factors effecting glaciated landscape Flashcards

1
Q

climate

A

Precipitation

  • amount if rain or snow
  • aeolian processes contribute to glaciated landscapes

Temperature

  • how hot/ cold it is = affecting the movement
  • temps above 0 = ablation > accumulation -> outputs
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2
Q

geology

A

lithology

  • physical and chemical composition of rocks
  • harder rock = slower erosion

structure

  • Properties of individual rock types: jointing, bedding and faulting
  • permeability of rocks
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3
Q

geology lithology - clay

A
  • Clay = weak lithology -> bonds between particles, weak

- Little resistance to erosion weathering mass movements

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4
Q

geology lithology - basalt

A
  • Basalt (dense interlocking crystals)
  • highly resistant
  • forms prominent glacial landforms
    EX - arêtes and pyramidal peaks
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5
Q

geology lithology - limestone

A
  • limestone (predominantly calcium carbonate)

- soluble in weak acids -> vulnerable to decay via chemical weathering process of carbonation @ low levels

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6
Q

geology - structure - chalk

A
  • chalk = pours rocks

- tiny air pores separate the mineral particles

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7
Q

geology - structure - carboniferous limestone

A
  • primary permeability (these pores absorb & store water)

- secondary permeability ( permeable but water seeps into it bc of its many joints

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8
Q

geology - structure - angle of dip

A
  • affects the valley side profile
  • stronger = parallel structure and equal spaces apart
  • weaker = curved and unequal
  • can be chipped = exposed areas to water = weakened rocks
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9
Q

latitude

A
  • How far North from the equator
  • High latitude = away from equator, low precipitation levels and low altitudes
    EX - Vostok station in Antarctica, 4.5mm of precipitation
    High latitudes (low altitudes) = beyond Artic -> Antarctic circles @ 66.5 degreed N&S
  • dry climates
  • little precipitation
  • large, stable ice sheets
    EX - Greenland & Antarcti
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10
Q

altitude

A
  • How far above sea levels
  • Higher = colder
  • High altitude = high precipitation levels
    EX - Jasper National park in Canada Rockies = above 600mm
  • High altitudes (low latitudes)
    EX - rocky mountains, Himalayas
  • variable temperatures
  • more summer melting
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11
Q

relief

A
  • The gradient
  • Larger gradient = more energy = more erosion
  • Steeper relief = greater resultant force of gravity (GPE)
  • Impact on microclimates and the moment of glacier
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12
Q

aspect

A
  • Placement of the sun
  • Aspect of slope faces away from general direction go sun
  • Less solar energy received = less melting
  • North facing slopes are larger because there’s less sunlight
  • Mass balance in these areas positive -> glacier advancing = larger glacier, - —- more erosive power
  • Mass balance negative = retreating glacier -> smaller glacier etc
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13
Q

ice formation

A

Diagenesis
Formation of glacier
More inputs of precipitation = more pressure = larger glacier = more erosion

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14
Q

glacier movement - valley glacier

A
  • large, slow-moving masses of ice
  • confined by valley sides
  • may be outlet glaciers from ice sheets or corrie glaciers
  • 10-30km in length
  • BUT - Karakoram Mountains, Pakistan = 60km
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15
Q

glacial movement - ice sheet

A
  • largest accumulation of ice - 50,000km2
  • 96% of worlds ice
  • Antarctic: covered 13.6 million km2, volume 30 million km2 and thickness 4700m+ deep
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16
Q

meltwater

A
  • Meltwater underneath glacier increases the movement

- More meltwater = shrinkage of glacier & more pressure

17
Q

erosion

A
  • Erosion takes place on all surfaces of glacier

- Helps movement

18
Q

deposition

A
  • The landforms left behind by glacier

- Erratic, moraine, drumlins etc

19
Q

climate change

A
  • Increase or decrease in temperate

- Colder temp = more powerful and larger glaciers

20
Q

landforms

A
  • Particular feature in a landscape