Rocks and Weathering Flashcards

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1
Q

weathering

A

the decomposition and disintegration of rocks in situ

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2
Q

decomposition

A

chemical weathering that creates altered rock substances

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3
Q

disintegration

A

mechanical weathering that produces smaller, angular fragments of the same rock

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4
Q

biological weathering

A

plants and animals chemically alter and physically break rocks through their growth and movement - not a separate type of weathering but a form of disintegration and decomposition

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5
Q

erosion

A

wearing away of soil and rock particles that are moved elsewhere by a transport agent

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6
Q

3 types of weathering

A

mechanical
chemical
biological

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7
Q

oxidation

A

rocks exposed to air, ferrous soil oxidises and changes to ferric state
rocks exposed by digging, attrition, plate movement, bio. weathering

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8
Q

oxidation equ.

A

4Fe + O2 –> 2Fe2O3

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9
Q

carbonation-solution

A

calcium carbonate reacts with acid water, forming calcium bicarbonate which is soluble and is removed by percolating water

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10
Q

carbonation-solution equ.

A

CO2 + H2O → H2CO3

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11
Q

carbonation-solution conditions

A

rocks containing calcium carbonate - eg. limestone, generally warmer wetter climates, rainfall combines with CO2 to form a weak carbonic acid-higher pH = more effective

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12
Q

hydrolysis

A

chemical breakdown of a substance when combined with water

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13
Q

hydration

A

certain minerals in the rock absorb water, expand and change, causing mechanical stresses also

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14
Q

hydration conditions

A

water absorbed into rocks - porous/cracked rocks make it more effective

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15
Q

freeze-thaw

A

water seeps into crack in the rock, freezes, expands, pushing crack open wider, thaws and water fills the crack further, repeating the process, over time breaking the rock

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16
Q

freeze-thaw conditions

A

coastal environments/environments where moisture is plentiful and temperature frequently fluctuates above and below freezing – eg. periglacial and alpine regions

17
Q

how do mudflows occur

[3]

A

A mud flow is caused by high water content of the regolith, so that internal cohesion is
reduced, and gravity causes movement downslope