2a- How Coastal Landscapes Develop Flashcards
Abrasion
- sediment carried by waves rub away coastline
Wave pounding
- force of breaking waves on coastline
Hydraulic action
- water pushed into cracks + compressing air = high pressure = widens the crack
3 definitions of Solution
Erosion= dissolving alkaline rock in acidic seawater
Transport= transport of dissolved sediment in water
Weathering= soluable rock minerals dissolve in rain water
Attrition
When sediment bumps into each other becoming smoother + rounder
Suspension
- floating small sediment carried by water
Saltation
-sediment bouncing along sea bed = too heavy to be suspended
Traction
- larger sediment pushes or rolled along sea bed
Flocculation
- fresh and salt water mixing allowing small particles to clump together until too heavy to be carried + are deposited
Freeze thaw
- water enters cracks and freezes expanding = widens crack
Salt crystallisation
- sea water evaporates leaving behind crystals in cracks = as crystals grow they put pressure on rock
Pressure release
- rocks above eroded = decrease in weight/pressure above so rock expands
(like releasing belt and stomach goes out)
Carbonation
- CO2 in rain makes it slightly acidic = reacts with some rocks + dissolves them
Biological weathering (2 types)
Physical = burrowing animals or tree roots push in rock causing rock to split
Chemical= organic acids produced reacting with rock minerals
How do headlands and bays form
1- disconcordant coastline = different speeds of erosion
2- bay forms in area of weaker geology and headland forms in area of strong geology