Paper 1 Glaciers Flashcards
What is plucking in glacial erosion?
Plucking occurs when meltwater at the base, back, or sides of a glacier freezes onto rock, and as the glacier moves forward, pieces of rock are pulled out.
Plucking is a significant process in glacial erosion, contributing to the landscape’s alteration.
What is abrasion in glacial erosion?
Abrasion is when rock frozen in the glacier grinds against the rock underneath, wearing it away.
This process contributes to the smoothing and shaping of the landscape beneath glaciers.
What is freeze-thaw weathering?
Freeze-thaw weathering occurs when water freezes in cracks in the rock and expands, further cracking the rock and causing pieces to break off.
This process is a key mechanism of weathering in cold climates.
How does the weight of ice affect glacier movement?
The weight of the ice makes the glacier move downhill.
This movement is crucial for the glacier’s ability to erode and shape the landscape.
What is rotational slip in glacier movement?
Rotational slip is when the top end of the glacier moves in a circular motion, which can erode landforms in the landscape.
This type of movement can lead to significant changes in the terrain.
What regions were covered by ice during the last glacial period?
During the last glacial period, ice covered most of Scotland, Ireland, and Wales.
Approximately 30% of England was not glaciated, but ice reached as far south as Bristol.
what is an arête
a narrow steep sided ridge
how is an arête formed
when 2 glaciers erode in parallel valleys and the glaciers erode the sides of the valleys, sharpening the ridge
example of an arête
striding edge, lake district
what is a pyramidal peak
a pointed mountain peak with at least 3 sides
how is a pyramidal peak formed
by at least 3 glaciers eroding back to back
example of a pyramidal peak
Snowdon, Wales
How is a corrie formed?
- begins as a hollow containing a small glacier
- ice moves by rotational slip and erodes the hollow into a steep-sided armchair shape with a lip at the bottom end
what can a corrie form when the ice melts
a tarn- a small, circular lake
eg. Red Tarn, Lake District
what is a ribbon lake
a long,thin lake that forms after glacial retreat
where do ribbon lakes form?
in hollows where softer rock was eroded more than harder rock
example of a ribbon lake
lake Windermere, lake district
what is a truncated spur
a cliff-like edge on the side of a valley
how are truncated spurs formed
formed when ridges of land that stick out into the main valley are cut off as the glacier moves past
what are hanging valleys?
valleys formed by smaller glaciers that flow into the main glacier
why are hanging valleys at a higher level that the valley of the large glaciers
the glacial trough is eroded much more deeply by the large glacier, leaving the hanging valleys at a higher level
what is a glacial trough
a steep-sided valley with a flat bottom
how are glacial troughs (or U-shaped valleys) formed?
they start of as a v-shaped river valley, changing to a U shape as the glaciers erode erodes the sides and bottom, making it wider and deeper
what are drumlins
elongated hills of glacial deposits