Chapter 15 -- Deserts and Stuff Flashcards
An area with less than ##cm (## inches)of annual precipitation.
_______ may be cold, temperate, or hot. All major continents have one type of desert or the other.
In desert regions the wind is an effective agent of ________ and _________ due to a lack of water.
Covers about ##% of the land on Earth.
Desert
Erosion and Transportation
25cm (10in)
The expansion of deserts into formerly productive lands.
These expansions destroy croplands and rangelands.
Causes starvation forcing people from their homelands
Main causes are drought and overpopulation
Closely related to global warming
Desertification
Signs of Desertification (6)
Lowering of water table
Marked reduction of water supply
Increased salinity in water and soil
Progressive destruction of native vegetation
Accelerated soil erosion
Death of cattle - water dependent - foods
Material too large or heavy to be carried in suspension by water or wind.
Particles are moved along the surface by saltation, rolling, or sliding.
Bed Load
Material that can be carried in suspension by water or wind.
Composed of silt and clay sized particles.
Can be carried for thousands of kilometers.
Suspended Load
Wind erosion can be caused through
Abrasion or Deflation
Is the impact of saltating sand grains on an object. Its effect is similar to sandblasting.
Abrasion
Stones whose surfaces have been polished, pitted, grooved, or faceted by the wind.
They are a common artifact of abrasion.
Ventifacts
Is the removal of loose surface material by wind.
Deflation
Is left behind after wind has removed the finer grained material and it protects the underlying material from deflation.
Desert Pavement
Occur in several distinctive types, consist of sand, and are deposited near their source and covers ##% of the land.
Mounds or ridges of wind deposited sand close to its source
Form when wind flows over and around the obstruction, resulting in the deposition of sand grains, which accumulate.
Dunes
10%
Consists of windblown silt and clay deposits composed of angular quartz grains, feldspar, micas, and calcite often found far from their source and covers 10% of the earth’s land and 30% of the US
Sources: Deserts, Pleistocene glacial deposits, floodplains.
Erode easily
Weathers to a rich, fertile soil.
Loess
Types of Sand Dunes
Crescent shaped dunes whose tips point downwind
Form in the areas that have a generally flat, dry surface with little vegetation, a limited sand supply, constant wind direction.
Most mobile dune, up to 10m/yr
Barchan Dune
Types of Dunes
Long, parallel ridges of sand aligned generally parallel to the direction of the prevailing winds.
Form where the sand supply is somewhat limited.
Can be up to 100m high (common in Egypt and Australia)
Longitudinal Dunes
Types of Dunes
Form long ridges perpendicular to the prevailing wind direction
Found in areas that have abundant sand and little to no vegetation.
Crest up to 200m high.
Transverse Dunes