Weathering and Rocks Flashcards

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1
Q

Freeze thaw weathering

A

when water in joints and cracks freeze at 0 degrees
expands by 10%
exerts pressure

most effective where moisture is plentiful so frequent fluctuations above and below freezing

common in peruglacial and alpine regions

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2
Q

Pressure Release

A

Overlying rocks are removed by erosion
causes underlying rocks to expand and fracture parallel to the surface
removal of a great weight e.g. glacier has the same effect

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3
Q

Heating and cooling

A

different minerals expand and contract at different temperatures

grandiose disintegration i rocks composed of different minerals
eg granite contains feldspar mica and quartz

block disintegration happens when the rock consists of a single mineral

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4
Q

Salt Crystallisation

A

the decomposition of rock by solutions of salt

in areas where temperatures fluctuate around 26-28 degrees sodium carbonate and sulphate expand by 300%
creates pressure on joints forcing them to crack

water evaporates leaving salt crystals behind
the temperature rises salts expand and exert pressure on rock

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5
Q

where is salt crystallisation found?

A

hot desert regions
low rainfall
high temperatures

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6
Q

Disintegration

A
Rock heats up in day and contracts at night
rocks of conductor of heat
stressed only occur on the outer layers
peeling or exfoliation thus occurs
moisture is essential
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7
Q

Where does disintegration occur

A

Hoy desert areas
large diurnal temperature range
deserts temperatures exceed 40 degrees and drop below freezing at night

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8
Q

where does physical weathering occur

A

at or near the earths surface

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9
Q

where does chemical weathering occur

A

sub surface

percolating water has gained organic acids from soil and vegetation

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10
Q

Carbonation (solution)

A

Occurs in rocks with calcium carbonate
eg chalk or limestone

rainfall columbines with dissolved carbon dioxide or organic acid to form weak carbonic acid

calcium carbonate reacts with acid water and forms calcium bicarbonate which is soluble and removed in solution by percolating water

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11
Q

Hydration

A

a process whereby certain minerals absorb water expand and change

eg shales and mudstone increase in volume by the 100% when clay minerals absorb water

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12
Q

Oxidation

A

when iron compounds react with oxygen to produce a reddish brown coating

dissolved oxygen in soil or atmosphere affects iron

oxidation is only under extreme acidity meaning it remains in many soils and rocks giving it a red colour

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13
Q

Hydration

A

Certain rocks containing feldspar (GRANITE) reacts with acid water
to produce kaolin and leaving behind quartz and mica

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14
Q

Organic Action

A

Acids derived from the decomposition of vegetation are termed humid acids

Bacterial activity and the respiration of plant roots raise carbon dioxide levels in soil siding solution

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15
Q

what type of sediment is prone to oxidation

A

iron oxide based

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16
Q

how can vegetating increase weathering

A

release of organic acids through root systems

solution of limestone is greater under soil than bare rock due to extra organic acids released by vegetation in soil

17
Q

how can grain size influence weathering

A

coarse trained rocks weather quickly due to large empty spaces and high permeability

fine grained rocks offer a greater surface area for weathering and may be highly susceptible to weathering

18
Q

vant hoffs law

A

the rate of chemical weathering increases 2/3 rimes for each increase of 10 degrees

19
Q

main processes of weathering for granite

A

freeze thaw

hydrolysis

20
Q

what is in granite

A

quartz
feldspar
mica

21
Q

how could a mudflow affect the shape of slopes

A

leave a bowl shaped scar where movement starts

depositional toe at base

stepened upper slope
decreased angle at the base as a result of depositional toe

flow tracks produced

22
Q

how can humans affect slopes

A

undercutting (roads, quarrying, mining)

vegetation removal (deforestation)

overloading slope (waste or resovoirs)

23
Q

describe the process of pressure release

A

creation of joints and other weakness in rocks by the removal of overburden and the release of pressure

24
Q

chelation

A

chemical weathering
of rocks
by organic acids and molecules

25
Q

how do fold mountains form (at both plate margarine)

A

sediments (accretionary wedges) are scraped off the ocean floor and rise over the higher plate