Question | Answer |
Process | A series of actions with an end |
Abrasion | when moraine carried by a glacier rubs against the ice and like sandpaper wears away sides and floor of valley (smooth surface) |
Freeze-thaw weathering | constant freezing and expansion of cracks on mountains which fill with rainwater |
Plucking | when rocks on bedrock stick to the ice and get transported when the glacier moves away (jagged surface) |
Erosion | rock being worn away due to the weather and animals/plants |
Weathering | the breaking down of rocks by wind, rivers, sea & ice |
Transportation | the moving of rocks by wind, rivers,sea and ice (conveyor belt) |
Deposition | putting down rocks by wind, rivers, sea & ice |
Rotational slip | movement of glacier along a curve |
Landform | a natural feature of the earth |
Moraine | small rocks carried and transported by a glacier |
Corrie | deep armchair-shaped crater on a hillside (often with tarn) |
Arete | a knife-edged ridge often formed between two corries |
Pyramidal peak | a sharp-edge mountain peak (formed between three corries) |
Truncated spur | an eroded interlocking spur characterised by a cliff-like feature |
Glacial trough/U shaped valley | a wide steep-sided valley floor eroded by a glacier |
Ribbon lake | long narrow lake on a glacial trough |
Tarn | a lake in a corrie |
Hanging valley | a tributary glacial trough perched up on the side of a main valley (often marked by a waterfall) |
Boulder clay/till | type of glacial deposit where very small particles (clay) are mixed with larger ones (boulders) |
Sublimation | snow turn directly to water vapour |
Drumlin | small hill of moraine, thought to be shaped by a second glacier moving over it after original glacier that deposited it retreated |
Snout | end of glacier |
Firn | snow that has survived a summer |
Avalanche | rapid and large fall of snow and rock down a cliff |
Accumulation | snowfall and avalanche |
Ablation | snowmelt, calving, sublimation |
Serac | block of ice |
Glacier budget | balance between inputs & outputs |
Equilibrium line | point on a glacier |
System analysis | inputs, stores, outputs |
Calving | formation of icebergs |
Glacier retreat | when ablation is greater than accumulation |
Glacier advance | when accumulation is greater than advance |
Crevasse | giant crack in glacier's surface |
Glacier ice | compacted snow after 100s of years |
Freeze-thaw weathering | When water gets into rocks cracks and freezes when temperatures go below 0°C. The ice expands and the cracks wide n so pieces of rock eventually break off. |
Scree | pile of loose rocks - result of freeze-thaw weathering |
Quaternary - Pleistocene | the geological period between 2 million and 10 000 years ago |
Interglacial | a period of ice retreated associated with rising temperatures |
Glacier | a river of ice usually extending downhill from an ice cap and occupying a valley |
Ice age | a period when there are many glacial periods in a sequence quite close together. A time when ice sheets are found on continents. |
Ice sheet | a huge mass of ice over 50 000 km² in size |
Glacial period | a period of ice advance associated with falling temperatures |
Ice cap | a smaller body of ice usually found in mountainous regions |
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