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
How do headlands and bays continue to change over time
- wave refraction round headlands
- caves arches stacks and stumps can form
- waves lose energy due to wave refraction and deposit sediment in bay= beach
- bay can become wider as headland erodes
What is wave refraction
1- shallow water in front of headland (wave cut platform) slows a part of the wave down
2- rest of the wave bends and breaks round the headland = erodes headland from side
How do cliffs retreat and form
1- erosion at base of cliff between high + low tides = wave cut notch
2- undercutting/ continued erosion at base causes cliff to collapse
3- collapsed material = wave cut platform
4- cycle starts again and cliff retreats
How do caves , arches , stacks and stumps form
1- wave refraction on WCP slows down waves directly infront of headland while waves either side bend round + attack cliff from side
2- crack forms = then cave = then arch and so on
How do blowholes form
1- waves erode cave in headland
2- structure + bedding planes of rock allow vertical erosion as well as lateral
3- tunnel forms allowing water to flow through cave and out of the top
What is a Geo
1- erosion enlarges a fault to form a cave
2- continued erosion causes roof to collapse = narrow steep-sided inlet called a geo
What is mass movement + give 3 examples
Movement of material due to gravity
- rock fall
- landslides
- slumping
Rock fall
- rocks detached by weathering fall due to gravity
Landslides
- sliding of rock along crack or fault
What is slumping
- Saturated material becomes heavy + lubricated = collapses along curved line
What is a beach + name 2 features found on a beach
- accumulation of material deposited
-berms + cusps
What are berms and cusps
- ridges formed at high tide mark as sediment is deposited at top of swash
-small depressions formed as backwash is channeled down beach
What are spits + how do they form
- long extended beaches attached to land at one end + stretch into sea at other
- longshore drift carries material along coast = sediment grows out from coast
- change in wind direction builds sediment in another direction = recurved end
Onshore bars
- a spit that connects 2 areas of land eg: across a bay
- salt marshes form behind
What is a tombolo
- wave refraction around island = waves lose energy + deposit sediment
- beach forms connecting island to mainland
What are salt marshes
- vegetated areas of deposition in low energy conditions
- submerged at high tide + exposed at low
How much does limestone erode per year
0.1m a year
How much does clay erode a year
0.8m a year
what angle do waves arrive at coast for LSD
45.c
Spit
long narrow beach of sand or shingle, attached to land at one end and stretch out across a bay, estuary or change in coastline.
Formed as LSD carries sediment into sheltered areas of open water
Onshore bars
Formed when a spit continues to grow across a bay or indentation.
Lagoons of brackish water are formed behind them.
Longshore drift
Process of sediment transportation across a beach. Dependent on the prevailing wind.
Sediment is transported with swash at a 45 degree angle up the beach and 90 degree angle back to the sea with backwash