2B.3 Rates of Coastal Recession Flashcards
lithology, rock strata and vegetation
name the three rock types
igneous
metamorphic
sedimentary
igneous rock
e.g. granite, basalt, dolerite
-interlocking crystals cause erosion rate to be very slow
-granite has few joints, limiting weaknesses available for erosion to exploit
metamorphic rock
e.g. slate, marble
-crystalline rocks are resistant to erosion
-some have a feature with the same direction crystals, causing weaknesses
-folded and heavily fractured for erosion to exploit rocks, erosion is slow
sedimentary rock
e.g. sandstone, shale, chalk and limestone
-erodes faster than others
-younger rocks are weaker
-bedding planes and fractures create vulnerability to erosion
what is the weakest coastal material
unconsolidated sediment
what factor of rocks influences cliff profiles
PERMEABILITY
permeable rocks
allow water to flow through e.g. sandstone and limestone
impermeable rocks
do not allow groundwater flow e.g. clays, mudstones
how can impermeable rocks become weak?
groundwater flow weakens rocks as it removes cement that binds sediment together in the rock
-also it creates a high pore water pressure, making the rock heavy, affecting its stability
describe a dalmation coastline
-concordant coastline
formed due to a rise in seal level, the tops of ridges can be seen above sea level which creates a series of offshore, long, thin islands
describe a haff coastline
-concordant coastline
it is enclosed by low lying sandy spits or dunes which are aligned parallel to the coast
-longshore drift occurs
describe a fjord
-discordant coastline
formed when deep glacial troughs flood by rising sea levels, cutting deep valleys perpendicular to the coastline, they are very deep
-found in Norway and west Iceland
describe a ria
-discordant coastline
these are drowned river valleys which are sheltered winding inlets formed by rising sea level, they are narrow and form natural harbours at the coast
e.g. Falmouth is the deepest natural harbour in the UK
what vegetation is found on a haff coastline?
marram grass
marram grass adaptations and features
it is a common type of grass that has a waxy, hard coating
-durable to winds and storms
-rounded tube shape to retain moisture
-deep roots to access more water
-wide roots for stability and reaching minerals and water
-halophyte plant with salt spray
stability
the protection of coastlines by vegetation such as sand dunes and salt marshes
succession
the changing nature of a plant community over time as an area is colonised
psammorsene
the succession of plants that develop on a sand dune complex
flocculation
the process by which river’s load of clay and silts carried in suspension is deposited more easily as it meets with sea water (salt)
halosene
the succession of plants that develop in a salt marsh
how do sand dunes play a role in the coast
it protects the coastal landscape from erosion by stablising plants
-they are important buffer zones between the sea and land, they take the impact of storms, reducing the impact on the land
describe how vegetation stabilises coastal deposition features
- plant roots bind sediment together, reducing erosion
- when submerged, plants provide a protective layer so the surface of sediment is not directly exposed to moving water (salt marshes)
- plants protect sediment form wind erosion, reducing speed at the surface with friction against the vegetation
how are halophytes salt tolerant?
they store water in special tissue with air spaces
-some excrete salt through glands or by dropping yellow leaves where salt has been accumulated
-they retain water- succulents
how are xerophytes dry condition tolerant?
they have thick cuticles to stop uncontrolled evaporation, with a small leaf surface area too
-low stomata density
-sunken stomata maintains humid air
-stomatal hairs
-rolled leaves
-extensive roots maximise water uptake