Coasts Landforms Flashcards

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1
Q

Formation of caves, arches stacks and stumps

A

-hydraulic action and abrasion form cracks in the headland to creat small caves
-the rock above may collapse
-marine erosion widens the fault
-falls through marine erosion and sub aerial processes through to other side creating arch
-continues to widen until it can’t support itself and falls through mass movement
-leaves a stack
-marine erosion attacking base will become stump

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2
Q

Formation of wave cut notch to a platform

A

-waves erode cliff through hydraulic action at the high tide line
-this creates a wave cut notch
-notch becomes deeper as subaerial weathering weakens top cliff
-become unstable and falls under its own weight through mass movement
-leaves behind a wave cut platform

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3
Q

Depositional landforms

A

Beach
Spits
Tombolo
Barrier beach
Offshore bar

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4
Q

Formation of beach

A

Accretion of sediment during constructive waves in summer months
Dependent on angle of prevailing wind in relation to the land

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5
Q

Swash aligned beaches

A

Wave approaches perpendicular to coast so limits longshore drift
Wave refraction may reduce speed of high energy waves

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6
Q

Drift aligned beaches

A

Waves approach at an angle so LSD moves sediment far along the beach
May lead to formation of a spit

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7
Q

Formation of spit

A

When long shore drift causes beach to extend out to sea by a change in direction of the coastline
Can create salt marsh in its sheltered environment
Length depends on amount of rivers
Change in wind direction will curve the spit

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8
Q

Formation of barrier beach

A

When a beach or spit extends across a bat to join two headlands
Traps water behind makes a lagoon
May form due to rising sea levels after last glacial period
If becomes separated it will become a barrier island

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9
Q

Formation of offshore bars

A

An offshore region where sand is deposited when waves lose energy to carry sediment to the shore
May form when wave breaks early
Waves may pick this up (input to coastal zone)
May absorb wave energy

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10
Q

Landforms erosion

A

Caves arches stacks stumps
Headlands and bays
Wave cut notches and platforms

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11
Q

2 types of physical weathering

A

Freeze thaw
Sly crystallisation

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12
Q

2 types of chemical weathering

A

Oxidation
Carbonation

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13
Q

2 types of biological weathering

A

Plant roots
Decaying vegetation

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14
Q

Explain carbonation

A

Rainwater absorbs CO2 from atmosphere
Creates weak carbonic. Acids
Reacts with calcium carbonate in rocks
Forms calcium bicarbonate
Easily dissolves

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15
Q

Explain oxidation

A

Minerals exposed to air through cracks in rock
Oxidised and increase in volume
Esters pressure on rock and it crumbles

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16
Q

6 factors mass movement is dependent on

A

Weathering
Ground saturation
Vegetation
Cliff angle
Rock type
Rock structure

17
Q

Define deposition

A

Deposition occurs when the sediment becomes too heavy for the wave to carry or the wave loses energy

18
Q

Define erosion

A

Erosion involved the removal of sediment from a coastline

19
Q

Types of erosion

A

Corrosion
Abrasion
Attrition
Hydraulic action
Wave quarrying

20
Q

Factors effecting erosion

A

Waves
Beaches
Subaerial processes
Rock type/lithology

21
Q

4 process of transportation and deposition

A

Traction
Saltation
Suspension
Solution

22
Q

Explain long shore drift

A

Waves hit the beach at an angle determined by direction of prevailing wind
Pushes sediment up beach (swash)
Gravity waves carry sediment back down the beach (backwash)

23
Q

Flocculation

A

(Important in salt and tidal marshes)
Clay particles clump together due to chemical attraction and sink due to their high density

24
Q

What promotors steep cliff development

A

Absence of a beach
Long fetch
High wave energy
Sedimentary rocks vertical strata

25
Q

What promotes gentle cliffs

A

Low energy waves
Short fetch
Water rock

26
Q

Inputs of sand dunes

A

Supply of sand
Onshore winds
Large tidal range

27
Q

sand dune succession

A

Sand blown by onshore winds and trapped behind obstacle e.g driftwood
Embryo dunes are colonised by pioneer species
Long roots of marram grass help bind the ground together
Foredunes occur and become fixed forming an organic layer

28
Q

Development of mudflats

A

Develop in sheltered shorelines and low energy coasts
Composed of silt and clay at the bottom of estuaries submerged by high tide
Saltwater flows and river freshwater flows meet
Causes flocculations where the individual particles aggregate together

29
Q

Development of salt marshes from mudflats

A

Low lying vegetation like eelgrass begins to grow in mudflats
Slows currents and leads to more deposition
Pioneers begin to colonise known as halophytes - tolerant to salty conditions
E.g glasswort and spartina
Prisoners develop amc become closer, slow down currents and trap sediments