Search results for Erosion

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Fractal design. 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
Fractal design. 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: 18732  
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: 18737  
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: 18739  
Torrey Pines State Reserve at Night, stars and clouds fill the night sky with the lights of La Jolla visible in the distance, San Diego, California
Torrey Pines State Reserve at Night, stars and clouds fill the night sky with the lights of La Jolla visible in the distance.
Location: Torrey Pines State Reserve, San Diego, California
Image ID: 28405  
Panorama dimensions: 6607 x 12076
The Fire Wave at night, lit by the light of the moon, Valley of Fire State Park
The Fire Wave at night, lit by the light of the moon.
Location: Valley of Fire State Park, Nevada
Image ID: 28430  
Panorama dimensions: 7280 x 7255
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
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  
Falling bluffs and reinforcements, buttressing, Encinitas and Leucadia. These bluffs are coming down, its only a matter of time, but residents spend to prop up the bluffs and keep their homes from falling into the ocean
Falling bluffs and reinforcements, buttressing, Encinitas and Leucadia. These bluffs are coming down, its only a matter of time, but residents spend to prop up the bluffs and keep their homes from falling into the ocean.
Location: Encinitas, California
Image ID: 37971  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38017  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38018  
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands, part 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, part 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: 38019  
Sunrise over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The San Rafael Swell is in the distance
Sunrise over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The San Rafael Swell is in the distance.
Location: Utah
Image ID: 38026  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38032  
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. Factory Butte is in the distance
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. Factory Butte is in the distance.
Location: Utah
Image ID: 38064  
Dawn breaks over the Bentonite Hills in the Utah Badlands. Striations in soil reveal layers of the Morrison Formation, formed in swamps and lakes in the Jurassic era. Aerial panoramic photograph
Dawn breaks over the Bentonite Hills in the Utah Badlands. Striations in soil reveal layers of the Morrison Formation, formed in swamps and lakes in the Jurassic era. Aerial panoramic photograph.
Location: Utah
Image ID: 38065  
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
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  
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: 38067  
Lower Blue Hills Badlands, sunrise, Utah
Lower Blue Hills Badlands, sunrise, Utah.
Location: Utah
Image ID: 38074  
Falling bluffs and reinforcements, buttressing, Encinitas and Leucadia. These bluffs are coming down, its only a matter of time, but residents spend to prop up the bluffs and keep their homes from falling into the ocean
Falling bluffs and reinforcements, buttressing, Encinitas and Leucadia. These bluffs are coming down, its only a matter of time, but residents spend to prop up the bluffs and keep their homes from falling into the ocean.
Location: Encinitas, California
Image ID: 38140  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38170  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38173  
Mars Desert Research Station, set amid beautiful Mars-like "Bentonite Hills", near Hanksville, Utah
Mars Desert Research Station, set amid beautiful Mars-like "Bentonite Hills", near Hanksville, Utah.
Location: Utah
Image ID: 38179  
Lower Blue Hills Badlands, sunrise, Utah
Lower Blue Hills Badlands, sunrise, Utah.
Location: Utah
Image ID: 38180  
White Cap Mesa overlooking Goblin Valley State Park, Utah
White Cap Mesa overlooking Goblin Valley State Park, Utah.
Location: Goblin Valley State Park, Utah
Image ID: 38182  
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
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  
Sunrise over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. Factory Butte is in the distance
Sunrise over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. Factory Butte is in the distance.
Location: Utah
Image ID: 38200  
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  
Lower Blue Hills Badlands, sunrise, Utah
Lower Blue Hills Badlands, sunrise, Utah.
Location: Utah
Image ID: 38202  
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The Henry Mountains are in the distance
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The Henry Mountains are in the distance.
Location: Utah
Image ID: 38210  
Aerial View of the San Rafael Reef, Utah. This is a canyon-like section of the San Rafael Reef, photographed at sunrise. The "reef proper" is on the right, with its characteristic triangular flatiron erosion. The canyon in the center is a fold in the Earth's crust affiliated with the boundary of the San Rafael Swell. The colors seen here arise primarily from Navajo and Wingate sandstone
Aerial View of the San Rafael Reef, Utah. This is a canyon-like section of the San Rafael Reef, photographed at sunrise. The "reef proper" is on the right, with its characteristic triangular flatiron erosion. The canyon in the center is a fold in the Earth's crust affiliated with the boundary of the San Rafael Swell. The colors seen here arise primarily from Navajo and Wingate sandstone.
Location: Utah
Image ID: 39496  
Owl Canyon, a beautiful slot canyon that is part of the larger Antelope Canyon system. Page, Arizona, Navajo Tribal Lands
Owl Canyon, a beautiful slot canyon that is part of the larger Antelope Canyon system. Page, Arizona.
Location: Navajo Tribal Lands, Page, Arizona
Image ID: 36032  
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