Chapter 13-16 Flashcards
Arid and semi-arid lands
Drylands
An arid land that receives less than 250mm of rainfall or snow equivalent per year and is sparsely vegetated unless it is irrigated
Desert (arid)
Land in which the annual rainfall ranges between 250 and 500mm
Semi-arid
Associated with the two belts of low rainfall near the 30N and 30S latitudes. Includes the Sahara, Kalahari, and the Great Australian deserts.
Subtropical deserts
This receives as little precipitation as sub-tropical deserts, but because the precipitation comes in the form of snow that never gets a chance to melt, these deserts gradually build up a thick ice sheet
Polar deserts
Forms when a mountain range creates a barrier to the flow of moist air, causing a zone of low precipitation to form on the downwind side of the range
Rainshadow desert
Occur locally along the western margins of continents, where cold, upwelling seawater cools and stabilizes maritime air flowing onshore, decreasing its ability to form precipitation
Coastal desert
Wind processes
Eolian
Sediment transport in which the wind causes particles to roll along the ground
Surface creep
Sediment transport in which particles move forward in a series of short jumps along arc shaped paths
Saltation
Sediment transport in which the wind carries very fine particles over long distances and periods of time
Suspension
Wind erosion in which airborne particles chip small fragments off rocks that protrude above the surface
Abrasion
“Wind artifact”
Ventifact
Steep-sided but flat topped desert landforms
Buttes
And erosion in which loose particles of sand and dust are removed by the wind leaving coarser particles behind
Deflation
Fine particles are removed, leaving a continuous pavement-like covering of coarse particles
Desert pavement
A hill or ridge of sand deposited by winds
Dunes
A leeward slope of a dune
Slip face
Crisscrossed strata within a dune. Former slip faces
Cross beds
The steepest angle at which loose particles will come to rest
Angle of repose
Dunes may migrate over long distances, and they can cause severe degradation and loss of agricultural productivity when they invade non-desert lands
Desertification
Crescent shaped dunes which are very mobile
Barchans
If the wind blows in several different directions, it piles up into stationary ____
Star dunes
When there is a copious sand supply, bar chan dunes can merge and form _____
Transverse dunes
Dunes that run parallel to the prevailing winds
Longitudinal dunes
These are oriented in the opposite direction from bar chan dunes: the arms, stabilized by vegetation, point upwind
Parabolic dunes
A steep-sided canyon where rapid runoff erodes into the landscape
Arroyos
If canyons are closely spaced along the base of a mountain range, the alluvial fans will sometimes coalesce into a broad alluvial apron called ____
Bajada
Invasion of desert conditions into non-desert areas
Desertification
Land damage or loss of productivity caused by human activity, which may lead to the advance of desert condition into non-desert areas
Land degradation
The perennially frozen part of the hydrosphere
Cryoshpere
A semi-permanent or perennially frozen body of ice, consisting largely of recrystallized snow, which moves under the pull of gravity
Glacier
The largest type of glacier. A continent-sized mass of ice that covers all or nearly all the land within its margins
Ice sheet
Thick sheets of floating ice hundreds of meters thick that adjoin glaciers on land
Ice shelves
Large pieces of ice that fall off of ice shelves
Icebergs