Search results for Trochoidal Patterns

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The Tree of Eons, a spectacular dendritic formation in the Bentonite Hills of Utah. Fantastic colorful sedimentary patterns, ancient Bentonite layers are exposed through erosion in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Photographed just before sunrise with soft pre-dawn illumination. Aerial panoramic photograph
The Tree of Eons, a spectacular dendritic formation in the Bentonite Hills of Utah. Fantastic colorful sedimentary patterns, ancient Bentonite layers are exposed through erosion in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Photographed just before sunrise with soft pre-dawn illumination. Aerial panoramic photograph.
Location: Utah
Image ID: 37951  
Panorama dimensions: 11000 x 15000
Surf grass on the rocky reef -- appearing blurred in this time exposure -- is tossed back and forth by powerful ocean waves passing by above. San Clemente Island, Phyllospadix
Surf grass on the rocky reef -- appearing blurred in this time exposure -- is tossed back and forth by powerful ocean waves passing by above. San Clemente Island.
Species: Surfgrass, Phyllospadix
Location: San Clemente Island, California
Image ID: 10237  
Aerial photo of the San Rafael Reef at dawn. A fold in the Earth's crust leads to this inclined section of the San Rafael Reef, at the eastern edge of the San Rafael Swell. Clearly seen are the characteristic triangular flatiron erosion patterns that typical this formation. The colors seen here arise primarily from Navajo and Wingate sandstone
Aerial photo of the San Rafael Reef at dawn. A fold in the Earth's crust leads to this inclined section of the San Rafael Reef, at the eastern edge of the San Rafael Swell. Clearly seen are the characteristic triangular flatiron erosion patterns that typical this formation. The colors seen here arise primarily from Navajo and Wingate sandstone.
Location: Utah
Image ID: 39787  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32327  
Underwater Light, Lake Tahoe, Nevada
Underwater Light, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32328  
Boulders underwater, Lake Tahoe, Nevada
Boulders underwater, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32349  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32358  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32359  
Fantastic colorful sedimentary patterns of Bentonite layers, seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes into layers, now revealed through erosion. Aerial photograph
Fantastic colorful sedimentary patterns of Bentonite layers, seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes into layers, now revealed through erosion. Aerial photograph.
Location: Utah
Image ID: 37947  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 37948  
Clouds light up with blazing colors at sunset, La Jolla, California
Clouds light up with blazing colors at sunset.
Location: La Jolla, California
Image ID: 04819  
Aerial photo of the San Rafael Reef at dawn. A fold in the Earth's crust leads to this inclined section of the San Rafael Reef, at the eastern edge of the San Rafael Swell. Clearly seen are the characteristic triangular flatiron erosion patterns that typical this formation. The colors seen here arise primarily from Navajo and Wingate sandstone
Aerial photo of the San Rafael Reef at dawn. A fold in the Earth's crust leads to this inclined section of the San Rafael Reef, at the eastern edge of the San Rafael Swell. Clearly seen are the characteristic triangular flatiron erosion patterns that typical this formation. The colors seen here arise primarily from Navajo and Wingate sandstone.
Location: Utah
Image ID: 39784  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32346  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32347  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32348  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32350  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32356  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32361  
Gray whales at sunset, Laguna San Ignacio, Eschrichtius robustus, San Ignacio Lagoon
Gray whales at sunset, Laguna San Ignacio.
Species: Gray whale, Eschrichtius robustus
Location: San Ignacio Lagoon, Baja California, Mexico
Image ID: 03387  
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Aerial photograph
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Aerial photograph.
Location: Utah
Image ID: 38029  
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands, part of the Chinle Formation formed during the Upper Triassic Period. Aerial photograph
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands, part of the Chinle Formation formed during the Upper Triassic Period. Aerial photograph.
Location: Utah
Image ID: 38177  
Beautiful underwater sunburst, glittering light through the ocean surface, Sea of Cortez, Baja California, Mexico
Beautiful underwater sunburst, glittering light through the ocean surface, Sea of Cortez, Baja California, Mexico.
Location: Sea of Cortez, Baja California, Mexico
Image ID: 27562  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32357  
Underwater Light and Sand, Lake Tahoe, Nevada
Underwater Light and Sand, Lake Tahoe, Nevada.
Location: Lake Tahoe, Nevada
Image ID: 32360  
Rissos dolphin. Note distinguishing and highly variable skin and dorsal fin patterns, characteristic of this species. White scarring, likely caused by other Risso dolphins teeth, accumulates during the dolphins life so that adult Rissos dolphins are usually almost entirely white, Grampus griseus, San Diego, California
Rissos dolphin. Note distinguishing and highly variable skin and dorsal fin patterns, characteristic of this species. White scarring, likely caused by other Risso dolphins teeth, accumulates during the dolphins life so that adult Rissos dolphins are usually almost entirely white.
Species: Risso's dolphin, Grampus griseus
Location: San Diego, California
Image ID: 12792  
Rissos dolphin. Note distinguishing and highly variable skin and dorsal fin patterns, characteristic of this species. White scarring, likely caused by other Risso dolphins teeth, accumulates during the dolphins life so that adult Rissos dolphins are usually almost entirely white, Grampus griseus, San Diego, California
Rissos dolphin. Note distinguishing and highly variable skin and dorsal fin patterns, characteristic of this species. White scarring, likely caused by other Risso dolphins teeth, accumulates during the dolphins life so that adult Rissos dolphins are usually almost entirely white.
Species: Risso's dolphin, Grampus griseus
Location: San Diego, California
Image ID: 12799  
Rissos dolphin surfacing with eye showing. Note distinguishing and highly variable skin and dorsal fin patterns, characteristic of this species. White scarring, likely caused by other Risso dolphins teeth, accumulates during the dolphins life so that adult Rissos dolphins are almost entirely white. San Diego, Grampus griseus
Rissos dolphin surfacing with eye showing. Note distinguishing and highly variable skin and dorsal fin patterns, characteristic of this species. White scarring, likely caused by other Risso dolphins teeth, accumulates during the dolphins life so that adult Rissos dolphins are almost entirely white. San Diego.
Species: Risso's dolphin, Grampus griseus
Location: San Diego, California
Image ID: 02314  
The Mandelbrot Fractal. Fractals are complex geometric shapes that exhibit repeating patterns typified by self-similarity, or the tendency for the details of a shape to appear similar to the shape itself. Often these shapes resemble patterns occurring naturally in the physical world, such as spiraling leaves, seemingly random coastlines, erosion and liquid waves. Fractals are generated through surprisingly simple underlying mathematical expressions, producing subtle and surprising patterns. The basic iterative expression for the Mandelbrot set is z = z-squared + c, operating in the complex (real, imaginary) number set, Mandelbrot set
The Mandelbrot Fractal. Fractals are complex geometric shapes that exhibit repeating patterns typified by self-similarity, or the tendency for the details of a shape to appear similar to the shape itself. Often these shapes resemble patterns occurring naturally in the physical world, such as spiraling leaves, seemingly random coastlines, erosion and liquid waves. Fractals are generated through surprisingly simple underlying mathematical expressions, producing subtle and surprising patterns. The basic iterative expression for the Mandelbrot set is z = z-squared + c, operating in the complex (real, imaginary) number set.
Species: Mandelbrot fractal, Mandelbrot set
Image ID: 10368  
The Mandelbrot Fractal. Fractals are complex geometric shapes that exhibit repeating patterns typified by self-similarity, or the tendency for the details of a shape to appear similar to the shape itself. Often these shapes resemble patterns occurring naturally in the physical world, such as spiraling leaves, seemingly random coastlines, erosion and liquid waves. Fractals are generated through surprisingly simple underlying mathematical expressions, producing subtle and surprising patterns. The basic iterative expression for the Mandelbrot set is z = z-squared + c, operating in the complex (real, imaginary) number set, Mandelbrot set
The Mandelbrot Fractal. Fractals are complex geometric shapes that exhibit repeating patterns typified by self-similarity, or the tendency for the details of a shape to appear similar to the shape itself. Often these shapes resemble patterns occurring naturally in the physical world, such as spiraling leaves, seemingly random coastlines, erosion and liquid waves. Fractals are generated through surprisingly simple underlying mathematical expressions, producing subtle and surprising patterns. The basic iterative expression for the Mandelbrot set is z = z-squared + c, operating in the complex (real, imaginary) number set.
Species: Mandelbrot fractal, Mandelbrot set
Image ID: 10369  
Detail within the Mandelbrot set fractal. This detail is found by zooming in on the overall Mandelbrot set image, finding edges and buds with interesting features. Fractals are complex geometric shapes that exhibit repeating patterns typified by self-similarity, or the tendency for the details of a shape to appear similar to the shape itself. Often these shapes resemble patterns occurring naturally in the physical world, such as spiraling leaves, seemingly random coastlines, erosion and liquid waves. Fractals are generated through surprisingly simple underlying mathematical expressions, producing subtle and surprising patterns. The basic iterative expression for the Mandelbrot set is z = z-squared + c, operating in the complex (real, imaginary) number set, Mandelbrot set
Detail within the Mandelbrot set fractal. This detail is found by zooming in on the overall Mandelbrot set image, finding edges and buds with interesting features. Fractals are complex geometric shapes that exhibit repeating patterns typified by self-similarity, or the tendency for the details of a shape to appear similar to the shape itself. Often these shapes resemble patterns occurring naturally in the physical world, such as spiraling leaves, seemingly random coastlines, erosion and liquid waves. Fractals are generated through surprisingly simple underlying mathematical expressions, producing subtle and surprising patterns. The basic iterative expression for the Mandelbrot set is z = z-squared + c, operating in the complex (real, imaginary) number set.
Species: Mandelbrot fractal, Mandelbrot set
Image ID: 10375  
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