Arid Lands Flashcards

1
Q

Special Desert Conditions

A

1) Weathering = only mechanical since no water for chemical
2) Soil/Regolith = thin + absent in most places –> lack of soil
3) hardpans widespread –> soil impermeable to water
4) sand = water infiltrates ground + easily moved by heavy winds
5) limited rainfall creates short-distance temporary streams + lack of vegetation
6) underdeveloped drainage systems

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2
Q

Weather type in arid regions

A

1) B climates

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3
Q

Main agent of erosion

A

WATER even in arid landscapes

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4
Q

Exotic Streams

A

1) exotic - water in stream comes from outside desert, usually from higher mountain area
2) ex = Nile River = water comes from mountains of Africa/Ethiopia
3) able to sustain itself through arid environments

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5
Q

Ephemeral Streams

A

1) carry water only seasonally or after rainstorm
2) when carries water = intense erosion, transportation, deposition
3) dry beds of ephemeral streams –> flat floors, sandy bottoms, steep sides

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6
Q

Playas

A

1) Dry lake beds (occasionally fill with water)
2) high salinity bc of evaporation of water

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7
Q

Saline Lakes

A

1) Permanent desert lakes BUT extremely high saline concentrations –> much more evaporation of water compared to inflow

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8
Q

How does fluvial erosion begin in desert

A

1) Begins with brief but intense thunderstorm
2) lots of water on ground BUT bc most of desert soil is impermeable –> water runs off into nearby ephemeral stream
3) fills up with water –> creating flash flood + debris flow

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9
Q

Flash Flood Hazard in desert

A

1) Risk to humans in arid lands
2) Desert cities –> flood-control channels + basins

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10
Q

Differential weathering effect in arid landscape

A

1) striking difference in erosion + weathering bc of sparse cover of soil/vegetation
2) Rocks resistant to weathering –> form cliffs, pinnacles, spires (pointy stuff) while less resistant rocks form gentle slopes

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11
Q

Fluvial Deposition

A

more common than fluvial erosion, most prominent along piedmonts (base area around mountains)

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12
Q

alluvial fan

A

1) Deposition of sediment in piedmont zone
2) occurs because river goes from flowing through mountain gorge into an open piedmont zone (water spreads out –> reduced CC –> drops sediment)

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13
Q

Aeolian processes

A

1) Related to wind action
2) most pronounced + effective in regions with fine grain sand + little vegetation and moisture (deserts_

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14
Q

2 divisions of Aoelian erosion

A

1) deflation
2) abrasian

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15
Q

Deflation

A

1) loose particles blown through air or along ground –> moved by deflation
2) GENERALLY wind not strong enough to move anything more than dust/sand grains

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16
Q

Blowout (deflation hollow)

A

1) shallow depression where abundance of fine material has been deflated
2) generally 1 mile in diameter

17
Q

Abrasion

A

1) similar to fluvial abrasion BUT much less effective
2) the sand/dust hitting rocks results in pitting, etching, faceting, polishing of exposed rock surfaces (ventifacts)
3) found in mesa-and-scarp regions

18
Q

Aeolian Transportation

A

1) finest particles carried in suspension as dust
2) larger particles moved through saltation + traction (like streamflow)

19
Q

Unanchored dunes

A

1) moved by local winds
2) force sand up + over crest (on windward side)
3) goes onto leeward side (slip face) which has a 32-34 degree angle of repose

20
Q

Anchored dunes

A

1) held in place by vegetation BUT they do not provide much nourishment/moisture for plant growth

21
Q

Types of dunes

A

1) Barchan
2) transverse
3) seif (longitudinal)
4) star

22
Q

Sheltered Pocket

A

On opposite side of dune (opposes wind direction)

23
Q

Barchan dunes

A

1) Crescent shaped + formed bc of strong winds blowing in one direction
2) fastest moving dunes

24
Q

Transverse Dunes

A

1) less crescent shaped + occur where entire landscape is sand-covered
2) much more sand than barchans
3) looks like ripples of water

25
Q

Seif (longitudinal)

A

1) Long, narrow + generally parallel
2) created by two dominant wind directions blowing in one direction half of the year and another direction the other half

26
Q

Star Dunes

A

1) pyramid shaped dunes that are star shaped
2) formed in areas where wind constantly changes directions

27
Q

Basin-and-range terrain features

A

1) ranges
2) piedmont zones
3) basins
basin-and-range place without external drainage + some exotic rivers

28
Q

How did basin + range topography form

A

1) repeated process caused by tension forces (inactive rifts)

29
Q

Ranges

A

1) rugged mountain ranges in all directions
2) tend to be long, narrow, parallel to one another
3) have alluvial fans (V-shaped cross sections)

30
Q

Piedmont Zone

A

1) Base of ranges –> zone of transition between steep range slopes to flatness of basin
2) full of alluvial fans + bajadas

31
Q

Bajada

A

1) interconnected alluvial fans
2) as deposition occurs, fans grow larger + interconnect

32
Q

Basins

A

1) Beyond flattish floor –> gently slopes from all sides to low point (usually playa)
2) poor drainage channels
3) salt accumulation common around the playa –> becomes salina if there is enuf salt

33
Q

Mesa-and-Scarp Terrain

A

1) Tall, steep vertical cliffs in the Four Corners Country (Colorado, Utah, Arizona, New Mexico)
2) Grand Canyon

34
Q

Weathering of mesa-scarp formation

A

1) horizontal + sedimentary strata
2) each level has different degrees of erosion which causes abrupt changes in slope angle
3) most resistant layer = at bottom = scarp
4) alternates between scarp + inclined + scarp + inclined
5) top scarp = mesa

35
Q

Plateaus

A

1) Extensive elevated flatlands of uniform horizontal layers

36
Q

Progression from plateau

A

1) Plateau –> mesa –> butte –> pinnacle
2) each consecutive is smaller + more eroded

37
Q

Badlands

A

1) rugged, heavily eroded landscapes
2) lots of ravines + gullies formed by overland flow from rain (effective erosive agent)