Search results for Little Cut

1 -2- 3 4 5
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, Coronado Islands (Islas Coronado)
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  
Hyena carrying a jawbone, Mara Triangle, Kenya, Crocuta crocuta, Mara North Conservancy
Hyena carrying a jawbone, Mara Triangle, Kenya.
Species: Spotted hyena, Crocuta crocuta
Location: Mara North Conservancy, Kenya
Image ID: 39697  
Hyena with Pieces of a Lion Kill, Greater Masai Mara, Kenya, Crocuta crocuta, Mara North Conservancy
Hyena with Pieces of a Lion Kill, Greater Masai Mara, Kenya.
Species: Spotted hyena, Crocuta crocuta
Location: Mara North Conservancy, Kenya
Image ID: 39714  
Northern pintail, male, Bosque Del Apache National Wildlife Refuge, Anas acuta, Bosque del Apache National Wildlife Refuge, Socorro, New Mexico
Northern pintail, male, Bosque Del Apache National Wildlife Refuge.
Species: Northern Pintail, Anas acuta
Location: Bosque del Apache National Wildlife Refuge, Socorro, New Mexico
Image ID: 39940  
West Side Road cuts across the Badwater Basin, Death Valley National Park, California
West Side Road cuts across the Badwater Basin.
Location: Badwater, Death Valley National Park, California
Image ID: 25261  
Sky Rock petroglyphs near Bishop, California. Hidden atop an enormous boulder in the Volcanic Tablelands lies Sky Rock, a set of petroglyphs that face the sky. These superb examples of native American petroglyph artwork are thought to be Paiute in origin, but little is known about them
Sky Rock petroglyphs near Bishop, California. Hidden atop an enormous boulder in the Volcanic Tablelands lies Sky Rock, a set of petroglyphs that face the sky. These superb examples of native American petroglyph artwork are thought to be Paiute in origin, but little is known about them.
Location: Bishop, California
Image ID: 27000  
Sky Rock petroglyphs near Bishop, California. Hidden atop an enormous boulder in the Volcanic Tablelands lies Sky Rock, a set of petroglyphs that face the sky. These superb examples of native American petroglyph artwork are thought to be Paiute in origin, but little is known about them
Sky Rock petroglyphs near Bishop, California. Hidden atop an enormous boulder in the Volcanic Tablelands lies Sky Rock, a set of petroglyphs that face the sky. These superb examples of native American petroglyph artwork are thought to be Paiute in origin, but little is known about them.
Location: Bishop, California
Image ID: 27006  
Nevada Falls, with Liberty Cap (center) and Half Dome (left). Nevada Falls marks where the Merced River plummets almost 600 feet through a joint in the Little Yosemite Valley, shooting out from a sheer granite cliff and then down to a boulder pile far below, Yosemite National Park, California
Nevada Falls, with Liberty Cap (center) and Half Dome (left). Nevada Falls marks where the Merced River plummets almost 600 feet through a joint in the Little Yosemite Valley, shooting out from a sheer granite cliff and then down to a boulder pile far below.
Location: Nevada Falls, Yosemite National Park, California
Image ID: 16115  
Hikers climb the Mist Trail (at right) through Little Yosemite Valley, approaching Vernal Falls. Spring, Yosemite National Park, California
Hikers climb the Mist Trail (at right) through Little Yosemite Valley, approaching Vernal Falls. Spring.
Location: Vernal Falls, Yosemite National Park, California
Image ID: 09200  
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, Yosemite National Park, California
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 Milky Way at Night over Sky Rock. Sky Rock petroglyphs near Bishop, California. Hidden atop an enormous boulder in the Volcanic Tablelands lies Sky Rock, a set of petroglyphs that face the sky. These superb examples of native American petroglyph artwork are thought to be Paiute in origin, but little is known about them
The Milky Way at Night over Sky Rock. Sky Rock petroglyphs near Bishop, California. Hidden atop an enormous boulder in the Volcanic Tablelands lies Sky Rock, a set of petroglyphs that face the sky. These superb examples of native American petroglyph artwork are thought to be Paiute in origin, but little is known about them.
Location: Bishop, California
Image ID: 28798  
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
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  
Panorama of Box Lake, morning, Little Lakes Valley, John Muir Wilderness, Inyo National Forest, Little Lakes Valley, Inyo National Forest
Panorama of Box Lake, morning, Little Lakes Valley, John Muir Wilderness, Inyo National Forest.
Location: Little Lakes Valley, Inyo National Forest, California
Image ID: 31177  
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
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, Devils Postpile National Monument, California
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, Devils Postpile National Monument, California
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, Devils Postpile National Monument, California
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  
Sky Rock petroglyphs and storm clouds over the Eastern Sierran Nevada, near Bishop, California. Hidden atop an enormous boulder in the Volcanic Tablelands lies Sky Rock, a set of petroglyphs that face the sky. These superb examples of native American petroglyph artwork are thought to be Paiute in origin, but little is known about them
Sky Rock petroglyphs and storm clouds over the Eastern Sierran Nevada, near Bishop, California. Hidden atop an enormous boulder in the Volcanic Tablelands lies Sky Rock, a set of petroglyphs that face the sky. These superb examples of native American petroglyph artwork are thought to be Paiute in origin, but little is known about them.
Location: Bishop, California
Image ID: 27001  
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, Yosemite National Park, California
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  
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
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
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
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
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
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
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  
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
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: 36016  
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
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: 36018  
Vermillion Cliffs at Sunrise, Page, Arizona
Vermillion Cliffs at Sunrise, Page, Arizona.
Location: Page, Arizona
Image ID: 36027  
Bear Creek Spire over Marsh Lake at Sunrise, Little Lakes Valley, John Muir Wilderness, Inyo National Forest, Little Lakes Valley, Inyo National Forest
Bear Creek Spire over Marsh Lake at Sunrise, Little Lakes Valley, John Muir Wilderness, Inyo National Forest.
Location: Little Lakes Valley, Inyo National Forest, California
Image ID: 31167  
Bear Creek Spire over Marsh Lake at Sunrise, Little Lakes Valley, John Muir Wilderness, Inyo National Forest, Little Lakes Valley, Inyo National Forest
Bear Creek Spire over Marsh Lake at Sunrise, Little Lakes Valley, John Muir Wilderness, Inyo National Forest.
Location: Little Lakes Valley, Inyo National Forest, California
Image ID: 31168  
1 -2- 3 4 5
Permalink: Little_Cut photos

All photographs copyright © Phillip Colla / Oceanlight.com, all rights reserved worldwide.