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Desert Landscapes
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Deserts Dry regions cover 30 percent of Earth’s land surface
Distribution and causes of dry lands Two climatic types are commonly recognized Desert or arid Steppe or semiarid
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Arid and Semiarid Regions
Figure
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Rainshadow Desert Figure 4.21
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Wind Processes and Desert Landscapes
The Work of Wind Overview of Desert Landscapes
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The Work of Wind Eolian Erosion Eolian Transportation
Eolian Depositional Landforms Loess Deposits
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The Work of Wind Figure 12.1
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Desert Pavement Figure 12.2
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Yardang Figure 12.3
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Dust Over the Red Sea Figure 12.4
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Sand Transport Figure 12.5
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Sand Transport Figure 12.5
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Sand Ripples Figure 12.7
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Dune Cross Section Figure 12.9
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Major Dune Forms Figure
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Sand Dunes in the Western United States
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Sandy Regions of the World
Figure
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Loess Regions of the World
Figure
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Loess Deposits Figure
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Overview of Desert Landscapes
Desert Climates Desert Fluvial Processes Desert Landscapes Desertification
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Death Valley
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Alluvial Fan Figure
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Differential Weathering
Figure
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Cross Bedding Figure
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Deserts Role of water in arid climates
Most streambeds are dry most of the time Desert streams are said to be ephemeral Carry water only during periods of rainfall Different names are used for desert streams in various region Wash and arroyo (western United States) Wadi (Arabia and North Africa)
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Deserts Role of water in arid climates Ephemeral streams
Different names are used for desert streams in various regions Donga (South America) Nullah (India) Desert rainfall Rain often occurs as heavy showers
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Deserts Role of water in arid climates Desert rainfall
Because desert vegetative cover is sparse, runoff is largely unhindered and flash floods are common Poorly integrated drainage systems and streams lack an extensive system of tributaries Most of the erosion work in a desert is done by running water
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A Dry Channel Contains Water Only Following Heavy Rain
Figure 4.22
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Basin and Range Figure
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Colorado River Basin Figure 1
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Inselbergs in So California
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