Sediment Transportation Flashcards
Longshore drift
LD transports material along coastlines when waves approach the beach at an angle
Swash direction
Wind approaches the coast at an angle because of a prevailing wind direction
Waves are controlled by the wind + so this angle will be the direction the swash moves up the beach
Backwash direction
Gravity = only force that acts on the backwash so it falls back to the sea at right angles to the coastline
Overall effect
Because of the difference b/ the angle of swash + angle of backwash sediment repeatedly moves in the shape of a rught angled triangle
Over time sediment is carried along a beach
Depositional landforms
Coastal landforms caused by deposition include beaches, spits, bars, tombolos, cuspate forelands
Spits
Coast changes direction at an estuary (river meets sea) longshore drift continues to move sediment across the inlet
River doesn’t let the spit completely join the coast on the other side because the river has the energy to move the sediment
Spits = long fingers of sand sticking out from 1 side in a coastline that have been curved by secondary winds. Often have salt marshes behind them.
Bars
Bar is formed when a spit grows across a bay
Lagoons often form behind bars
Beaches
Are made by constructive waves moving + depositing sand/shingle inland
Generally a more gently sloping beach tends 2 be formed from sand whereas a steeper sloping beach is formed from pebbles
Tombolos
If a spit stretches across the mainland + joins an offshore island this causes the formation of a tombolo
Cuspate forelands
Form when sediment is deposited across a bag caused by longshore drift transporting sediment in 2 directions
Leads to the formation of 2 spits which eventually meet + results in the trapping of sediment until eventually new land is formed
Sediment cell concept
Describes a closed system operated by sources, transfer, sinks driven by erosion, transportation, deposition processes
Sources
Sources are subaerial processes, erosional processes (breaking down cliffs) + sediment brought to the coastline by rivers
Transfers
Transfers are longshore drift, onshore, offshore winds + tides
Sinks
Sinks are depositional landforms (spits, bars, beaches, sand dunes)
Uk
Has 11 key sediment cells + sub-cells each with its own shoreline management plan