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Published byMaude King Modified over 9 years ago
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Arid region geomorphology What causes the erosion and deposition? - Wind, Water, and Gravity Arid region geomorphology What causes the erosion and deposition? - Wind, Water, and Gravity
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Badlands topography with terraces
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Types of streams in Arid and semi-Arid locales Exotic streams - begin in areas that are not arid and flow into the desert. Ex. Nile River, Colorado River, Okavango River Local streams (Arroyos) - begin in the arid region, and often end there as well. There are many streams of this type… Types of streams in Arid and semi-Arid locales Exotic streams - begin in areas that are not arid and flow into the desert. Ex. Nile River, Colorado River, Okavango River Local streams (Arroyos) - begin in the arid region, and often end there as well. There are many streams of this type…
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Nile River- An exotic stream Nile River- An exotic stream
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Colorado River- Dammed
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Alluvial fans in Death Valley Graben
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Playa lake, Owens Valley, CA
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Sand Dunes in Colorado Great Sand Dunes National Monument
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Star Dune in Mexico
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Linear Dunes With an exotic stream
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Transverse dunes in Namibia
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Erosional landforms vs. Depositional landforms Erosional forms include Pediment - bedrock ramp that leads up to the mountain front Plateau- large flat undeformed area that is topographically higher than the surrounding region Mesa- Smaller than the plateau, but basically the same feature Buttes- smaller than the Mesa, but basically the same feature Spires (a.k.a. Hoodoos)- smaller than the buttes
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Piedmont in Colorado
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Colorado Plateau with Grand Canyon
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A Mesa
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Buttes and Spires in Monument valley, Utah
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Yardang
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Desert Pavement and Desert Varnish
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Ventifact
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ventifacts
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Walking Boulders
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