coastal zone keywords

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(the coastal zone) geography Fichas sobre coastal zone keywords, creado por kat1jj el 10/04/2013.
kat1jj
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kat1jj
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intertidal- high tide covered by water, low tide- exposed land sub-tidal- always covered by water
backshore- never covered by water how are waves formed? By the wind blowing over a sea. it is basically the formation of ripples on the surface.
what determines the wave size? the distance the wave travels and the strength of the wind. (THE FETCH) the wind generates a ripple that gets bigger over distance.(fetch)
SWASH= water runs up the beach/ shore BACKWASH=water returns to sea. why do waves break? FRICTION reduces speed of the bottom section.
constructive wave- smaller in height= less energy strong swash- pushes material up the beach. weak back wash- little erosion.
destructive waves- very tall- a lot of energy weak swash- little beach building strong backwash- pulls sand/shingle down beach= starves beach
air gets forced into rocks from the water (strong waves) rocks eventually - explode/break/fall off constructive waves go further and have more power, stronger swash. they create a big and flat shaped beach.
EROSION hydraulic power- the sheer power of waves abrasion- sand paper effect EROSION attrition- the knocking together of pebbles, making them gradually smaller and smoother. eventually turns to sand. solution- dissolving of rocks e.g chalk
weathering PHYSICAL- water freezes in cracks, the ice expands, rock shatters. CHEMICAL- weak acid in rain, dissolves limestone+chalk weathering BIOLOGICAL- roots of plants crack rocks in the cliff face as they grow. weakens cliff face. nesting birds. SALT WEATHERING-salt crystals from when sea dries, rock crumbles/ diintergrates.
mass movement- a movement of material down slope factors for mass movement- heavy rain- adds weight to cliff/ reduces friction tectonic movement- e.g. earthquake weathering processes slope angle/ gradient, steepness of cliff
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