Glacial Landscapes in the UK Flashcards
Relief of the land
Refers to the highest and lowest elevation points in an area. e.g. mountains and rivers are typically the highest elevation points
Topography
The natural features of land, especially the shape of its surface.
Altitude
Height above sea level, measured in metres or feet.
Land use
The purpose or function of land for example pasture, grassland, retail.
Lowland
Are close to or below 200m above sea level. One example is the Fens in East Anglia.
Uplands
Are normally made up of mountains or high hills. Normally they are areas over 600m above sea level. Examples include the Cumbria mountains in the Lake District.
Glacial erosion
The wearing away and removal of the land by flowing water, ice or wind.
Plucking
Is where a glacier moves over an area of rock. Due to friction, the glacier melts and water seeps into cracks around the rocks below. The water freezes and the rock effectively becomes part of the glacier and is ripped out when the glacier continues to move forward.
Abrasion
Is where rocks at the bottom of the glacier act like sandpaper - grinding over the bedrock. This can polish the rocks or create sharp grooves called striations.
Bulldozing
When a glacier moves forward it can act like a giant earthmover, bulldozing piles of rock debris in front of it to create a high ridge called moraine. The furthest advance of a glacier is marked by a terminal moraine.
Glacial Till
Sediment transported by ice.
Moraine till
Sediment that is deposited
Outwash
Sediment carried by meltwater. Is more rounded due to attrition by river erosion.
Corrie
Corries are bowl shaped hollows with a steep back wall and ridges, forming an armchair shape around a hollow sometimes containing a small round lake called a tarn.
Aretes
A freeze-thawed ridge that develops when 2 corries are side by side/back to back.