Glacial Landforms Flashcards

1
Q

How do corries (cirques) form? (Give 5 facts)

A

• Nivation initially deepens a hollow.
• Rotational sliding increases abrasion, deepening the base.
• Plucking occurs at the back wall, forming a steep slope.
• A bergschrund (crevasse) forms, collecting debris that enhances erosion.
• Moraine deposition at the lip may form a tarn (corrie lake).

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2
Q

What are arêtes and pyramidal peaks?

A

• Arêtes: Narrow, steep ridges formed when two adjacent corries erode towards each other.
• Pyramidal Peaks: Sharp mountain peaks formed when three or more corries erode a single mountain (e.g., the Matterhorn).

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3
Q

What are glacial troughs and ribbon lakes?

A

• Glacial troughs (U-shaped valleys): Former V-shaped river valleys widened and deepened by glaciers.
• Ribbon lakes: Formed when glaciers over-deepen sections of valleys, which later fill with water.

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4
Q

What are hanging valleys? (Give 2 facts)

A

• Smaller tributary glaciers erode less deeply than the main glacier.
• After glaciation, the tributary valley is left hanging above the main valley, often with a waterfall.

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5
Q

What is a roche moutonnée? (Give 3 facts)

A

• Asymmetrical rock formations eroded by glaciers.
• Upstream side: Smooth, polished by abrasion.
• Downstream side: Jagged, plucked by the glacier.

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6
Q

What are crag and tail landforms?

A

• Crag: Resistant rock that protects softer rock from erosion.
• Tail: Depositional feature behind the crag (e.g., Edinburgh Castle on a crag and tail).

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7
Q

What are the 3(or 4) different types of moraines?

A

• Lateral Moraine: Forms along the edges of a glacier from debris falling off valley walls.
• Medial Moraine: Forms in the centre of a glacier when two glaciers merge.
• End Moraine (Terminal/Recessional): Forms at the glacier snout when ice melts and deposits sediment.

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8
Q

What are drumlins? (Give 3 facts)

A

• Oval-shaped hills of glacial till found in swarms (basket of eggs topography).
• Steep stoss end (facing ice movement) and gently sloping lee end.
• Exact formation is debated, but likely linked to ice deformation and sediment strength.

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9
Q

What is a till plain? (Give 2 facts)

A

• Extensive flat areas formed by glacial deposition.
• Composed of unsorted glacial till (boulders, clay, sand).

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10
Q

What are subglacial and ice-marginal landscapes?

A

• Subglacial: Formed under ice masses, dominated by erosion (e.g., glacial troughs).
• Ice-marginal: Formed at glacier edges, dominated by deposition (e.g., moraines).

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11
Q

What are proglacial and periglacial environments?

A

• Proglacial: Found in front of glaciers, where meltwater and wind action shape the landscape.
• Periglacial: Cold environments near but not under glaciers, featuring permafrost.

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12
Q

What are the three main scales of glacial landforms?

A

• Macro-scale: Large landforms (corries, glacial troughs, pyramidal peaks).
• Meso-scale: Medium landforms (drumlins, roches moutonnées).
• Micro-scale: Small features (striations, chattermarks, erratics).

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