coasts eq2 Flashcards
what are waves caused by?
friction between wind and water, with some energy being transferred into the water.
Waves depend on a number of factors:
- the strength of the wind
- Water depth
- the duration the wind has been blowing
- the distance of sea it has travelled over (the fetch)
Where in the UK do we experience the largest waves?
Cornwall because the prevailing wind is from the South west and the fetch from Florida to Cornwall is 4000 km.
How do waves form?
by the wind blowing across the surface of the water. Initially, the blowing wind will create ripples and these will then turn into waves. As waves reach the coast the lower part of the wave will slow down due to friction. The upper part of the wave then falls forward and breaks onto the beach
Why do waves break at the shoreline?
- the crest of the wave begins to move forward much faster than the wave trough.
- The trough experiences friction with the sediment on the sea bed and therefore slows even more.
- Eventually the crest outruns the trough and the waves topples.
marine processes
those associated with the action of waves. This includes erosion, transportation and deposition.
erosion
Erosion refers to the wearing away of the land surface and removal of materials by river and seawater, ice and wind. There are four main processes of erosion along the coast. These are hydraulic action, abrasion and attrition and solution ( Corrosion).
What does geomorphic mean?
Relates to the formation and shaping of landforms and landscapes by natural processes such as weathering, mass movement transportation and erosion
weathering
The breakdown or disintegration of
rock in situ ( its original place). As a process, weathering leads to the transfer (flow) of material.
mass movement
The downhill movement of material under the influence of gravity.
coastal sediment or littoral cell
system by which sediment is sourced, transported and deposited within a part of the coast.
They appear as a coastal system because sediments are derived from estuaries and coastal erosion, transported by longshore drift and deposited in the form of beaches, bars and spits etc.
sources
places where sediment is generated.
transfer zones
places where sediment is moving along the shore
sinks
locations where the dominant process is deposition
dynamic equilibrrium
Under natural conditions the systems operate in a state of dynamic equilibrium with sediment inputs balancing outputs to sinks.