coastal processes Flashcards
formation of a wave
wind moves across the water surface creating small ripples via frictional drag. Towards the coastline, the seabed gets shallower and the water particles become more elliptical causing wave height to increase. Water backs up behind the wave until it breaks and surges onto the beach
factors affecting the size and energy of a wave
duration of wind
strength of wind
size of fetch
what are the two wave types
constructive and destructive
features of a constructive wave:
long wave length
strong swash
weak backwash
forming a gentle sloped beach
features of a destructive wave:
short wave length
weak swash
strong backwash
forming a steep sloped beach
what is wave refraction?
where waves turn and loose energy around a headland or uneven coastline. Energy is then concentrated on the headland creating erosional landforms. energy dissipates in bays leading to depositional landforms
6 types of marine erosion:
hydraulic action
cavitation
corrasion
abrasion
solution
attrition
define hydraulic action
water pressure breaks down sediment
define cavitation
compression of air in joints as waves crash against cliffs causing sea water to be compressed, forcing rock apart
define corrasion
a type of chemical erosion breaking down the rocks
define abrasion
rocks erode by being thrown against cliffs etc
define solution
when sea water dissolves certain types of rocks
define attrition
when material carried by waves hit and knock against each other
what are sub-aerial processes
weathering and mass movement
define mass movement
material moving downslope via force of gravity
define weathering
the break down of rocks in situ
methods of marine transportation
traction
saltation
suspension
solution
longshore drift
define traction
roll along the sea bed
define saltation
bounce along the sea bed
define suspension
carried in the flow of water
what is longshore drift
when waves hit a beach at an angle due to prevailing wind direction, pushing sediment this way up the beach
what are sediment cells
coastlines split into sections usually by prominent headlands. Within these is dynamic equilibrium is achieved as the movement of sediment is contained