2 - Extreme environments processes & terminology Flashcards
(22 cards)
Glacial erosion
Processes like plucking and abrasion that shape glacial landscapes.
Glacial transport and deposition
Movement and dropping of sediment by glaciers.
Cirques/Corries
Bowl-shaped hollows formed by glacial erosion at the head of a valley.
Pyramidal peaks/Horns
Sharp mountain peaks formed by erosion from multiple glaciers.
Arêtes
Narrow ridges between two cirques or glacial valleys.
Glacial troughs
U-shaped valleys formed by glacial erosion.
Moraines (lateral, medial, terminal)
Accumulations of debris deposited by glaciers.
Erratics
Large boulders transported and deposited by glaciers far from their origin.
Freeze-thaw weathering
Water freezes in cracks, expands, and breaks the rock apart.
Solifluction
Slow downhill flow of saturated soil in periglacial areas.
Frost heave
Expansion of frozen water beneath the surface pushes soil and rocks upward.
Permafrost
Ground that remains frozen year-round.
Thermokarst
Uneven ground caused by melting permafrost.
Patterned ground
Surface patterns (e.g., polygons or circles) formed by freeze-thaw cycles.
Pingos
Ice-cored hills formed in permafrost regions by freezing groundwater.
Physical weathering (hot environments)
Breakdown of rock by temperature changes (e.g., insolation weathering).
Chemical weathering (hot environments)
Breakdown of rocks by chemical reactions (e.g., oxidation).
Erosion by wind and water
Wind deflation/abrasion and water-based erosion common in deserts.
Desert landscape features
Dunes, wadis, rock pedestals, mesas, and buttes shaped by erosion and deposition.
What is plucking in glacial erosion?
Glacier freezes onto rocks and pulls them away as it moves, removing chunks of bedrock.
What is abrasion in glacial erosion?
Rocks and debris embedded in the glacier scrape against the bedrock, wearing it down and creating striations.
What is freeze-thaw weathering?
Water enters cracks in rock, freezes, expands, and breaks the rock apart; prepares debris for glacial erosion.