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Arid Landforms
Basic Concepts I. Most deserts exhibit highly angular landscapes. ,[object Object]
 angular particles of weathered rock; bedrock outcrops
 little soil or vegetation to soften landscape II. Softer, more rounded landscapes appear where deposition is predominant. ,[object Object],III. Desert rainfall is infrequent, intense, and unreliable. ,[object Object]
 ephemeral streams,[object Object]
Death Valley, July 15, 1999
Las Vegas Flash Flood
Types of Deserts Erg - sea of sand ,[object Object]
 vegetation rare
 sand probably formed during more humid climate,[object Object]
Types of Deserts Reg - desert “pavement” of pebbles and stones ,[object Object]
 may be very thin coating of stones,[object Object]
Hamada - bedrock predominates
Desert varnish - oxidation of iron and manganese, useful for dating desert surfaces
DESERT FLUVIAL PROCESSES/LANDFORMS  Fluvial Erosion - rare, intense flash floods. ,[object Object]
 fluvial systems decrease in discharge downstreamFluvial Transportation - large amounts of rock and sand moved short distances. Fluvial Deposition – where water slows on flat playas material is deposited and sorted by size. ,[object Object]
 rock debris in piedmont region,[object Object]
Virga
Joshua Tree N.P.
Slot Canyon
The Narrows, Zion N.P., Utah
AEOLIAN (WIND) PROCESSES/LANDFORMS  Aeolian Erosion - much less effective than fluvial ,[object Object]
 abrasion - polishes and etches exposed surfacesAeolian Transportation - moves nothing bigger than sand ,[object Object]
 sand storms - only very near the surfaceAeolian Deposition - dunes form and shift where winds and terrain combine to slow the winds or block the movement of dunes.
Dust Storm, Senegal Sand Storm
AEOLIAN (WIND) PROCESSES/LANDFORMS
Types of Dunes  BARCHAN TRANSVERSE DUNES SEIFS
Types of Dunes  Barchans- migrating crescent dune with horns pointing downwind; form where strong winds blow in a consistent direction. Move fast. Common in central Asia and Sahara. Can reach hundreds of feet in height.
Transverse Dunes - parallel waves of crescent dunes perpendicular to wind direction; migrate downwind. Found in areas with large supply of sand.
Seifs - multiple very long narrow, parallel dunes. May be caused in areas with at least two dominant wind directions. Can be tens of miles long. Common outside of U.S.
Namib Desert Star Dunes
BASIN AND RANGE TOPOGRAPHY
Piedmont - gently sloping land that extends out from base of mountains. Pediment - sloping bedrock at base that develops.
Badwater, Death Valley, CA
Playas
Mesa and Scarp Topography
Differential Erosion

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