Geography Flashcards
(17 cards)
Coastal processes are divided into two parts
Marine processes: offshore (water-based)
Terrestrial processes: onshore (land-based)
5 types of coastal processes
Wave action, erosion, weathering, transportation, mass movement
Properties of constructive waves
Strong swash
Weak backwash
Long wavelength
Low wave height
Low frequency (6-8 waves a minute)
Cause gently sloping beaches
Properties of destructive waves
Weak swash
Strong backwash
Short wavelength
High wave height
High frequency (10-12 a minute)
Cause steep beaches
4 methods of erosion
Hydraulic action: Sheerforce of the waves hitting the coast
Attrition: Material carried in the waves bumps against each other and becomes
smaller and smoother
Corrosion: Seawater is slightly acidic and gradually dissolves some types of coastal rock
Abrasion: Waves pick up material and hurl it at the coast
4 methods of transportation
Traction: Large heavy material is dragged along the sea floor
Saltation: Smaller material bounces along the sea floor
Suspension: Fine material held in the water
Solution: Dissolved material carried in the water
Process of longshore drift
Longshore drift is the main process of deposition and transportation along the coast. The prevailing wind pushes the waves at an angle to the beach. As the waves break, the swash carries material up the beach at the same angle. The backwash then carries the material down the beach at right angles (90°). The process repeats, transporting material along the beach in a zig-zag movement.
4 methods of deposition
.Wave energy decreases
.There is increased friction between the water and the seabed
.Large amounts of sediment are being carried by the water
.The water encounters obstacles causing the waves to break
3 types of weathering
Mechanical
Chemical
Biological
Mechanical weathering
Weathering physically breaks up rock:
Describe the process of freeze-thaw
Water gets into cracks and joints in the rock. When the water freezes it expands and the cracks open a little wider. Overtime, pieces of rock split off the rock face, whilst big boulders are broken into smaller rocks and gravel. This process is mechanical.
Chemical weathering
Occurs when rocks are broken down by a chemical process:
Biological weathering
Takes place when rocks are worn away by living organisms
Mass movement
The downhill movement of material under the influence of gravity. Throughflow and overland flow caused by heavy rain can also make cliffs more unstable and increase the likelihood of mass movement. It includes landslides, slumping and rockfalls.
Soil creep
Speed is below 1cm per year
Common in humid climates
When soil expands, individual particles are lifted up perpendicular to the slope
Soil also expands when itfreezes, gets wet or is heated up in the sun
When the soil shrinks again,the particles fall straight back down
Soil creep takes a long time because the soil moves only a millimetre to a few centimetres at a time
Flow
It occurs on slopes between 5° and 15°, usually after the soil has become saturated with a flow of water across the surface. Vegetation can be flattened and carried away with the soil
Speeds range from 1to 15km per year