2b.3b Flashcards

1
Q

Define impermeable

A

A rock that doesn’t allow water to pass through it.

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2
Q

Define permeable rock

A

rock that allows water to pass through it

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3
Q

Two types of alternating strata in cliff

A
  • resistant and less resistant
  • permeable and impermeable
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4
Q

What does differential erosion of alternating strata of rock produce

A

complex cliff profiles and influences recession rates

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5
Q

Define till

A

Deposits of angular rock fragments in a finer medium.

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6
Q

What happens if there is a cliff wiht permeable rock strata above the impermeable strata

A

Weakly consolidated rock is vulnerable to mass movement as rainwater percolating into the upper strata creates instability

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7
Q

What is the overall rate of cliff erosion determined by

A

determined by the resistance of its weakest rock layer

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8
Q

What happens to less resistant strata

A

Less resistant strata erode and weather quickly, being cut back rapidly, wave cut notches may be formed.

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9
Q

What happens to resistant strata

A

Resistant strata erode and weather slowly, retreating less rapidly. They may form a ‘bench’ feature at the cliff base. Higher up, they form overhanging sections until they collapse by mass movement

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10
Q

Why is rock permeable

A

they’re porous (chalk and poorly cemented sandstones)
they have numerous joints (e.g. carboniferous limestone)

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11
Q

Why is permeable rock less resistant to weathering

A

water percolating comes into contact with a large surface area that can be chemically weathered
e.g. Limestone weathered by carbonation converting calcium carbonate to soluble calcium bicarbonate.
Feldspar in granite weathered by hydrolysis into kaolin (china clay)

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12
Q

State impermeable rocks

A

clays, mudstones, igneous, metamorphic

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13
Q

How does saturation affect cliff profile

A
  • Saturation promotes mass movement through lubrication and by adding weight.
  • Leads to slumping in unconsolidated material and sliding in consolidated strata.
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14
Q

How does permeability create springs

A

Where a permeable rock overlays an impermeable stratum groundwater is unable to percolate down into the lower layer.
Water accumulates in the permeable layer, producing a saturated layer where the pores are full of water.
A spring will form on the cliff face at the top of the saturated layer.
As the stream flows down the cliff, fluvial erosion (surface run off erosion( will attack the saturated permeable bed and lower impermeable stratum, reducing the angle of the cliff profile.

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15
Q

How does groundwater flow remove cement

A

Water flows through the permeable (sands) but can’t flow through the impermable (clay), so flows along the interface. Groundwater flow through rock layers can weaken rock by removing the cement that binds them together. Weak, unconsolidated layers slump.

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