Search results for Pile Seaperch

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Nevada Falls marks where the Merced River plummets almost 600 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 marks where the Merced River plummets almost 600 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: 16114  
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  
Shiner perch, Cymatogaster aggregata
Shiner perch.
Species: Shiner perch, Cymatogaster aggregata
Image ID: 08918  
Spotfin surfperch, Hyperprosopon anale
Spotfin surfperch.
Species: Spotfin surfperch, Hyperprosopon anale
Image ID: 08997  
Rainbow surfperch, Hypsurus caryi
Rainbow surfperch.
Species: Rainbow surfperch, Hypsurus caryi
Image ID: 09006  
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  
Pelagic red tuna crabs, washed ashore to form dense piles on the beach, Pleuroncodes planipes, Ocean Beach, California
Pelagic red tuna crabs, washed ashore to form dense piles on the beach.
Species: Pelagic red crab, Pleuroncodes planipes
Location: Ocean Beach, California
Image ID: 30982  
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: 23281  
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: 23282  
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: 23283  
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: 23284  
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: 23286  
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: 23287  
Pelagic red tuna crabs, washed ashore to form dense piles on the beach, Pleuroncodes planipes, Ocean Beach, California
Pelagic red tuna crabs, washed ashore to form dense piles on the beach.
Species: Pelagic red crab, Pleuroncodes planipes
Location: Ocean Beach, California
Image ID: 06068  
Pelagic red tuna crabs, washed ashore to form dense piles on the beach, Pleuroncodes planipes, Ocean Beach, California
Pelagic red tuna crabs, washed ashore to form dense piles on the beach.
Species: Pelagic red crab, Pleuroncodes planipes
Location: Ocean Beach, California
Image ID: 06077  
Pelagic red tuna crabs, washed ashore to form dense piles on the beach, Pleuroncodes planipes, Ocean Beach, California
Pelagic red tuna crabs, washed ashore to form dense piles on the beach.
Species: Pelagic red crab, Pleuroncodes planipes
Location: Ocean Beach, California
Image ID: 30980  
Pelagic red tuna crabs, washed ashore to form dense piles on the beach, Pleuroncodes planipes, Ocean Beach, California
Pelagic red tuna crabs, washed ashore to form dense piles on the beach.
Species: Pelagic red crab, Pleuroncodes planipes
Location: Ocean Beach, California
Image ID: 30981  
Pelagic red tuna crabs, washed ashore to form dense piles on the beach, Pleuroncodes planipes, Ocean Beach, California
Pelagic red tuna crabs, washed ashore to form dense piles on the beach.
Species: Pelagic red crab, Pleuroncodes planipes
Location: Ocean Beach, California
Image ID: 30983  
Lyretail fairy basslet, male, Pseudanthias squamipinnis
Lyretail fairy basslet, male.
Species: Jewel fairy basslet, Pseudanthias squamipinnis
Image ID: 12866  
Lyretail fairy basslet, female, Pseudanthias squamipinnis
Lyretail fairy basslet, female.
Species: Jewel fairy basslet, Pseudanthias squamipinnis
Image ID: 11795  
Lyretail fairy basslet, female, Pseudanthias squamipinnis
Lyretail fairy basslet, female.
Species: Jewel fairy basslet, Pseudanthias squamipinnis
Image ID: 11796  
Lyretail fairy basslet, female, Pseudanthias squamipinnis
Lyretail fairy basslet, female.
Species: Jewel fairy basslet, Pseudanthias squamipinnis
Image ID: 11797  
Lyretail fairy basslet, female, Pseudanthias squamipinnis
Lyretail fairy basslet, female.
Species: Jewel fairy basslet, Pseudanthias squamipinnis
Image ID: 11798  
Lyretail fairy basslet, female, Pseudanthias squamipinnis
Lyretail fairy basslet, female.
Species: Jewel fairy basslet, Pseudanthias squamipinnis
Image ID: 11799  
Trans-Pecos copperhead snake. The Trans-Pecos copperhead is a pit viper found in the Chihuahuan desert of west Texas. It is found near streams and rivers, wooded areas, logs and woodpiles, Agkistrodon contortrix pictigaster
Trans-Pecos copperhead snake. The Trans-Pecos copperhead is a pit viper found in the Chihuahuan desert of west Texas. It is found near streams and rivers, wooded areas, logs and woodpiles.
Species: Trans-pecos copperhead snake, Agkistrodon contortrix pictigaster
Image ID: 12578  
Trans-Pecos copperhead snake. The Trans-Pecos copperhead is a pit viper found in the Chihuahuan desert of west Texas. It is found near streams and rivers, wooded areas, logs and woodpiles, Agkistrodon contortrix pictigaster
Trans-Pecos copperhead snake. The Trans-Pecos copperhead is a pit viper found in the Chihuahuan desert of west Texas. It is found near streams and rivers, wooded areas, logs and woodpiles.
Species: Trans-pecos copperhead snake, Agkistrodon contortrix pictigaster
Image ID: 12579  
Trans-Pecos copperhead snake. The Trans-Pecos copperhead is a pit viper found in the Chihuahuan desert of west Texas. It is found near streams and rivers, wooded areas, logs and woodpiles, Agkistrodon contortrix pictigaster
Trans-Pecos copperhead snake. The Trans-Pecos copperhead is a pit viper found in the Chihuahuan desert of west Texas. It is found near streams and rivers, wooded areas, logs and woodpiles.
Species: Trans-pecos copperhead snake, Agkistrodon contortrix pictigaster
Image ID: 12580  
Trans-Pecos copperhead snake. The Trans-Pecos copperhead is a pit viper found in the Chihuahuan desert of west Texas. It is found near streams and rivers, wooded areas, logs and woodpiles, Agkistrodon contortrix pictigaster
Trans-Pecos copperhead snake. The Trans-Pecos copperhead is a pit viper found in the Chihuahuan desert of west Texas. It is found near streams and rivers, wooded areas, logs and woodpiles.
Species: Trans-pecos copperhead snake, Agkistrodon contortrix pictigaster
Image ID: 12581  
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