Glacial Landscapes in the UK Flashcards

1
Q

Relief of the land

A

Refers to the highest and lowest elevation points in an area. e.g. mountains and rivers are typically the highest elevation points

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2
Q

Topography

A

The natural features of land, especially the shape of its surface.

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3
Q

Altitude

A

Height above sea level, measured in metres or feet.

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4
Q

Land use

A

The purpose or function of land for example pasture, grassland, retail.

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5
Q

Lowland

A

Are close to or below 200m above sea level. One example is the Fens in East Anglia.

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6
Q

Uplands

A

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.

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7
Q

Glacial erosion

A

The wearing away and removal of the land by flowing water, ice or wind.

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8
Q

Plucking

A

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.

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9
Q

Abrasion

A

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.

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10
Q

Bulldozing

A

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.

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11
Q

Glacial Till

A

Sediment transported by ice.

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12
Q

Moraine till

A

Sediment that is deposited

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13
Q

Outwash

A

Sediment carried by meltwater. Is more rounded due to attrition by river erosion.

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14
Q

Corrie

A

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.

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15
Q

Aretes

A

A freeze-thawed ridge that develops when 2 corries are side by side/back to back.

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16
Q

Pyramidal Peaks

A

Are produced as the corries erode the mountain behind, the rest is weathered into a sharp point.