coastal environments Flashcards
coral reef conditions
made of polyps, that photosynthesise. have high biodiversity
- less than 25m deep
- water temp of 27 degrees
- oxygen, low salinity
mangroves conditions
- temps more than 5 degrees, do better in consistent temps
- salt water
- can survive in waterlogged environments
- tropical and subtropical areas
- threats: pollution, deforestation, over fishing, climate change
sand dunes conditions
- wind to move sand
- obstacle to form around
- lots of sand
- constructive waves to deposit sand
- large tidal range so there’s time for the sand to dry
- can be found anywhere
- threats: pollution
salt marshes conditions
- halophytic plants develop fast
- succession on mudflats known as halorose
- low energy coasts, constructive waves which deposit silt
- vegetation slows waves to allow deposition
- threats: pollution, eutrophication, dredging
weathering
the gradual break down of rock in situ.
mechanical weathering
freeze thaw:
water collects in a rock crack and freezes and expands, forcing the crack to widen. the ice thaws and water goes deeper, repeating process. rock eventually splits
chemical weathering
break down of rocks due to reaction with materials around it
carbonation: slow dissolution of limestone due to rainfall
oxidation: addition of oxygen to compounds eg rusting
mass movement
movement of weathered material downslope as a result of gravity
types of mass movement
rock fall
slide
slump
topple
flow
rock fall
when rocks are broken into pieces and fall down a cliff, crumple on one another
sloped over 40 degrees
mechanical weathering
slide
increase in water reduces friction, slabs of rock slide over one another. material remains intact
slump
saturated solids ove harder rocks slide down a cliff, leaving ridges along the way
topple
undercutting by erosion causes the top heavy part of a cliff to fall
flow
increase water causes mud and silt to slide down over underlying bedrock, material jumbles up
discordant coastline
alternating soft and hard rock perpendicular to the coastline
concordant coastline
alternating soft and hard rock parallel to coastline
abrasion
rocks carried by water scrape and wear away surfaces like coastlines through friction
attrition
rocks and pebbles carried by the water collide, forcing them to break down into smaller, rounder pieces
solution
chemicals in the water dissolve and break down rocks
hydraulic action
water pushes air into cracks and crevices of rocks, forces them apart due to the high pressure
cliff formation
erosion of all kinds
weathering
wave cut platforms formation
erosion at base of cliff greatest, starts to form a notch
undercutting continues, eventually the overhanging cliff is too heavy and falls
this repeats overtime, making the cliff face retreat
as it retreats, a gently sloping platform is left at the base, exposed at low tide.
caves
large crack created by erosion (hydraulic action and solution), grows into cave by hydraulic action and abrasion
arches
a cave breaks through the other side of the headland due to erosion