Explain features and processes at conservative plate boundaries
Explain features and processes at convergent plate boundaries
Explain feature and processes at divergent plate boundaries
explain the formation of headlands and bays
formed on discordant coastline
weaker lithology rock is eroded much more easily forming a bay and the stronger lithology rock still sticking out is a headland
give me an example of a headland and bay
flamborough head and filey bay
explain the formation of cliffs and shore platforms
hydralic action undercuts a cliff along a concordant coastline between high and low tides. weakening strata eventually causing mass movement due to gravity and leads to cliff retreat over long period of time with a platform exposed at low tide.
give me an example of a shore platform
robin hood bay
explain formation of geos
long inlet into a cliff. caused by lines of weakness on a concordant coastline edroded via hydralic action but also can be caused when tunnel like caves have a roof collaspe
name an example of a geo
huntsman leap in pembrokeshire which is 35m deep and has a geology of limestone
explain formation of blowholes
similar to geos blowholes are caused from the collapse of a cave roof, either eroded from hydraulic action due to a fault in structure creating a large hole in the cliff side which during storm events or high energy waves cause sprays of water through the top
give me an example of a blowhole
trevone blowhole in cornwall which is 25m deep
explain the formation of a cave,arch,stack and stump
discordant as hydraulic action erodes rock of a headland starting from a fault in the structure forming a cave. this continues until its eroded through a headland forming an arch such as durdle door the top of the arch is then weathered and eventually collapses creating a stack then further erosion and weathering causes the top of the stack to collapse creating a stump.
give me an example of a cave, stack, stump and arch
old harrys rocks and durdle door
explain the formation of a beach
give me an example of a beach
cornwall and dorset such as chesil beach
explain the formation of spits
longshore drift follows the direction of the dominant prevailing wind transporting sediment outwards to sea creating a pennisula of sediment depositied once the cosltine changes direction which causes a loss of energy which is why sediment is deposited
is fast during storm events due to more powerful gusts so smore sediment transported along the coastline
give me an example of a spit
sandbanks
explain the formation of an onshore bar
when a spit continues to grow across an indentation such as a cove or bay until it reaches the land on the other end forming a lagoon behind it
give me an example of a onshore bar
slapton sands in devon which is 100m wide and made of shingle
explain the formation of a tombolo
when spits continue and join with an island connecting it to the mainland. typically causes by onshore movement as well as continued deposition until it reaches land
give an example of a tombolo
chesil beach in dorset which is 30km long
explain the formation of a salt marsh
its a feature of a spit caused by low energy environments which are vegetated by salt tolerant species which are exposed and flooded daily by the tides. plants help with keeping sediment trapped. the higher the marsh the lower the saline content and the shorter the period of submergence deposition is usually 10cm per year
give an example of a salt marsh
flookbrugh in cumbria