Aeolian Environment Flashcards

1
Q

a. Less than 250mm/yr precipitation

b. between 250 and 500mm/yr

A

a. Desert (Arid)

b. Steppe (Semi-Arid)

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2
Q

(a) -Regions near 30° N & S latitude air sinks
(subtropical highs)
-Produce clear skies, sunshine, and ongoing
drought

(b) Give one example

A

Low Lattitude Desert

Simpson Desert

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3
Q

(a) -Located in the deep interiors of continents
- Precipitation only 10-20 cm/yr

(b) Give one example

A

Mid Lattitude Desert

Gobi Desert

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4
Q

are formed because tall mountain ranges prevent moisture-rich clouds from reaching areas on the lee, or protected side, of the range. As air rises over the mountain, water is precipitated and the air loses its moisture content.

A

Rainshadow Desert

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5
Q
  • Mean summer temperatures of -1.5 to 2° C
  • Mean winter temperatures of -32 to -23° C

(b) Give one example

A

Polar Desert

Antarctic Desert

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6
Q

is an area where sand has accumulated as a result of

aeolian processes.

A

Erg

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7
Q

is blowing out and scattering of rock particles by

wind.

A

Deflation

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8
Q

are sandy depressions in a sand dune ecosystem

(psammosere) caused by the removal of sediments by wind

A

Blowouts

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9
Q

is the mechanical scraping of a rock surface, by

friction between rocks and moving particles

A

Abrasion

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10
Q

Long exposure of rock surface in the oxidizing conditions of a desert also results of a dark, surface patina of iron and manganese oxides

A

Desert Varnish

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11
Q

impact of saltating grains to have a frosted patina, like the frosting of glass windows

A

Grain Surface Frosting

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12
Q

the selective removal of finer grains from the sediment in a flow, but is more effective in the lower density and viscosity medium of air

A

Winnowing Effect

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13
Q

consisting of gravel-sized particles that are too large to be transported by the wind

A

Lag Deposits

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14
Q

are dust that accumulate far from their source

A

Loess

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15
Q

a hill or ridge of wind-deposited sand. Ranges from

3m to 600m in wavelength and are between 10cm and 100m high.

A

Dunes

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16
Q

lunate structures with arcuate slips faces forming cross-bedding

A

Barchan Dunes

17
Q

straight-crested forms aligned perpendicular to the prevailing wind direction

A

Transverse Dunes

18
Q

a variety of dune intermediate between barchan and transverse dunes;these dunes form scalloped rows of sand perpendicular to the wind

A

Barchanoid Dunes

19
Q

characterized by cross-bedding reflecting avalanching down on both sides of the dune and oriented in different directions

A

Longitudinal Dunes

20
Q

– slip faces in many orientations and hence crossbedding directions are variable

A

Star Dunes

21
Q

initially originate as blowouts and the dune forms as the head of the dune at the downwind edge of
the blowout

A

Parabolic Dunes

22
Q
wind eroded (sand blasted) surfaces. With
changing direction of dominant winds, different facets
merge along sharp ridges to transform rounded stones to angular \_\_\_\_\_\_\_\_\_
A

Ventifacts

23
Q

are larger hill-sized features sculpted by the

wind. It is composed of cohesive silts and clays, sandstone, or limestone

A

Yardang

24
Q

An isolated mountain remnant characteristic of

the late stage of erosion in a mountainous region

A

Inselberg

25
Q

a broad, flat-topped area elevated above the surrounding land and bounded, at least in part, by cliffs.

A

Plateau

26
Q

a broad, flat-topped hill bounded by cliffs and capped with a resistant rock layer

A

Mesa

27
Q

a narrow hill of resistant rock with a flat top and very steep sides

A

Butte

28
Q

is determined by the amount of water that is charging the water-bearing strata

A

Water Table

29
Q

– sand dunes built up by aeolian action that from

adjacent to beaches in any climatic setting

A

Beach Dunes

30
Q

Wind blowing over the outwash plain can pick up sand

and redeposit it locally, such as the side of a valley.

A

Periglacial Deposit