erosional landforms Flashcards

1
Q

erosional landforms examples

A

forms wave cut notches, wave cut platform, cliffs, caves, arcs, stacks, stumps

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2
Q

4 types of erosion

A

hydraulic action/ abrasion/ attrition/ solution

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3
Q

erosion wave type

A

destructive waves

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4
Q

explain how wave cut notches are formed

A

eroded by hydraulic action and abrasion and possibly corrosion

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5
Q

what is the formation of a wave cut platform

A
  • Marine erosion between high tide and low tide is eroded by abrasion and hydraulic action forming a wave cut notch along the length of the cliff base.
  • the notch deepens until the overlying material collapses by mass movement due to gravity.
  • coastal recession occurs this process repeats.
  • the rock below tide level is always submerged and is not eroded as it is not exposed to wave impact
    as the overlying material is eroded the uneroded rock at low tide is flat
    forming a wave cut platform
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6
Q

how are cliffs formed

A

marine erosion of the land between high tide and low tide - hydraulic action and abrasion forms a wave cut notch
the notch deepens until the overlying rock collapses due to gravity and the exposed face forms a cliff

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7
Q

explain the cave FORMATION

A

rocks have joints or faults which are eroded and widened by hydraulic action until a cave forms

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8
Q

ARCH FORMATION

A

the cave is eroded through the headland until its meets the other side and connect forming an arch
Hydraulic action and abrasion attack the sides of the arch between low tide and high tide, forming wave cut notches.
overlying material collapses widening the arch.

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9
Q

STACK FORMATION

A

Weathering and other sub-aerial processes attack the arch roof.
Eventually, the roof of the arch will collapse by blockfall leaving the seaward end of the headland detached from the land as a tall vertical column called a stack.

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10
Q

STUMP

A

Marine erosion at the base of the stack will form a notch on all sides until the stack collapses by blockfall.
Remnants of the stack base form a stump, a small projection of rock, exposed only at low tide.

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