KQ1 - What processes and factors give hot / semi-arid environments their distinctive characteristics? Flashcards

1
Q

How much mean annual precipitation do arid environments get?

A

100-250 mm

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2
Q

How much mean annual precipitation do semi-arid environments get?

A

250-500 mm

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3
Q

What are the characteristics of arid areas?

A
  • Infrequent and unreliable rainfall
  • Some grasses, shrubs and trees grow
  • Pastoral farming only possible where there are perennial streams / aquifers
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4
Q

What are the characteristics of semi-arid areas?

A
  • High and more reliable rainfall
  • Seasonal pattern of rainfall
  • More continuous vegetation
  • Arable farming is possible
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5
Q

What causes aridity?

A
  • High pressure / latitude
  • Hot arid and semi-arid areas are affected by subtropical high pressure cells found 30 degrees north and south of the equator
  • Continentality
  • Rain Shadow / relief
  • Ocean currents / offshore winds
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6
Q

Why does sinking are provide ideal air conditions?

A
  • Dry air
  • Cloudless and warm
  • Persistant
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7
Q

Why does continentality affect areas?

A

Areas in the centre of land masses (central Australia) are dry because they are far from rain-bearing winds which collect moisture from the sea

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8
Q

Why does rain shadow / relief affect areas?

A
  • High mountain ranges block the passage of rain-bearing winds which increases aridity on the sheltered side
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9
Q

What is the distribution of arid areas?

A
  • Hyper-arid mainly in Africa
  • Deserts further north and south of the equator
  • Concentrated on the west side of continents
  • Hyper arid surrounded by arid surrounded by semi-arid
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10
Q

What is mechanical weathering?

A
  • occurs as a result of sudden temperature changes between hot days and freezing nights
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11
Q

Name mechanical weathering processes

A
  • Shattering: Rocks which have neither coarse grains nor blocky structure ma shatter into irregular fragments with sharp edges.
  • Exfoliation: expansion and contraction causes the surface layer flakes off, as it is more exposed to temperature. The peeling of process is known as ‘onion-skin weathering’
  • Granular disintegration: grain rocks e.g. granite break down into grains of sand. Granite breaks down quickly as it contains black and white crystals which heat up and cool down at different rates.
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12
Q

Name chemical weathering proccesses

A
  • Hydrolysis: the breakdown of rock by acidic water to produce clay and soluble salts
  • Oxidation: the breakdown of rock by oxygen and water, often giving iron-rich rocks a rusty coloured weathered surface
  • Crystal growth: salt crystals grow between pores and joints when high temps draw saline groundwater to the surface and the water evaporates. They lead to granular and block disintegration.
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13
Q

What are the other forms of weathering?

A

Wetting and drying (rain also chills the rocks): repeated expansion on wetting and contraction on drying causes the rock to disintegrate

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14
Q

Why is wind erosion so effective?

A
  • Extreme pressure differences
  • Little vegetation to slow wind
  • A lot of fine debris from mechanical weathering
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15
Q

What are the wind processes?

A
  • Abrasion: when wind-blown sand abrades rock surfaces

* Attrition: the action of sand grains colliding with each other and in doing so becoming smaller

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16
Q

How does wind transport?

A
  • Suspension: fine sediment carried within the air
  • Saltation: usually sand grains hopping along the surface
  • Surface creep: rolling along the ground
17
Q

Name the landforms formed by wind erosion?

A
  • Yardang
  • Rock pedestals
  • Desert pavement
  • Ventifact
18
Q

What is a yardang?

A
  • Steep-crested, linear ridges of rock orientated parallel to the prevailing wind
  • Occur in groups
  • Develop is easily eroded soft, but cohesive, sediments e.g. silt and clay and in more resistant rocks e.g. limestone and sandstone
  • Length to width ratio = 4:1
  • Can vary in height from a few cm’s to over 100m and can be several km’s in length
19
Q

What is a rock pedestal?

A
  • Zeugen= a type of pedestal rock with a resistant cap rock
  • The top is case hardened by rising ground water that contains salts
  • Case hardened: formation of a mineral coating on the surface of porous rock by evaporation of a mineral-bearing solution
  • These salts crystallise (a form of weathering) in the upper part, so it becomes hardened to erosion and further weathering
  • The bottom part/stem is thing due to the process of wind abrasion- saltating grains abrade the rock between 0-60cm. it is more effective here as it is not case hardened.
20
Q

What is a ventidact?

A
  • wind-polished stones which look like Brazil nuts and are a few centimetres in size
21
Q

What is a landform formed by wind deposition?

A

Sand dune e.g. Namib Sand seas
• Description → a mound of sand built by Aeolian processes. A desert covered with dunes is known as a sand sea. There are many different types of dunes such as transverse dunes, linear dunes and star dunes. Dunes are found all over the world
• Explanation → they are formed depending on the direction of the wind. Sand is transported by suspension, saltation or by surface creep; sand deposited as dunes by the wind can be divided into 2 main types

22
Q

Name the types of water erosion

A
  • Flash floods: rare thunderstorms but ground is baked so runoff is rapid
  • Exogenous rivers (a permanent river deriving its flow from beyond the desert margin): flow from wetter areas
  • Historic water: at the end of the last ice ages, these climates were wetter
  • Underground water: groundwater
  • Fog may bring moisture to these arid areas
23
Q

What are landforms formed by water erosion?

A
  • Alluvial Fans
  • Salt Pans / Playa Lake
  • Canyon
  • Wadis
24
Q

What are alluvial fans?

A
  • A fan shaped deposit made up of sediment overtime, often found at the base of mountain ranges where intermittent streams flow out e.g. at the end of a wadi or canyon
  • Sediment drops out of stream flow as energy decreases due to widening of the channel
  • Sediment builds up overtime in the channels at the base of the mountains and forces the stream to carve another channel
25
Q

What are salt pans / playa lake?

A
  • Formed where water pools evaporate
  • Large and flat areas of land that were once lake beds
  • Covered with salt and other minerals, often look white due to salt presence
26
Q

What are wadis?

A
  • Dry river bed with steep sides and a wide floor covered with channel deposits
  • Form when flash floods/seasonal rain creates an ephemeral river (temporary river flowing seasonally/intermittently)
  • High discharge with the availability of loose, dry sediment in the channel bed encourages the transport of large amounts of sediment
  • Boulders are abraded and underlying bed rock is scoured
  • Vary in size from a single channel a few metres long to dense networks many km’s in length
27
Q

What is a canyon?

A
  • A gorge with a deep, narrow channel bounded by resistant rocks
  • Result from vertical erosion by rivers, which carry coarse loads at times of high flow, … abrading the channel base … = deeper
  • Valley floor often occupied by an exogenous river e.g. the Colorado