coasts - seneca Flashcards
what is the littoral zone
series of sub zones from the sea to land. we consider it a closed system
what are the four sub-zones in the littoral zones
offshore (open sea)
foreshore (land where most wave processes occur
backshore (area above high tide level that is only affected during exceptionally high tides.)
how does a system reach dynamic equilibrium
input=output
inputs of the littoral zone
sediment brought by waves, current and wind
outputs of the littoral zone
sediment washed out to sea by erosion
what are high energy coasts
destructive waves, long fetches, high erosion rates, caves, arches, stacks and stumps, cliffs and wave cut platforms
what are low energy coasts
constructive waves, shorter fetches, high deposition rates, spits and bars, beaches, sand dunes and salt marshes
how ma sediment ells are there in england & wales?
11
what are the sources of sediment cells
where sediment comes from (cliffs, offshore bars)
what are the flows in a sediment cells
movement of sediment in LSD
what are the sinks in sediment cells
where sediment is deposited (spits, beaches)
what is a positive feedback loop
takes system away from dynamic equilibrium
what is a negative feedback loop
returning a system back to equilibrium
negative feedback loop - a storm increases input of sediment to beach
- When the destructive waves from the storm lose their energy excess sediment is deposited
as an offshore bar. - The bar dissipates the waves energy which protects the beach from further erosion.
- Over time the bar gets eroded instead of the beach.
- Once the bar has gone normal conditions ensue and the system goes back to dynamic
equilibrium.
positive feedback loop - a storm increases input of sediment to beach
People walking over sand dunes destroys vegetation growing there and causes erosion.
- As the roots from the vegetation have been holding the sand dunes together, damaging the vegetation makes the sand dunes more susceptible to erosion. This increases the rate of
erosion.
- Eventually the sand dunes will be completely eroded leaving more of the beach open to
erosion taking the beach further away from dynamic equilibrium.
Valentine’s Classification
describes the range of coastlines that can occur
An advancing coastline may be due to the land emerging or deposition being the prominent
process. Alternatively, a coastline may be retreating due to the land submerging or erosion
becoming the prominent process.
Emergent or submergent coastlines may be due to post-glacial adjustment (the land ‘wobbles’ as
the glacier above it melts, causing isostatic sea level change), as well as other causes (discussed
later).
concordant coast
parallel bands to coast