Glaciation Flashcards
What is the case study for Glaciation
The Lake district
Name a corrie in the lake district
NE side of Helyvellyn
Name an Arête in the lake district
Striding edge
Name a pyramidal peak in the lake district
Scafell pike
name the processes of erosion
plucking
abrasion
freeze- thaw weathering
describe plucking
Ice freezes onto cracked rocks
ice moves downhill due to the force of gravity and tears out pieces of rock
leaving behind a ruff or ragged surface
describe abrasion
peices of rock frozen onto the base of a glacier grind away the landscape underneath it
leaving a smooth polished surface
describe freeze thaw weathering
water enters cracks and freezes and expands and contracts
after many times expanding and contracting rocks eventually break off
leaving behind a ragged surface
describe the formation of a corrie
- snow gathers in north facing hallows
- snow pills up and compresses lower layers of snow turning them into ice called glaciers
- the back of the hallow was steeped by plucking
- the base of the hallow was depended by abrasion
- rocks in the back wall were removed by freeze thaw weathering
- the rotation movement create a deep hallow and a rock lip from over deepening
- when ice melted a deep step backed semi circular hallow was left
- a corrie loch or tarn was left in the base of a corrie
decribe the formation of an arête
an arête is a ridge that results when two corrie are formed back to back
describe how a corrie is formed ….
glaciers eroded backwards
- the edge becomes narrow until a narrow ridge was formed called an arête
- the ridge is jagged as it is exposed to freeze thaw weathering
describe the formation of a pyramidal peak
three corries form back to back
explain corries …
corries we’re created on all sides of the mountain
arêtes seperate the corries
as the corries eroded backwards and got bigger a steep sided peak between them was formed
ftw eroded the top of the mountain abc created a pyramidal peak
describe the formation of a u shaped valley
- glaciers flowed into v shaped valleys and changed it shape by eroding it
- the sides of the valley were steepened by plucking
- the valley flor became wider and deeper by abrasion
- the valley also was stepped by ftw
- interlocking spurs were eroded creating truncated spurs making the valley staigheter
it became deeper and steeper creating such shape
-now there is no ice they have small rivers called misfit streams running through them - some u shaped valley floors were over deepened and were filled with water called ribbon lakes
hanging valleys
tributary river valley had small glaciers
ther valleys eroded less deeply
tributary valley hung over u shaped valley
rivers flowing fell down steep gradients to join the main river
rivers often fall in the form of a waterfall
an alluvial fan is formed at the bad when materials are deposited
formation of a ribbon lake
some glaciers were able to erode more deeply
a barrier of hard rock ran across the valley
this acted as an obstruction
the ice was dammed so the glacier thickened and became a more powerful eroded
ice flowing over the barrier was faster and stronger
as a result the glacier over deepened the valley
when the ice melted it resulted in the formation of a king narrown ribbon lake
name land uses in the lake district
hill sheep farming
forestry
water supply
industry
renewable energy
tourism