a source of energy for coastal erosion and sediment transportation
created by thermal energy which creates kinetic energy
outline how waves influence coastal landscapes
transports and deposits sediment
creates energy for erosion
generated by frictional drag of wind over the water surface.
energy and size of a wave depends on...
wind strength
wind duration
water depth = how much energy is put into the wave
fetch (distance) of the wave
describe the process of wave propagation
ALWAYS SAY a wave propagates instead of forms
a wave propagates in the deep ocean and moves towards the shore
as the wave propagates out of the area it was generated, it becomes a swell wave
when the wave base hits the sea floor, it breaks and becomes a translatory wave
define swell wave
smooth ocean wave that travels a distance from its area of generation
define translatory wave
transfers both water and energy
define constructive wave
AKA spilling breaker
builds the beach
stronger swash than backwash
finer sand and flat beach
define destructive wave
AKA plungingbreaker
removes sediment
stronger backwash
when the energy increases = marine erosion accelerates:
creates steeper beach bc wave can travel further before it loses energy and deposits sediment.
coarse sediment bc waves can transfer more and larger sediment.
formula for calculating: amount of energy in a wave in deep water
P = H²T
outline how tides influence coastal landscapes
cyclical pattern = most coasts have 2 high and 2 low tides per day, approximately every 6 hours and 13 mins.
tidal patterns created by variation in gravitational pull of sun and moon on ocean surface = as the moon orbits the earth, it alters the tidal range.
define tidal range
the difference between a high and low tide
define spring tide
when the gravitational pull of the sun and mooncombines = creates an extreme tidal range. for example the highest high and lowest low.
define neap tide
when the gravitational pull go the sun and moon are opposite = creates a small tidal range.
define lithology
the composition of rock and its resistance to weathering and erosion
outline SEDIMENTARY rock - types of geology
example = sandstone and limestone
forms under the ocean from deadanimals by consolidation of sediment layers under heat and pressure.
porous = the least resistant to erosion
outline IGNEOUS rock - types of geology
example = granite and basalt
forms under extreme heat and pressure which removes imperfections = increases resistance.
created by crystallisation = solidification of magma
outline METAMORPHIC rock - types of geology
example = slate
forms under extreme heat and pressure which removes imperfections = increases resistance.
created by recrystallisation in solid state of new minerals.
most resistant to erosion
outline how geological structure influences coastal landscapes
it influences the rate of erosion = cliffs made from strata with different resistances
responsible for concordant and discordant coasts
define folds - geological structure
formed by layers of rock being bent and folded, created by pressure of tectonic forces
define joints - geological structure
fractures in rocks where no displacement has occurred
define faults - geological structure
large scale fractures and displacements created between 2 blocks of rocks, created by tectonic forces, which allows them to move relative to each other
define concordant coasts - geology
forms where rock strata runs parallel to coast
define discordant coasts - geology
forms where rock strata is aligned at an angle to coastline = forming headlands and bays
define vertical dip (cliff) - geology
rock strata angled vertically
erosion type = wave cut notches + weathering and mass movement of jointed strata
define seaward dip (cliff) - geology
rock strata angled downwards diagonally towards the sea
vulnerable to rockfalling
frequent mass movement and landslides of cliff collapse due to marine undercutting.
define landward dip (cliff) - geology
rock strata angled downwards diagonally towards the land
creates a steep profile with few rockfalls
outline surface ocean currents - ocean currents
caused mainly by wind and weather patterns
defined mainly by atmospheric circulation
influenced by gravitational tides
outline deep ocean currents - ocean currents
caused by changes in water density
cold water freezes and concentrates salt
downwelling occurs = saline water sinks = occurs at poles
deep ocean currents move towards equator
upwelling occurs = cold water moves to surface = occurs at tropics
warm surface = more circulation, waves, evaporation