Aeloan Flashcards
what is the primary control of deserts
plate tectonics
what are deserts characterized by
- extreme dryness
- hot or cold temps
- specialized ecosystems
- low huma populations
- unique geologic processes
do deserts have more evaporation or precipitation
evaporation
how does evaporation affect a desert ecosystem
evaporation prevents surface water being permanent
is a desert arid or not
yes - extremely arid
how much surface is covered in vegetation in a desert
less than 15%
how much annual rainfall is there in a desert
less than 25 cm
are deserts only in hot climates
NO - can be in cold as well
where are hot deserts found
- low latitudes
- low elevations
are hot deserts found close to oceans
NO - far from oceans
where are cold deserts found
- high latitudes
- high elevations
are cold deserts found far from oceans
NO - found close to them
how much of earth’s land surface is covered by dry regions
30%
what are two common climatic types of dry regions
deserts (Arid)
steppes (semiarid)
what are often found on desert land surfaces
- exposed bedrock
- accumulated clasts
- unweather sediment
- precipitated salt
- windblown sand
5 types of deserts
- subtropical desert
- rain shadow desert
- costal desert
- continental interiors
- polar deserts
example of polar deserts
Antarctica
example of continental interior deserts
Gobi
example of costal deserts
Atacama
example of rain shadow deserts
western Alberta
example of subtropical deserts
Sahara
latitude of subtropical desert
20 to 30 degrees N and S
describe moisture pattern in subtropical deserts
- solar energy evaporates water which rises as hot, moist air
- as the hot air rises it cools and expands
- rain forms
- the air stripped of moisture flows N and S
what is earth’s largest desert
subtropical desert
describe air patterns in rain shadow deserts
- air picks up moisture as it travels over the ocean
- the water heavy air is driven over mountains and cools to form clouds
- the moisture in the air condenses and becomes rain BEFORE REACHING TOP OF MOUNTAIN to form rain forest
- over the mountain, the air stripped of moisture sinks, compresses and sucks water out of the land
type of desert
subtropical
type of desert
rain shadow
type of desert
costal
describe movement of air in costal deserts
- cool air over the cold oceans cannot hold moisture
- as the air interacts with land it absorbs moisture which dries the desert more
where is the driest place on earth
Atacama desert (Peru)
describe air movement in interior deserts
- air loses moisture as it crosses continents
- deserts way inland receives air that is low in moisture and would likely force water out of already dry environment
does air lose or gain moisture as it crosses continents
loses moisture
are interior deserts close to large bodies of water
NO
where can polar deserts be found
above 66 degrees North and S latitude
is there lots of moisture above 66 Degrees N and S
NO
describe movement of air in polar deserts
- air circulation carries dry air to polar regions
- such cold climates means the air cannot hold moisture
processes that happen in a desert
- erosion by water and wind
- weathering
- soil formation
- deposition
type of weathering that dominates deserts
physical weathering
is chemical weathering common in deserts
no - very few chemicals present
what can exposed surfaces in deserts form
desert varnish
what is desert varnish
a dark surface coating of iron and magnesium oxides that forms by bacterial activity, dust and water
describe desert soils
thin with poor defined horizons
describe the colour of desert soils
like bedrock (widely coloured)
what magnifies sediment erosion in deserts
lack of roots = lack of stability against water erosion
what can happen in deserts with lots of rain
flash floods
does water often infiltrate the ground in deserts
no - often remain on the surface due to aquicludes
where do flash floods infiltrate
dry stream beds
types of loads carried by wind erosion
- surface load
- saltation
- suspended load
describe the main types of loads in wind erosion
- surface load
- grains moved in contact with the ground - saltation
- sand skipped and bounced by grain impact (jumping along ground) - suspended load
- sediment carried in the air
what type of clast cannot be lifted and moved by wind
coarse clasts
how do large deposits of sediments form
when finer sediment is removed
what is desert pavement
a surface layer of stones which is resistant to erosion
is desert pavement susceptible to erosion
NO
ventifacts vs yardangs
ventifacts
- rocks pitted, grooved or polished by wind abrasion
- caused by dust suspended by wind
yardangs
- wind sculpted bedrock
sand blasting
rock or other solid object blasted by sand and dust particles suspended and being move through saltation (jumping)
two forms of wind erosion
deflation
abrasion
contrast abrasion and deflation
deflation
- REMOVAL of material by wind transport
abrasion
- mechanical WEATHERING of rock by wind blow sand
what is left behind by deflation
large rock particles that are densely packed (desert pavement)
what is removed by deflation
the top layer of fine very dry soil
what mechanism commonly forms desert pavement
deflation
when do blowout occur
when wind picks up dry fine grained sediment and leaves behind exposed areas
what is vegetation called that remains in place as a blowout forms
pilar
dunes
windblown accumulations of sand
when does wind deposition occur
when wind velocity decreases
two sides to a dune
windward side: side the wind blows (GENTLE SLOPE)
leeward side: side protected from wind (STEEP SLOPE)
two types of wind deposition
- dunes
- loess
what direction do dunes move
direction of wind movement
types of dunes
- star
- barchan
- transverse
- longitudinal
- parabolic
what factors determine shape of dunes
- available sand
- wind velocity
- wind direction
- amount of vegetation present
what direction does sand move in dunes
from windward side to leeward side
what is loess
deposition of very fine grain material (silt and clay)
what is loess thought to be derived from in Europe/NA
glacial and periglacial sources
what is loess thought to be derived from in China
desert sources
barchan dune is what shaped
crescent shaped
where does the horn point in Barchan dune
downwind
where is the steep side on Barchan dune
concave side
describe wind movement in Barchan dune
moves in ONE direction
describe supply of sand needed in Barchan dunes
short supply
type of dune
barchan
type of dune
Barchan
describe shape of parabolic dune
deeply curved
describe horns in parabolic dune
anchored by vegetation
describe movement of wind in parabolic dune
one direction
describe strength of wind in parabolic dune
strong winds
what amount of sand is needed for parabolic dune
large sand supply
describe how parabolic dunes are opposite barchan dunes
their convex side is facing downwind NOT the concave side
type of dune
parabolic
describe shape of transverse dunes
straight and elongated
describe transverse dunes to wind direction
perpendicular to the wind direction
amount of sand needed for transverse dunes
large supply
types of dune
transverse dune
describe shape of longitudinal dunes
extremely long, high and straight
describe longitudinal dunes with wind direction
parallel to wind direction
type of dune
longitudinal
describe shape of star dune
center with radiating arms
describe wind direction for star dunes
changing directions
types of desert deposition
alluvial fans
playas
describe how sediments change in alluvial fans
near source: coarse sediments
away from source: finner
playas
desert lake that have no outlet streams which collect drainage from flash floods