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John Day River and Sheep Rock (vertical)

Sheep Rock at John Day Fossil Beds National Monument, shows a resistant cap of Picture Gorge Basalt (Columbia River Basalt Group) on top the Turtle Cove Member of the John Day Formation. (1171-JFR)
Download ImageResistant caprock: basalt over tuff-rich sandstone, Oregon.

Sheep Rock at John Day Fossil Beds National Monument, shows a resistant cap of Picture Gorge Basalt (Columbia River Basalt Group) on top the Turtle Cove Member of the John Day Formation. (1173-JFR)
Download ImagePaleosols: John Day Fm, Oregon.

Oligocene paleosols of John Day Formation in John Day Fossil Beds National Monument, Oregon. (1159_JFR)
Download ImagePaleosols: John Day Fm, Oregon.

Oligocene paleosols of John Day Formation in John Day Fossil Beds National Monument, Oregon. (1165_JFR)
Download ImagePaleosols: John Day Fm, Oregon.

View of Oregon’s Painted Hills at John Day Fossil Beds National Monument. Gently folded paleosols of the Oligocene John Day Formation underlie flat-lying Picture Gorge Basalt, part of the Columbia River Basalt Group.(1150_JFR)
Download ImagePaleosols: John Day Fm, Oregon.

Oligocene paleosols of John Day Formation in John Day Fossil Beds National Monument, Oregon. (1156_JFR)
Download ImagePaleosols: John Day Fm, Oregon.

Oligocene paleosols of John Day Formation in John Day Fossil Beds National Monument. Note open anticline defined by the red beds. (1149_JFR)
Download ImagePaleosols: John Day Fm, Oregon (vertical).

Oligocene paleosols of John Day Formation in John Day Fossil Beds National Monument. (1157_JFR)
Download ImageDebris flow depost, SW Oregon.

Debris flow deposit, likely a submarine canyon fill in the Hunters Cove Formation, SW Oregon. (111207-99)
Download ImagePaleosols: John Day Fm, Oregon. (vertical)

Oligocene paleosols of John Day Formation in John Day Fossil Beds National Monument. Note open anticline defined by the red beds. (1148_JFR)
Download ImageSea stacks and waves, SW Oregon.

Sea stacks and incoming waves, SW Oregon (111207-92).
Download ImageFolded radiolarian chert, Oregon.

Folded radiolarian (ribbon) chert, Oregon. These rocks belong to the Jurassic Otter Point Formation. Photo is about 15 meters across. (111207-7)
Download ImageTilted marine sandstone outcrop, SW Oregon Coast. Sea stack in

Tilted marine sandstone, SW Oregon Coast. This rock is part of the Cretaceous Hunters Cove Formation.
Download ImageTurbidite deposits on Oregon Coast.

Turbidite deposits: alternating beds of sandstone and shale. Cretaceous Hunters Cove Formation, SW Oregon. Rock hammer for scale. (111207-197)
Download ImageSea stacks SW Oregon (Pan).

Sea stacks along SW Oregon coast. Bedrock is mostly accreted Jurassic radiolarian (ribbon) chert. (111207-3)
Download ImageRecumbent fold in radiolarian chert, Oregon

Recumbent fold in Jurassic-age radiolarian (ribbon) chert, Oregon coast. (111206-54)
Download ImageTilted sandstone and surf, Oregon.

Tilted sandstone and incoming surf, Oregon Coast. This rock is part of the Jurassic Otter Point Formation. Sea stack in background.
Download ImageHeadwall of landslide and marine terrace, OR

Headwall of a landslide and uplifted marine terrace. Note small normal fault offsetting the Pleistocene marine gravels, Cape Blanco, Oregon.
Download ImageFolded radiolarian chert, Oregon and sea cave.

Folded radiolarian chert, Oregon and sea cave. These rocks belong to the Jurassic Otter Point Formation. (111206-52)
Download ImageFolded ribbon chert, California

Folded beds of Jurassic-Cretaceous age radiolarian chert, Marin Headlands, California. Main fold is an overturned anticline. (111205-6)
Download Image
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