3.6 Weathering And Mass Movement At The Coast Flashcards
Sub-aerial processes
Weathering and mass movement.
Weathering
Gradual breakdown of rock. Divided into 3 categories: biological, chemical and mechanical. Can also increase rate of erosion
Mass movement
Movement of weathered material down slop as a result of gravity
Freeze-thaw weathering
Mechanical. Rain > water in crack freeze > ice expands > widens crack > cycle continues
Scree
Collection of loose rock found on sides of hills and mountains
Salt-weathering
Mechanical. Salt water evaporates > leaves salt crystals > grows time causing cracks > can also corrode rock
Wetting and drying
Mechanical. Rocks rich in clay expand when wet and contract when dry. Causes cracks and breaking
Biological weathering occurrences
Plant roots in rock widening. Water running through vegetation becomes acidic. Animals burrowing into rock. Marine organisms secreting acid (limpets)
Carbonation
Chemical weathering. Process of rock minerals reacting with carbonic acid. Dissolves minerals.
Mass movement factors
Slope of cliff.
Rock type and structure.
Vegetation cover.
Antecedent conditions.
Soil creep
Mass movement. Slowest form. Downhill movement of individual particles.
Solifluction
Mass movement. Occurs mainly in tundra areas, where ground is frozen. Top layer thaws, surface layer becomes saturated and flows over frozen subsoil.
Earth flows and mudflows
Increase in water amount reduces friction. Earth and mud flows over underlying bedrock
Rock falls
Occurs on slopes over 40⁰. Material, when broken, falls vertically.
Rock/debris slides
Slabs of rock sliding over a slide or slip plane. Increase in water reduces friction