Hoodoos in Goblin Valley State Park, aerial panorama. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago. Aerial panoramic photograph.
Location: Goblin Valley State Park, Utah
Image ID: 37957
Hoodoos in Goblin Valley State Park. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago.
Location: Goblin Valley State Park, Utah
Image ID: 38066
Hoodoos in Goblin Valley State Park. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago.
Location: Goblin Valley State Park, Utah
Image ID: 38183
Remarkable Rocks Panoramic Photo. It took 500 million years for rain, wind and surf to erode these rocks into their current form. They are a signature part of Flinders Chase National Park on Kangaroo Island, South Australia.
Location: Flinders Chase National Park, Kangaroo Island, South Australia
Image ID: 39224
Panorama dimensions: 200 x 674
Waves wash over sandstone reef, clouds and sky.
Location: La Jolla, California
Image ID: 26335
Waves wash over sandstone reef, clouds and sky.
Location: La Jolla, California
Image ID: 26336
Wind turbines, rise above the flat floor of the San Gorgonio Pass near Palm Springs, with snow covered Mount San Jacinto in the background, provide electricity to Palm Springs and the Coachella Valley.
Location: San Gorgonio Pass, Palm Springs, California
Image ID: 22209
Ocotillo Express Wind Energy Projects, moving turbines lit by the rising sun,.
Location: Ocotillo, California
Image ID: 30248
Los Angeles Convention Center, south hall, interior design exhibiting exposed space frame steel beams and glass enclosure.
Image ID: 29146
Los Angeles Convention Center, south hall, interior design exhibiting exposed space frame steel beams and glass enclosure.
Image ID: 29151
Sunrise on the Racetrack Playa. The sliding rocks, or sailing stones, move across the mud flats of the Racetrack Playa, leaving trails behind in the mud. The explanation for their movement is not known with certainty, but many believe wind pushes the rocks over wet and perhaps icy mud in winter.
Location: Racetrack Playa, Death Valley National Park, California
Image ID: 27701
A sliding rock of the Racetrack Playa. The sliding rocks, or sailing stones, move across the mud flats of the Racetrack Playa, leaving trails behind in the mud. The explanation for their movement is not known with certainty, but many believe wind pushes the rocks over wet and perhaps icy mud in winter.
Location: Racetrack Playa, Death Valley National Park, California
Image ID: 25243
Waves wash over sandstone reef, clouds and sky.
Location: La Jolla, California
Image ID: 26345
Racetrack sailing stone and star trails. A sliding rock of the Racetrack Playa. The sliding rocks, or sailing stones, move across the mud flats of the Racetrack Playa, leaving trails behind in the mud. The explanation for their movement is not known with certainty, but many believe wind pushes the rocks over wet and perhaps icy mud in winter.
Location: Racetrack Playa, Death Valley National Park, California
Image ID: 27668
The Wave in the North Coyote Buttes, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 28609
The Second Wave at sunset. The Second Wave, a curiously-shaped sandstone swirl, takes on rich warm tones and dramatic shadowed textures at sunset. Set in the North Coyote Buttes of Arizona and Utah, the Second Wave is characterized by striations revealing layers of sedimentary deposits, a visible historical record depicting eons of submarine geology.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 28615
The Wave at Night, under a clear night sky full of stars. The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 28624
Wind turbines, rise above the flat floor of the San Gorgonio Pass near Palm Springs, with snow covered Mount San Jacinto in the background, provide electricity to Palm Springs and the Coachella Valley.
Location: San Gorgonio Pass, Palm Springs, California
Image ID: 22205
Barker Dam, Joshua Tree National Park. Barker Dam, also known as the Big Horn Dam, is a water-storage facility located in Joshua Tree National Park in California. The dam was constructed by early cattlemen and ranchers. It is situated between Queen Valley and the Wonderland of Rocks near the Wall Street Mill and is a gathering place for desert wildlife.
Location: Joshua Tree National Park, California
Image ID: 26731
Panorama dimensions: 5645 x 10823
Wind turbines provide electricity to Palm Springs and the Coachella Valley. San Gorgonio pass, San Bernardino mountains.
Location: San Gorgonio Pass, Palm Springs, California
Image ID: 06856
Eglise de Knokke, 1894, Camille Pissarro, Musee d'Orsay, Paris.
Location: Musee dOrsay, Paris, France
Image ID: 35614
Canyon X, a spectacular slot canyon near Page, Arizona. Slot canyons are formed when water and wind erode a cut through a (usually sandstone) mesa, producing a very narrow passage that may be as slim as a few feet and a hundred feet or more in height.
Location: Page, Arizona
Image ID: 36007
Canyon X, a spectacular slot canyon near Page, Arizona. Slot canyons are formed when water and wind erode a cut through a (usually sandstone) mesa, producing a very narrow passage that may be as slim as a few feet and a hundred feet or more in height.
Location: Page, Arizona
Image ID: 36008
Canyon X, a spectacular slot canyon near Page, Arizona. Slot canyons are formed when water and wind erode a cut through a (usually sandstone) mesa, producing a very narrow passage that may be as slim as a few feet and a hundred feet or more in height.
Location: Page, Arizona
Image ID: 36010
Canyon X, a spectacular slot canyon near Page, Arizona. Slot canyons are formed when water and wind erode a cut through a (usually sandstone) mesa, producing a very narrow passage that may be as slim as a few feet and a hundred feet or more in height.
Location: Page, Arizona
Image ID: 36011
Canyon X, a spectacular slot canyon near Page, Arizona. Slot canyons are formed when water and wind erode a cut through a (usually sandstone) mesa, producing a very narrow passage that may be as slim as a few feet and a hundred feet or more in height.
Location: Page, Arizona
Image ID: 36012
Canyon X, a spectacular slot canyon near Page, Arizona. Slot canyons are formed when water and wind erode a cut through a (usually sandstone) mesa, producing a very narrow passage that may be as slim as a few feet and a hundred feet or more in height.
Location: Page, Arizona
Image ID: 36015