Weathering + Mass Wasting Flashcards

1
Q

Denudation

A

removal, wearing away, disintegration of rock material

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2
Q

3 types of denudation in order

A

1) weathering = breaking down of rock into smaller pieces by atmosphere
2) mass wasting = short distance VERTICAL movement of broken rock material
3) erosion = (horizontal) removal, transportation, deposition of rock material over wider areas

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3
Q

What are rock openings

A

1) Microscopic openings
2) joints
3) faults
4) lava vesicles
5) solution cavities

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4
Q

Microscopic openings

A

1) consist of spaces between crystals of igneous or metamorphic rocks

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5
Q

Joints

A

VERTICAL Cracks that develop as a result of stress BUT rocks do not show noticeable displacement along breaks
most important of all rock openings in facilitating weathering

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6
Q

Bedding Plane

A

horizontal crack (similar to joint BUT not vertical)

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7
Q

Faults

A

Breaks in bedrock caused by forced displacement of rock structure

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8
Q

Lava vesciles

A

holes of various sizes that develop in cooling lava when gases aren’t able to escape

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9
Q

solution cavities

A

holes formed in carbonate rocks (limestone) by soluble minerals dissolving + being carried away

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10
Q

Joints vs faults

A

Joints = no displacement
Faults = displacement

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11
Q

Types of weathering agents

A

1) mechanical
2) chemical
3) biological

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12
Q

Mechanical Weathering

A

1) Physical disintegration of rock without changing composition
(grinding)
2) occurs at surface 3) Examples:
- frost wedging (cold places) or salt wedging (hot places w. capillary reaction)
- temp changes (think wildfires) cause rocks to expand + weaken –> mini fractures form
- exfoliation = curved layers peel off bedrock, creating shapes like Halfdome (need bedrock)
- biotic processes = plant roots can spread rocks apart

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13
Q

Chemical Weathering

A

1) decomposition of rock by chemical alteration of minerals
2) requires moisture + surface area –> finely grained materials decompose more rapidly

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14
Q

Examples of chemical weathering

A

1) oxidation = when oxygen (in water) comes into contact with rock –> produces iron oxide
2) Hydration = water added to compound + becomes part of it –> forms hydrates (increases volume, contribute to disintegration)
3) hydrolysis = water added to compound + breaks it up i.e. silicate materials
4) carbonation = carbon dioxide dissolved in water, producing carbonic acid –> reacts with carbonate rocks to produce calcium bicarb –> forms stalagmites/tites
5) spheroidal weathering = thin rock layers peel off boulders, rounding it. outcome of hydration

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15
Q

Biological Weathering

A

1) weathering that involves living organisms
2) examples = plant roots into cracks + crevices
3) lichen remove minerals from rock + alternate btwn wet/dry, weakening rock –> leading to weathering
4) burrowing by animals

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16
Q

Weathering in diff climates

A

1) High temps + abundant precipitation = lead to more weathering
2) moisture more important than temp
3) desert regions = more mechanical than chem. weathering bc lack of water
$4) shallow weathering in tundra/desert + deep weathering in trop. rainforest

17
Q

What factors influence mass wasting

A

1) angle of repose
2) water
3) clay
4) permafrost

18
Q

Mass wasting factor = angle of repose

A

1) angle of repose = steepest angle where rocks/soil don’t slide off
2) balance between gravity + cohesion of rock to surface

19
Q

Mass wasting factor = water

A

1) addition of water = lubricating medium + diminishes friction btwn particles
2) reduces angle of repose

20
Q

Mass wasting factor = clay

A

1) clay becomes very slippery when absorbs water
2) quick clays = change from solid mass to near liquid very quickly

21
Q

Mass wasting factor = permafrost

A

contributes to mass wasting in subarctic regions + high latitudes

22
Q

Types of mass wasting

A

1) fall
2) slide
3) flow
4) creep

23
Q

Mass wasting = fall

A

1) falling of rock downslope
2) Rock that falls called talus
3) dry + fast

24
Q

Slide

A

1) abrupt + rapid
2) top of hill has a deep scar –> exposed bedrock + debris
3) more moist than fall –> if extremely moist it’s mudflow

25
Q

Flow

A

1) becomes unstable because absorption of water + moves downhill
2) can vary in speed, depending on friction
3) gravity is impelling force + water is catalyst
4) Earthflow = portion of water-saturated slope moves downhill
5) mudflow = rapid movement of wet material through canyon/valley + deposited in fan-shape

26
Q

Creep

A

1) slowest + dry
2) very gradual downhill movement of regolith that hard to notice
3) occurs mostly on steep lightly vegetated slope
4) caused by freeze/thaw cycles –> freezes moved upward bc of increasing vol of ice BUT when it thaws particle settles slightly downslope

27
Q

Solifluction

A

1) Special form of creep
2) restricted to high latitude + high elevation tundra
3) thaws BUT water not able to penetrate permafrost, so active layer (Above frost) becomes oversaturated + moves downhill

28
Q

Differential weathering

A

1) All rock does not weather at same rate or to same extent
2) some rocks easily weathered –> weak
3) other rocks –> stronger + more resistant to weathering

29
Q

What are agents of erosion

A

1) wind
2) water (biggest factor)
3) ice

30
Q

A Climate weathering type

A

1) Chemical - hot + lots of water draining through –> lots of oxygen WHICH is why there is lots of oxidation –> laterization = red soil (bc of iron)
2) No mechanical = too hot for frost wedging + not enough bedrock for exfoliation

31
Q

E Climate weathering type

A

1) No chemical = standing water –> soil is saturated + no oxygen –> no chemical reactions
2) mechanical = frost wedging + temperature fluctuations

32
Q

B, C, D Climate weathering type

A

1) BOTH MECHANICAL + CHEMICAL
B climates = mainly mechanical since not enuf water for chemical weathering

33
Q

Describe how mass wasting varies by moisture + speed

A

1) As you add moisture: rockfall –> landslide –> mudslide
2) Speed: Solifluction (slowest) –> earthflow –> mudflow
3) Slowest + driest = creep (poles tilting bc ground moves v slowly)
FLOWS NEED WATER