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Paleosols of John Day Formation, Oregon

Oligocene paleosols in John Day Fossil Beds National Monument. (110805-141)
Download ImagePaleosols: John Day Fm, Oregon. (vertical)

Oligocene paleosols in John Day Fossil Beds National Monument. (110805-111)
Download ImageBelknap Shield Volcano, Oregon.

Belknap Shield Volcano is a basaltic volcano of Oregon’s High Cascades.(110805-8)
Download ImagePaleosols of John Day Formation, Oregon.

Oligocene paleosols in John Day Fossil Beds National Monument. (110805-107)
Download ImageCinder cone: Collier Cone, Oregon

Collier Cone is a basaltic cinder cone of the Oregon Cascades. (110730-87)
Download ImageSand blowing off dune, Oregon.

Sand blowing off dune along Oregon’s coast. (110731-21)
Download ImageNorth Sister volcano, Oregon

North Sister, an eroded stratovolcano, Oregon. Middle Sister in background. (110730-70)
Download ImageVolcano and Lava Flow, Oregon (vertical)

North Sister stratovolcano and Lava Flow, Oregon (110730-118)
Download ImageStratovolcanoes and lava flow, Oregon

North and Middle Sister stratovolcanoes and Lava Flow, Oregon (110730-124)
Download ImageCascade Volcanoes, Oregon (Pan)

View from Collier Cone. From left (south) to right, the volcanoes are Belknap Shield Volcano, Mount Washington, Three-Fingered Jack, Mount Jefferson (large snowy one), Mt. Hood. (110730-54)
Download ImageGranitic bedrock and glacial cirque, Colorado.

Upper reaches of Glacier Gorge, a U-shaped valley in Rocky Mountain National Park. Longs Peak forms the high peak in the center. (110716-26)
Download ImageGlacial cirque, Colorado

Upper reaches of Glacier Gorge, a U-shaped valley and cirque in Rocky Mountain National Park. From left to right, the peaks on the skyline are Longs Peak, Pagoda Mtn., and Chiefs Head. Spearhead forms the end of the arete coming off Chiefs Head. (110716-39)
Download ImageLongs Peak, Colorado (vertical)

Longs Peak forms the side of Glacier Gorge, a U-shaped valley in Rocky Mountain National Park, Colorado. The dark stripe is a large inclusion of metamorphic rock in the Proterozoic granitic rock. (110716-72)
Download ImageGlacial arete, Colorado

Glacial aretes are the narrow ridges that separate glacial cirques. This one is formed of Proterozoic granitic rock in Rocky Mountain National Park, Colorado. (110716-58)
Download ImageFull moon over moraine, Colorado

Full moon over high forested moraine, Rocky Mountain National Park, Colorado. (110716-6)
Download ImageMoon over Front Fange, Colorado

Full moon over the Front Range of Rocky Mountain National Park, Colorado. Each peak is separated by a U-shaped, glacial valley. (110716-2).
Download ImageGlacial arete, Colorado

The Spearhead is a peak at the end of a glacial arete that ends in a headwall in Rocky Mountain National Park, Colorado.
Download ImageGlacial erosional features, Colorado

Glacial headwall, cirque, and U-shaped Valley on Longs Peak, in Rocky Mountain National Park, Colorado. A lateral moraine (Mills Moraine) follows the right side of the valley. Mt. Meeker on the left and Mt. Lady Washington are on the right. Longs Peak consists primarily of Proterozoic granitic rock. (110715-45)
Download Image
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