Geology:

Desert Geologic Features


About one-third of the earth's landmass is desert or semi-desert. These regions have unique geologic features not found in more humid environments. These features are most often caused by wind and water erosion in the stark desert environment.

Deserts are usually created because they are located in a Rain Shadow -- a dry region downwind of mountain ranges caused by air losing its moisture as it passes over mountains.

Desert areas usually have Internal Drainage -- when streams drain toward landlocked basins rather than flowing eventually to the sea. When the water from these basins dry it is called a playa.

Because of the factors above, deserts often have less vegetation to prevent erosion, which in turn leads to further barrenness through Deflation -- the removal of silt and sand particles from the land surface by wind.

Below are some geologic features and unique charactreristic of the desert regions:

Alluvial Fan: A large, fan-shaped pile of sediment -- unconsolidated gravel, sand, silt and clay -- forming at the base of narrow canyons onto a flat plain at the foot of a mountain range.

Arroyo: A dry desert gully, usually a small, narrow canyon with steep walls and flat, gravel strewn floor.

Bajada: A broad, sloping depositional surface at the base of a mountain range caused by the coalescing of alluvial fans.

Blowout: A depression in the land surface caused by wind erosion.

Butte: A narrow, flat-topped hill of resistant rock with very steep sides. Probably formerly a mesa.

Desert Pavement: A thin, surface layer of closely packed pebbles.

Desert Varnish: A hard, dark, shiny coating on rocks caused by chemical/biological action.

Dunes: Mounds of loose sand grains shaped by the wind.

Flash Flood: Sudden local flood of high discharge and short duration.

Hoodoo: A bizarre-shaped column or pillar caused by differential erosion on rocks of different hardness.

Loess: Deposit of wind-blow silt and clay in angular grains and weakly cemented by calcite.

Mesa: A large, broad, flat-topped hill bounded by cliffs and capped with a resistant rock layer.

Mudflow: In the desert, usually flash flood laden with enough sediment to become plastic.

Pediment: A gently sloping surface cut into the solid rock of a mountain, covered with a thin layer of gravel. Occurs uphill of a bajada, which is completely depositional.

Playa: A very flat, dry lakebed of hard, mud-cracked clay.

Ventifacts: Rocks with flat, abraded surfaces caused by wind-blown sand.

-- Bob Katz


Desert Minerals & Geology Index
Things To Do: Rockhounding
The Desert Environment

Rainbow Basin Natural Landmark -
A major feature in Rainbow Basin is the unique formation called the Barstow Syncline — a "U" shaped fold in the rocks. In structural geology, a syncline is a downward-curving fold, with layers that dip toward the center of the structure.


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