Ice on the land Flashcards
Interglacial period
Ice melts when temperature increases or gets hotter
Glacial period
Ice advances as temperature starts to decrease or gets colder
Ice sheet
Body of ice over 50,000 km (2) in extent
Ice cap
Smaller body of ice. Less than 50,000 km
Glacier
A finger of ice extending downhill
Abrasion (erosion)
Sand paper effect as the glacier scours the valley floor because of rocks underneath the glacier leaving striations
Plucking (erosion)
Water melting underneath the glacier bonds with the rocky surface and freezes due to freeze thaw weathering like glue. When the glacier moves the rocks are plucked away like loose teeth leaving jagged rocky surfaces
Corries
Large hollowed out depressions on upper slopes of glaciated valleys
Formation of Corries
Snow accumulates in a sheltered hollow and the snow turns into ice and a small corrie glacier is formed. Through the process of rotational slip, the glacier scoops put a deep hollow. If there is less erosion in front of the corrie this will cause a lip to raise, and the ice will melt forming a tarn behind the lip
Arête
An knife edged ridge at the back of a corrie separating 2 glaciated valleys
Formation Pyramidal peak
When 3 or more corrie are formed on a mountain the process of erosion may lead to a formation of a single peak rather than a ridge
Truncated spur
A ridge that descends towards a valley floor from a higher elevation
Formation of truncated spur
In a v shaped valley, When a glacier cannot flow around existing interlocking Spurs, the glacier will simply cut through them, forming truncated Spurs with steep edges
Glacial trough
Steep sided, wide and flat bottomed valley due to the process of abrasion
Ribbon lake
Long narrow lake at the bottom of a glacial trough