Pre-Dawn over the Tree of Eons, Utah. The Tree of Eons is a spectacular geologic sight near the San Rafael Swell. Erosion has cut a "tree" through red, blue, purple and white layers of the Chinle formation. The Tree of Eons is a superb example of dendritic erosion and to really appreciate the complex fractal-like details it must be observed from above. Photographed here in the soft, predawn light, it takes on magenta, red and purple hues just before the sun reaches it. Aerial panoramic photograph.
Location: Utah
Image ID: 38027
Teepee rocks at sunrise with the Vermillion Cliffs in the distance.
Location: Page, Arizona
Image ID: 36026
Fisher Towers at sunset, near Moab, Utah. Fisher Towers are a series of towers made of Cutler sandstone capped with Moenkopi sandstone and caked with a stucco of red mud located near Moab, Utah.
Location: Fisher Towers, Moab, Utah
Image ID: 38225
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: 36009
Female California Sea Lion with Severe Fishing Line Entanglement Injury, in the Coronado Islands, Baja California, Mexico. The line is buried in the sea lion's tissue so far that is difficult to see. It is possible this synthetic line will continue to cut into the skin of this sea lion until it succumbs to infection or blood loss. I have never seen any marine mammal rescue teams at the Coronado islands and suspect this poor animal will not live long.
Species: California sea lion, Zalophus californianus
Location: Coronado Islands (Islas Coronado), Baja California, Mexico
Image ID: 39959
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: 36014
Agaltha Peak, also know as El Capitan Peak, rises to over 1500' in height near Kayenta, Arizona and Monument Valley. Agathla Peak is an eroded volcanic plug consisting of volcanic breccia cut by dikes of an unusual igneous rock called minette.
Location: Kayenta, Arizona
Image ID: 28553
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: 36017
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: 36013
Teepee rocks at sunrise with the Vermillion Cliffs in the distance.
Location: Page, Arizona
Image ID: 36025
Aerial Photo of North Coronado Island, Baja California, Mexico, viewed from the southwest. The Keyhole, a spectacular narrow cut and underwater tunnel through the island, is seen at the narrow neck of the island. The San Diego and Tijuana coastline is visible in the distance.
Location: Coronado Islands (Islas Coronado), Baja California, Mexico
Image ID: 35896
Clouds Rest viewed from Olmsted Point. Clouds Rest is one of the most massive -- if not the singlemost massive -- granite monoliths in the world. A vast lobe of Mesozoic-era granodiorite magma cooled to rock and was gradually uplifted to its present altitude of 9926 ft. Later, glaciers cut it into its present shape.
Location: Yosemite National Park, California
Image ID: 09965
The Tree of Eons, Utah. The Tree of Eons is a spectacular geologic sight near the San Rafael Swell in Utah. Here the Tree of Eons is seen under the direct light of midday. Erosion has cut a dendritic "tree" through red, blue, purple and white layers of the Chinle formation. The Tree of Eons is a superb example of dendritic erosion and, to really appreciate its complex fractal-like details, must be observed from above.
Location: Utah
Image ID: 38201
Art Seller along La Rive Gauche, the Left Bank, Paris. La Rive Gauch, the Left Bank, is the southern bank of the river Seine in Paris. Here the river flows roughly westward, cutting the city in two: looking downstream, the southern bank is to the left, and the northern bank (or Rive Droite) is to the right.
Location: La Rive Gauche, Paris, France
Image ID: 28146
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23266
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23267
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23285
Cloud's Rest at sunset, viewed from Olmsted Point. Clouds Rest is one of the most massive -- if not the singlemost massive -- granite monoliths in the world. A vast lobe of Mesozoic-era granodiorite magma cooled to rock and was gradually uplifted to its present altitude of 9926 ft. Later, glaciers cut it into its present shape.
Location: Yosemite National Park, California
Image ID: 25761