Formation of landforms

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13 Terms

1

What are the main erosional landforms

Bays + headlands

Cliffs

Wave cut notches, shore platforms

Caves, arches, stacks, stumps

Blowholes

Goes

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2

What’s a Discordant coastline

Where there’s alternating bands of soft and hard rock

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3

How are bays and headlands formed

  • discordant coastline is eroded through abrasion

  • Rock with weaker lithology retreats faster, forming a bay

  • Rock with stronger lithology is not as easily eroded, left sticking out as a headland

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4

How are geo formed

A geo is a narrow steep sided inlet

  • faults or joints are eroded by hydraulic action and solution, forming a cave

  • Continued erosion by abrasion, pounding and solution causes roof to collapse forming a geo

  • (Continued erosion creates a bay)

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5

How’s a blowhole formed

  • Faults or joints are eroded by hydraulic action and solution forming a cave

  • Continued erosion of vertical fault can create vertical shaft to the top of the cliff, creating a blowhole

  • (Continued erosion can cause blowhole roof to collapse forming a geo)

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6

How’s caves formed

  • the waves abrade away the rock

  • Faults in cliff are exploited by hydraulic action, breaking rock further to form a cave

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7

How are arches formed

  • constant erosion ( abrasion and hydraulic action) makes the cave wider and deeper

  • The sea cut through to form an arch

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8

How are stacks formed

  • the sea erodes the bottom of the arch over time making it wider

  • Results in the roof of the arch collapsing, leaving a stack

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9

How are stumps formed

  • overtime there will be abrading of the bottom of the stack, collapsing leaving a stump

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10

How are cliffs formed

  • the waves abrade the base of rock

  • Landslides

  • Gradual retreat

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11

How are shore platforms created

  • wave cut notch develops, undercutting cliff, cliff collapses leaving shore platforms

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12

How are wave cut platforms created

Wave erosion (hydraulic action, abrasion specifically solution) forms a wave cut notch at the bottom of the cliff between the high and low tide marks this then undercuts the cliff which retreats, this leaves a flat rocky platform then the cliff had been often covered at high tide

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