D:Hot and Semi-Arid Environments Flashcards

(44 cards)

1
Q

What are the 4 different types of desert landscapes

A
  1. Mountain Deserts
  2. Sand Deserts
  3. Shield Deserts
  4. Stony Deserts
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Characteristics of a mountain desert

A
  • Exposed bedrock
  • Steep surfaces
  • Upland with desert lake basins and salt flats
  • e.g. Ksar Plateau, Tunisia
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Characteristics of a sand desert

A

the presence of ergs (broad flat area covered in sand).

  • Vegetation is rare
  • Desert likely formed during a pluvial period
  • e.g. The Sahara
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Characteristics of a stony desert

A
  • Sediment has been removed by deflation
  • Bigger pebbles and rocks get left behind forming a desert pavement
  • e.g. Syrian-Jordanian Desert
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Characteristics of a shield desert

A
  • Hamada (bare rock plateau surfaces)
  • Scattered rock fragments
  • e.g. Chott-el Djerid, South Tunisia
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Define Equifinality, in terms of landforms

A

They are landforms that look similar but have been formed in different ways

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

What are the 5 erosional landforms due to wind

A
  1. Deflation Hollows
  2. Ventifacts
  3. Rock pedestals
  4. Zeugen
  5. Yardangs
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

What are the 8 erosional landforms due to water

A
  1. Wadi
  2. Arroyos
  3. Canyons
  4. Mesas
  5. Buttes
  6. Inselbergs
  7. Surface Crusts
  8. Pediments
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What is a deflation hollow

A

Large enclosed surface depressions that have been created by the removal of large amounts of loose particles by the wind.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

What is a ventifact

A

Individual rocks with sharp edges

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

What is a rock pedestal

A

Mushroom shaped rocks that occur where an isolated rock has been eroded more rapidly as the base, causing it to have a top-heavy shape.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

What is a Zeugen

A

A narrow ridge of land, with protective cap rock above it

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

What is a Yardang

A

They are steep-crested, linear ridges of clay/rock. They consist of parallel troughs, separated by regular ridges

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

What’s the difference between sheet floods and flash floods

A

Sheet floods are overland flow of water during heavy rainfall, while flash floods tend to occur in channels

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

What is a Wadis

A

A dry river bed that form temporary channels following periods of heavy rain. Most are ephemeral rivers, with steep sides and a wide channel floor. e.g. Atlas Mountains Morocco

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Formation of Wadis

A
  1. Formed during flash floods in a steep and smooth landscape
  2. The floods cut the rills and widen them into gullies
  3. The streams of water then widen the gullies to form steep sided valleys known as Wadis
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

What is an Arroyo

A

Its a dry riverbed or seasonally active creek. They completely dry up during dry periods and are filled with water and become active again after substantial rainfall

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

How do Arroyo’s form

A
  1. Most arroyos form as a result of flash-flooding. The flash flood cuts through the dry ground to create these geological formation
  2. Ephemeral streams,which are rivers that flow intermittently, often generating high discharge
  3. The impermeable surfaces, lack of vegetation and particles being displaced by rain splash all reduce the infiltration rate
  4. Due to these minimal infiltration rates the collective runoff eventually becomes concentrated into deep sided ravines called arroyos
19
Q

Whats the difference between an Arroyo and a Wadis

A

They form in the same way but an Arroyo is narrower

20
Q

What is a Canyon

A

Canyons are desert gorges, much deeper version of wadis. They have steep often vertical sides cut into resistant rock

21
Q

What is a Mesas

A

An elevated area of land with a flat top and sides that are usually steep cliffs. It takes its name from its characteristic table-top shape. Often bordered by steep canyons

22
Q

How does a Mesas Form

A
  1. Through weathering and erosion of horizontally layered rocks that have been uplifted by tectonic activity. Differential erosion is what gives mesas their distinct shape
  2. LEss resistant rocks are eroded away on the surface into the valleys, while the more resistant layers are left standing
23
Q

What is a Butte

A

An isolated hill with steep, often vertical sides and a small relatively flat top. Similar to a mesa but smaller and represent a more advanced stage of landscape development

24
Q

Formation of a Butte

A
  1. Form when hard cap rock overlies a layer of less resistant rock that is eventually worn away
  2. As the top is further eroded, the excess material that falls adds to the scree around the base
25
What is an inselberg
Isolated relict hills of resistant rocks that are more rounded than mesas and buttes
26
What is a surface crust
Extensive areas of flat or gently sloping desert surfaces covered with a mantle of weather debris
27
Formation of a surface crust
1. Formed due to the transportation of fine particle by wind 2. Repeated wetting and drying- when wet there is no removal by wind and stones are pushed towards the surface. When dry, particles are removed and fine particles move down filling spaces left by stones that had risen before 3. They are the end product of surface deflation by wind and selective stone sorting by moisture
28
What is a pediment
They are gently sloping erosional rock surfaces, with an angle of less than 7 degrees, found at the foot of mountain ranges
29
How do pediments form
1. Formed by the parallel retreat of the slope of a plateau 2. As they retreat they leave behind a gently sloping rock platform 3. Parallel retreat occurs because rock is removed from the base of steep slopes at the same rate it is weathered
30
Name the depositional and transportational landforms by wind x6
1. Barchans/Crescent 2. Transverse 3. Seifs 4. Longitudinal/Linear 5. Star 6. Draa
31
What does Dune morphology depend on
1. Sand availability 2. Wind strength, direction and duration 3. Vegetation type and amount 4. Ground surface roughness
32
What is a Barchans/Crescent dune
they have 3 characteristics: 1.Crescent shaped 2. Formed of desert sand 3. Always point towards the wind Material is moved by saltation and surface creep up the windward side, it then slides down the steeper leeward side Usually found around shrybs as they act as anchors to hold the central area in place
33
What is a transverse dune
Resemble ocean waves, they are long, with wavy ridges. They are arranged in rows which are parallel and lie a right angles to the direction of the wind To cause this type of dune there has to be steady trade winds
34
What are seif dunes
Long narrow dunes that form in ridges, shapeddue to winds blowing in 2 directions
35
What are Star dunes
Pyramidal in shape they are the tallest dune, caused by winds coming from many different directions
36
What are draa dunes
They are a sequence of large star dunes forming a ridge
37
What are longitudinal/linear dunes
Form when Barchan dunes become highly elongated, but are very rare
38
Name the 5 depositional and transportational landforms by water
1. Alluvial fans 2. Bajadas 3. Playas 4. Washes 5. Salt Flats
39
What is an alluvial fan
Triangular fan shaped depsoits of water transported material, known as alluvium. Generally form in mountainous regions, where there is a sudden change in gradient
40
Formation of an alluvial fan
1. As flowing water travels down a slope to a lowland, the velocity of the water decreases and it will spread out into a fan shape 2. As the river slows and loses energy, it despoits alluvium, the largest sediment first 3. Depostion is aided as the stream isn't confined to valley walls
41
What is a Bajadas
Created where a number of parallel wadis arrive at the mountain front, causing a series of alluvial fans to join together, creating a continuous apron of sediment covering the lower slopes
42
What is a playas
Hollows on the land surface, that may be occupied by hallow ephemeral saline lakes. The water in the lakes build up, but water is only retained for a short duration
43
What is a desert wash
They are the drainage areas in desert terrains. Runoff scours the lowest lying areas, creating dry beds of loose sandy soil which are desert washes
44
What is a salt flat
As the water leaves the lake through evaporation, it leaves behind deposits of soluble salts that were carried in solution. These