428-18)
Download ImageUinta Mountains, Utah

Aerial view of glacial valleys in the Uinta Mountains and Proterozoic Uinta Mountain Group, Utah. (130102-56)
Download ImageSea Arch, Oregon

A small sea arch produced by wave erosion along the Oregon Coast. Devil’s Punchbowl. (130428-33)
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