Com2--EQ2-4.3 + 4.4 Flashcards
Hard rock coasts
Consist of more resistant rocks that erode slower, such as igneous granite or resistant chalk
- Flamborough head (E. Yorkshire)
- Lulworth cove (Dorset)
Soft rock coasts
Consist of less resistant rocks that erode faster, such as clays or shales
- Holderness coast (E. Yorkshire)
- North Norfolk coasts
What are joints
Joints are small, usually vertical, cracks found in many rocks
What are faults
Faults are larger cracks caused by past tectonic movements where rocks have been moved
Effects of joints and faults on a cliff
- 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
Discordant Rock Structure
- Rock alignment to coast
- Type of rock facing the wave
- Features and landforms
- Examples
- Perpendicular
- Alternating rock types; resistant, weak, resistant, weak
- Arch, stacks, stumps, HEADLANDS AND BAYS
- Studland bay, Ballard Point; Swanage Bay, Durlston Head
Concordant Rock Structure
- Rock alignment to coast
- Type of rock facing the wave
- Features and landforms
- Examples
- Parallel
- One rock type facing waves, may vary in weakness
- Can be featureless, coves, cliffs, caves, stair holes
- Durlston Head to Kimmeridge
Constructive waves -Wave height -Wave length -When are they common -Wave frequency -Swash/Backwash Wave shape and effect
- 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
Destructive waves
- Wave height
- Wave length
- When are they common
- Wave frequency
- Swash/Backwash
- Wave shape and effect
- 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
Sub-Ariel processes
Freeze thaw weathering
Biological weathering (mechanical weathering)
Chemical weathering
Mass Movement- Rotational slumping
- Rain falls and it accumulates at the boundary between sand and clay which lubricates the boundary
- Sand is permeable and allows water to pass through but clay is impermeable and prevent water passing through
- Sand becomes saturated becomes and will dramatically slump rotationally
Mass movement- Rock Slides
- Joints or bending planes are aligned diagonally to the sea
- Erosion at the base or weathering st the top of cliff means the cliff becomes unsupported and sometimes lubricated by the rain
- The rocks moves in a straight diagonal line
Long shore drift
- Winds and waves break at an angle to the coast
- Sediment moved up the beach by swash
- Sediment dragged down at an angle by the backwash
- Sediment is gradually moved along the beach
Hydraulic Action
Water is forced into the cracks, compressing the air within the rock.
The pressure increases and expands.
Rock chips of and cracks get bigger
Abrasion
The rocks are picked up by the waves and thrown against the cliffs
This action wears away the rock and gradually removed