Lesson 8-What are the erosional landforms at the coast? Flashcards
Concordant coastlines
- Lines of rock parallel with coastline; uniform erosion. Less dramatic, fewer features as the same band of rock will follow the shape of the coastline> Culworth Cove
Discordant coastline
- Lines of rock perpandicular to coastlines, irregular erosion; formation of headlands and bays.
How are headlands eroded?
- Wave refraction
-Headlands have a shallow depth around them that make waves slow down due to friction with the sea bed
-wave energy concentrates on the headland
Erosional landforms?
- Blowhole
- Geos
- Stacks
Erosional landforms-Blowhole
- Hole in the tpop of a cave created whren a sea cove grows inland and upwards through vertical erosion
- As air flows into the cove air is expelled through the pipe like joing casusing a blast of air
-e.g Portland in Dorset
Erosional landforms-Geos
- Is an inlet, a gully or a cliff
- Created by the erosion of cliffs along faults and bedding planes in the rock
-geos are common on the coastline of the Scotland and Orkney Islands in Norway
Erosional landforms-Stacks
1) Geological weakness
2) Formation of sea cove by erosion
3) Enlargementof cove to form and an arch to form a stack
4) Collapses to form a stack
5) Removal of stack to create a stump
What are cliffs?
- Landforms shaped through a combination of erosion, weathering and mass movement
Factors affecting cliffs
- Weathering
- Erosion from waves
- Mass movement
Factors affecting cliffs-Weathering
- Biological weathering attacks the cliff top, can also weaken them
Factors affecting cliffs-Erosion from waves
- Erosion aqttacks the foot, causing a wave-cut notch at the bottom particularly where waves break in a similar pattern
-the tidal range
Factors affecting cliffs-Mass movement
- Affects the shape of the cliff as more mass movement will create a steeper gradient
Factors affecting cliff erosion?
- Geology
- No beach-
- Energy of environment
- Angle of rock layers- if vertical then its more steep
Lithology of the coast
- Strata
- Bedding planes
- Joints
- Folds
- Faults
- Dip
Strata
- Layers of rock
Bedding planes
Horizontal natural breaks in the strata- caused by gaps in time changing periods of rock formation
Joints
Vertical fractures caused either by contraction as sediments dry out or by earth movements causing uplift
Faults
- Formed when the stress or pressure to which a rock is subjected to exceeds its internal strength
-The faults then slip or move along fault planes
Dip
- Refers to the angle at which rock strata lie (horizontally, vertically, dipping towards the sea or dipping inland)
What are wave cut platforms?
- Marine erosion between the high tide and low tide mark by abrasion and hydraulic action forms a wave-cut notch along the length of the cliff base with a maximum width of 0.5km
-usually occurs when there is a low tidal range as it constantly eroding the same area and when waves break at the foot of the cliff
Wave cut platforms a positive or negative feedback loop?
- Negative feedback loop as a wave will break earlier and its energy will be dissipated before it reaches the cliff, thus reducing the rate of erosion, limiting the further growth of the platform
-at flamborough head there are wave-cut platforms
Why is erosion the more dominant process rather than deposition at the Holderness ?
Due to geology>boulder clay
Due to weather>weathering leads to more mass movement
Due to waves>quite a large fetch from the North Sea