2a- How Coastal Landscapes Develop Flashcards

1
Q

Abrasion

A
  • sediment carried by waves rub away coastline
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2
Q

Wave pounding

A
  • force of breaking waves on coastline
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3
Q

Hydraulic action

A
  • water pushed into cracks + compressing air = high pressure = widens the crack
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4
Q

3 definitions of Solution

A

Erosion= dissolving alkaline rock in acidic seawater
Transport= transport of dissolved sediment in water
Weathering= soluable rock minerals dissolve in rain water

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5
Q

Attrition

A

When sediment bumps into each other becoming smoother + rounder

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6
Q

Suspension

A
  • floating small sediment carried by water
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7
Q

Saltation

A

-sediment bouncing along sea bed = too heavy to be suspended

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8
Q

Traction

A
  • larger sediment pushes or rolled along sea bed
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9
Q

Flocculation

A
  • fresh and salt water mixing allowing small particles to clump together until too heavy to be carried + are deposited
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10
Q

Freeze thaw

A
  • water enters cracks and freezes expanding = widens crack
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11
Q

Salt crystallisation

A
  • sea water evaporates leaving behind crystals in cracks = as crystals grow they put pressure on rock
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12
Q

Pressure release

A
  • rocks above eroded = decrease in weight/pressure above so rock expands
    (like releasing belt and stomach goes out)
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13
Q

Carbonation

A
  • CO2 in rain makes it slightly acidic = reacts with some rocks + dissolves them
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14
Q

Biological weathering (2 types)

A

Physical = burrowing animals or tree roots push in rock causing rock to split

Chemical= organic acids produced reacting with rock minerals

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15
Q

How do headlands and bays form

A

1- disconcordant coastline = different speeds of erosion
2- bay forms in area of weaker geology and headland forms in area of strong geology

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16
Q

How do headlands and bays continue to change over time

A
  • wave refraction round headlands
  • caves arches stacks and stumps can form
  • waves lose energy due to wave refraction and deposit sediment in bay= beach
  • bay can become wider as headland erodes
17
Q

What is wave refraction

A

1- shallow water in front of headland (wave cut platform) slows a part of the wave down
2- rest of the wave bends and breaks round the headland = erodes headland from side

18
Q

How do cliffs retreat and form

A

1- erosion at base of cliff between high + low tides = wave cut notch
2- undercutting/ continued erosion at base causes cliff to collapse
3- collapsed material = wave cut platform
4- cycle starts again and cliff retreats

19
Q

How do caves , arches , stacks and stumps form

A

1- wave refraction on WCP slows down waves directly infront of headland while waves either side bend round + attack cliff from side
2- crack forms = then cave = then arch and so on

20
Q

How do blowholes form

A

1- waves erode cave in headland
2- structure + bedding planes of rock allow vertical erosion as well as lateral
3- tunnel forms allowing water to flow through cave and out of the top

21
Q

What is a Geo

A

1- erosion enlarges a fault to form a cave
2- continued erosion causes roof to collapse = narrow steep-sided inlet called a geo

22
Q

What is mass movement + give 3 examples

A

Movement of material due to gravity
- rock fall
- landslides
- slumping

23
Q

Rock fall

A
  • rocks detached by weathering fall due to gravity
24
Q

Landslides

A
  • sliding of rock along crack or fault
25
Q

What is slumping

A
  • Saturated material becomes heavy + lubricated = collapses along curved line
26
Q

What is a beach + name 2 features found on a beach

A
  • accumulation of material deposited
    -berms + cusps
27
Q

What are berms and cusps

A
  • ridges formed at high tide mark as sediment is deposited at top of swash

-small depressions formed as backwash is channeled down beach

28
Q

What are spits + how do they form

A
  • long extended beaches attached to land at one end + stretch into sea at other
  • longshore drift carries material along coast = sediment grows out from coast
  • change in wind direction builds sediment in another direction = recurved end
29
Q

Onshore bars

A
  • a spit that connects 2 areas of land eg: across a bay
  • salt marshes form behind
30
Q

What is a tombolo

A
  • wave refraction around island = waves lose energy + deposit sediment
  • beach forms connecting island to mainland
31
Q

What are salt marshes

A
  • vegetated areas of deposition in low energy conditions
  • submerged at high tide + exposed at low
32
Q

How much does limestone erode per year

A

0.1m a year

33
Q

How much does clay erode a year

A

0.8m a year

34
Q

what angle do waves arrive at coast for LSD

A

45.c

35
Q

Spit

A

long narrow beach of sand or shingle, attached to land at one end and stretch out across a bay, estuary or change in coastline.
Formed as LSD carries sediment into sheltered areas of open water

36
Q

Onshore bars

A

Formed when a spit continues to grow across a bay or indentation.
Lagoons of brackish water are formed behind them.

37
Q

Longshore drift

A

Process of sediment transportation across a beach. Dependent on the prevailing wind.
Sediment is transported with swash at a 45 degree angle up the beach and 90 degree angle back to the sea with backwash