Depositional - the waves leave material on the beach, and so build up the material (sand, pebbles, etc) over time
Destructive waves
Strong backwash, weak swash
High wave height, small wavelength
High frequency
Erosional - the waves erode the beach and any rocks and take the material away to other locations. Over time, the beach wears away
Factors affecting wave size
Strength of the wind
How long the wind has been blowing for
Water depth
Fetch - the distance the waves have travelled from where they originated from
Coastlines hit by constructive waves
Tend to have depositional landforms such as sandybeaches
Coastlines hit by destructive waves
Typically have erosionallandforms such as rockyheadlands and landforms, such as tall cliffs and caves
Coastal processes
Erosion
Weathering
Transportation
Mass movement
Deposition
Corrasion
Sand and pebbles are picked up by the sea and hurled against the cliffs at hightide, causing the cliffs to be eroded. The shape, weight and quantity of sediment picked up, as well as the wave speed, affects the rate of erosion
Abrasion
Sediment scrapes and bangs against the base of a rockface, and so wear away the face gradually (like sandpaper against a piece of wood)
Attrition
Wave action causes rocks and pebbles to hit against each other, wearing each other down and so becoming round and eventually smaller
Hydraulic action
As a wave crashes onto a rock or cliff face, air is forced into cracks within the rock. The high pressure causes the cracks to force apart and widen when the wave retreats and the air expands. Over time this causes the rock to fracture
Corrosion (Solution)
The mildly acidic seawater can cause alkaline rock such as limestone to be eroded
Erosional landforms
Caves
Arches
Stacks
Stumps
Erosional landforms
Wave-cut notch
Wave-cut platform
Longshore drift
Sediment is transported along the coast through the process of longshore drift
Longshore drift
1. Waves hit the beach at an angle determined by the direction of the prevailing wind
2. The waves push sediment in the direction of the prevailing wind up the beach in the swash
3. Due to gravity, the wave then carries sediment back down the beach in the backwash
4. This moves sediment along the beach over time
Deposition
Occurs when a wave loses energy meaning the sediment becomes too heavy to carry
Depositional landforms
Beaches
Spits
Bars
Sand dunes
Berm
Ridges where high tide reaches and deposits a ridge of sand and materials (seaweed, driftwood, etc)
Spit
A long narrow strip of land which is formed due to deposition. Longshore drift occurs along the coastline but as the waves lose energy (normally due to going into a sheltered area such as behind a headland) they deposit their sediment. Over time this creates a spit
Bar
Bars can form from spits, but only in certain locations. A bar is a spit that has grownacross the mouth of a bay. This cuts off the sea water from the bay, creating a lagoon with still water and over time this will become a freshwater lake
Sand dunes
Occur when prevailing winds blow sediment to the back of the beach. There are different types of sand dunes, the name they're given depends on their stage of development and position on the beach
Embryo dunes are found in the upper beach area where sand starts to accumulate around a small obstacle (driftwood, wooden peg, ridge of shingle)
Yellow dunes are formed as more sand accumulates and the dunes become more vegetated
Bar
Forms from spits, but only in certain locations
A spit that has grown across the mouth of a bay, cutting off the sea water and creating a lagoon which over time becomes a freshwater lake
Can also form between land and an island, known as a barrier beach
Sand Dunes
Occur when prevailing winds blow sediment to the back of the beach
Different types of sand dunes depending on their stage of development and position on the beach
Weathering
The breakdown of rocks over time, producing material which creates coastal landforms or sediment taken away through transportation
Types of weathering processes
Mechanical (Physical) Weathering
Chemical Weathering
Biological Weathering
Mechanical (Physical) Weathering
The breakdown of rocks due to exertion of physical forces without any chemical changes taking place
Freeze-thaw
Water enters cracks in rocks, then freezes overnight, expanding by 10% in volume which increases the pressure acting on the rock, causing cracks to develop over time
Chemical Weathering
The breakdown of rocks through chemical reactions, the most common type being carbonation where acidrain reacts with calciumcarbonate in rocks
Biological Weathering
The breakdown of rocks due to the actions of plants, bacteria and animals
Types of mass movement
Rockfalls
Landslides
Mudflow
RotationalSlip
Rock Fall
Occur on sloped cliffs (over 40 degrees to the beach floor) when the rock becomes exposed to mechanical weathering (often freeze thaw)
Landslide
Water betweensheets of rock (called bedding planes) and the rock face reduces friction and allows large chunks of rock to slide down the cliff
Mudflow
Saturated (waterlogged) soil flows down the face of a hill like a fluid, bulging at the bottom in a lobe
Rotational Slip
Also known as slumps, soil and rock fragments become saturated with water and slip, creating stepped 'heads' down the cliff face
Coastal management strategies
Hard engineering
Soft engineering
Managed retreat
Hard engineering
Uses man-made, artificial structures to reduce or halt erosion, often very effective but high cost and significant environmental impact
Soft engineering
Uses more natural materials to reduce erosion, in a more environmentally friendly way, aiming to complement the physical environment
Managed retreat
Allows erosion rates to carry on unchanged, monitoring the rate of erosion and putting ways of adapting to this erosion in place for the future