Coasts Landforms Flashcards
Formation of caves, arches stacks and stumps
-hydraulic action and abrasion form cracks in the headland to creat small caves
-the rock above may collapse
-marine erosion widens the fault
-falls through marine erosion and sub aerial processes through to other side creating arch
-continues to widen until it can’t support itself and falls through mass movement
-leaves a stack
-marine erosion attacking base will become stump
Formation of wave cut notch to a platform
-waves erode cliff through hydraulic action at the high tide line
-this creates a wave cut notch
-notch becomes deeper as subaerial weathering weakens top cliff
-become unstable and falls under its own weight through mass movement
-leaves behind a wave cut platform
Depositional landforms
Beach
Spits
Tombolo
Barrier beach
Offshore bar
Formation of beach
Accretion of sediment during constructive waves in summer months
Dependent on angle of prevailing wind in relation to the land
Swash aligned beaches
Wave approaches perpendicular to coast so limits longshore drift
Wave refraction may reduce speed of high energy waves
Drift aligned beaches
Waves approach at an angle so LSD moves sediment far along the beach
May lead to formation of a spit
Formation of spit
When long shore drift causes beach to extend out to sea by a change in direction of the coastline
Can create salt marsh in its sheltered environment
Length depends on amount of rivers
Change in wind direction will curve the spit
Formation of barrier beach
When a beach or spit extends across a bat to join two headlands
Traps water behind makes a lagoon
May form due to rising sea levels after last glacial period
If becomes separated it will become a barrier island
Formation of offshore bars
An offshore region where sand is deposited when waves lose energy to carry sediment to the shore
May form when wave breaks early
Waves may pick this up (input to coastal zone)
May absorb wave energy
Landforms erosion
Caves arches stacks stumps
Headlands and bays
Wave cut notches and platforms
2 types of physical weathering
Freeze thaw
Sly crystallisation
2 types of chemical weathering
Oxidation
Carbonation
2 types of biological weathering
Plant roots
Decaying vegetation
Explain carbonation
Rainwater absorbs CO2 from atmosphere
Creates weak carbonic. Acids
Reacts with calcium carbonate in rocks
Forms calcium bicarbonate
Easily dissolves
Explain oxidation
Minerals exposed to air through cracks in rock
Oxidised and increase in volume
Esters pressure on rock and it crumbles