Com2--EQ2-4.3 + 4.4 Flashcards

1
Q

Hard rock coasts

A

Consist of more resistant rocks that erode slower, such as igneous granite or resistant chalk

  • Flamborough head (E. Yorkshire)
  • Lulworth cove (Dorset)
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2
Q

Soft rock coasts

A

Consist of less resistant rocks that erode faster, such as clays or shales

  • Holderness coast (E. Yorkshire)
  • North Norfolk coasts
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3
Q

What are joints

A

Joints are small, usually vertical, cracks found in many rocks

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4
Q

What are faults

A

Faults are larger cracks caused by past tectonic movements where rocks have been moved

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5
Q

Effects of joints and faults on a cliff

A
  • The more joints and faults that are in a cliff, the easier it is to erode as it is weaker
  • Joints and faults in a cliff can form caves which turn into arches which then become stacks, which can erode to make stumps
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6
Q

Discordant Rock Structure

  • Rock alignment to coast
  • Type of rock facing the wave
  • Features and landforms
  • Examples
A
  • Perpendicular
  • Alternating rock types; resistant, weak, resistant, weak
  • Arch, stacks, stumps, HEADLANDS AND BAYS
  • Studland bay, Ballard Point; Swanage Bay, Durlston Head
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7
Q

Concordant Rock Structure

  • Rock alignment to coast
  • Type of rock facing the wave
  • Features and landforms
  • Examples
A
  • Parallel
  • One rock type facing waves, may vary in weakness
  • Can be featureless, coves, cliffs, caves, stair holes
  • Durlston Head to Kimmeridge
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8
Q
Constructive waves
-Wave height
-Wave length
-When are they common
-Wave frequency
-Swash/Backwash
Wave shape and effect
A
  • Low wave height
  • Long wave length
  • Common in summer
  • Low wave frequency(6-8 waves per minute)
  • Strong swash than backwash
  • Surging waves add sediment to the beach
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9
Q

Destructive waves

  • Wave height
  • Wave length
  • When are they common
  • Wave frequency
  • Swash/Backwash
  • Wave shape and effect
A
  • High wave height
  • Short wave length
  • Common in winter
  • High wave frequency(10-14 waves per minute)
  • Stronger back wash than smash
  • Plunging waves remove sediment from the beach
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10
Q

Sub-Ariel processes

A

Freeze thaw weathering
Biological weathering (mechanical weathering)
Chemical weathering

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11
Q

Mass Movement- Rotational slumping

A
  1. Rain falls and it accumulates at the boundary between sand and clay which lubricates the boundary
  2. Sand is permeable and allows water to pass through but clay is impermeable and prevent water passing through
  3. Sand becomes saturated becomes and will dramatically slump rotationally
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12
Q

Mass movement- Rock Slides

A
  1. Joints or bending planes are aligned diagonally to the sea
  2. Erosion at the base or weathering st the top of cliff means the cliff becomes unsupported and sometimes lubricated by the rain
  3. The rocks moves in a straight diagonal line
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13
Q

Long shore drift

A
  1. Winds and waves break at an angle to the coast
  2. Sediment moved up the beach by swash
  3. Sediment dragged down at an angle by the backwash
  4. Sediment is gradually moved along the beach
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14
Q

Hydraulic Action

A

Water is forced into the cracks, compressing the air within the rock.
The pressure increases and expands.
Rock chips of and cracks get bigger

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15
Q

Abrasion

A

The rocks are picked up by the waves and thrown against the cliffs
This action wears away the rock and gradually removed

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16
Q

Solution

A

The sea becomes slightly acidic. This is caused by vegetation near the cliffs.
This erodes rock such chalk or limestone

17
Q

Attrition

A

Rocks that are held within the waves smash into each other. Gradually the rocks become rounder and smoother (pebbles)