Weathering, Erosion, and Mass Movement Flashcards

1
Q

Define weathering

A

physical breakdown and chemical alteration of rock at or near Earth’s surface

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2
Q

What are the two kinds of weathering?

A

Mechanical and Chemical

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3
Q

Mechanical Weathering

A

physical forces breaking rock into smaller pieces

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4
Q

Chemical weathering

A

chemical transformation of rock into new compounds

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5
Q

True or False: Both kinds of weathering work simultaneously and reinforce each other?

A

True

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6
Q

True or False: Mechanical weathering increases surface area?

A

True

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7
Q

What is the relation between mechanical and chemical weathering

A

as mechanical weathering breaks rocks into smaller pieces, more surface area is exposed to chemical weathering

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8
Q

Types of mechanical weathering

A
  • Frost wedging
  • Sheeting/unloading
  • Biological Activity
  • Salt crystal growth
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9
Q

Frost wedging

A
  • water that freezes in cracks enlarges the cracks

- lenses of ice increase in size as they attract liquid water

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10
Q

Unloading/Sheeting

A
  • unloading leads to sheeting

- concentric slabs break loose when large masses of igneous rock are exposed due to erosion and glaciation.

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11
Q

How does an exfoliation dome form?

A

-continued weathering causes slabs to fall off and form a EXFOLIATION DOME

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12
Q

What are joints?

A

Joints are fractures produced by contraction during the crystallization of magma

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13
Q

Biological growth

A
  • PLANT ROOTS grow into fractures in rocks, expanding cracks

- BURROWING ANIMALS move fresh material to the surface, enhancing mechanical and chemical weathering

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14
Q

Types of Chemical Weathering

A
  • Dissolution
  • oxidation
  • hydrolysis
  • spheroidal weathering
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15
Q

What is the most important agent in chemical wearthing?

A

Water

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16
Q

Three things about Dissolution

A

A small amount of acid in water is responsible for the corrosive properties

  • CO2 dissolved in rain=carbonic acid
  • Calcite (CaCO3) is particularily susceptible to weakly acidic solutoin
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17
Q

Three things about Oxidation

A

rust (iron oxide) forms when O2 combines with Fe

  • water catalyses the rxn
  • important in decomposing ferromagnesium minerals (olivine, pyroxene, hornblende, and biotite)
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18
Q

Two things Hydrolysis

A
  • any rxn with water

- silicates (clay) decompose via hydrolysis

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19
Q

True or False: Clay minerals are the most abundant product of weathering

A

true

20
Q

Spheroid weathering (3)

A

1) water penetrates jointed rocks
2) chemical waethering decomposes minerals and enlarges joints
3) rocks are attacked around the corners and edges, producing spherical shapes and fragments

21
Q

What influences the rate of weathering

A

Rock Type and Climate

  • silicate minerals weather in same order as Bowen’s rxn series (Olivine –> pyroxine –> amphibole –> biotite etc)
  • warm/moist climates enhance weathering
  • cold/dry climates inhibit
22
Q

Differential Weathering

A

uneven weathering due to different mineral composition

23
Q

Examples of differential weathering

A

Soil

-portion of regolith that supports growth of plants

24
Q

Define regolith

A

Mineral fragments that cover the surface of earth

25
Q

Impact of human activity on soil

A

soil erosion (loss of topsoil)
-enhanced by deforestation and farming
soil conservation
-planting in patterns that follow contour of landscape reduces rate of water runoff
-grassed waterways between crops prevetns formation of gullies and traps soil washed from cropland

26
Q

True or False: Weathering and erosion are slow processes (snail)

A

true

27
Q

Define Mass Movement

A

movement of bedrock, rock debris, or soil downslope due to gravity
-ie. landslide

28
Q

What is the main driving force of mass movement?

A

erosion agents (weathering, erosion etc)

29
Q

Gravitational Driving Force

A

F(drive)=ma=mg

30
Q

Friction and Cohesion RESISTING FORCE

A

F(res)= mu(fric)mgcos(theta)

F(res)=basal friction+internal strength

31
Q

Shear deformation

A

internal deformation (flow) due to gravity

32
Q

Factors that influence internal strength of rock debris, sediment, or soil

A

1) electrostatic forces (ie. clay particles)
2) friction @ grain contact=f(angularity, grain size)
3) pore pressure
4) surface tension
(wet sand–>dry sand–>damp sand) (in order of increasing cohesion)

33
Q

Define Angle of repose

A

increase with grain size

  • fine sand (round): 35 degrees
  • fine sand (angluar): 40
  • course sand: 45
34
Q

What makes a slope SUSCEPTIBLE to mass movement

A

1) slope angle
2) relief
3) bedrock type (ie. jointed, fractured, bedded)
4) thickness of debris (ie. soil cover)
5) climate
- a) ice (freeze-thaw cycle)
- b) water/moisture
- c) rain
- d) vegetation (low cover)

35
Q

What TRIGGERS mass movement

A
  • heavy rainfall/snowmelt
  • addition of buildings
  • earthquakes/explosions/eruptions
  • excavation/road construction/ river erosion
36
Q

Falls

A

Rock: rockfall, very fast
Debris: debrisfall, fast-very fast

37
Q

Slide

A

Rock: rockslide, fast
Debris:
-slump (rotational), slow-moderate
-debris slide (translational), slow-fast

38
Q

Flow:

A
Rock: 
-creep, very slow (10 cm/yr)
Debris:
-creep, very slow (,10 cm/yr)
-Earthflow/gelifluction/debris flow/mudflow/quick clays, mod-fast
-avalanche, very fast
-
39
Q

creep

A

very slow
Mechanisms:
-wet/dry cycle
-freeze/thaw cycle

40
Q

gelifluction

A

in colder climate: H2O saturated debris moves over permafrost during warmer months

41
Q

Debris flow

A

course material (boulder/gravel) is predominant, supported by matrix of finer sediment

42
Q

mudflow

A

mix of debris and water, confined by chanel

  • faster/further than debris flow
  • high water content
43
Q

Where do mudflows occur

A

flanks of volcanoes, steep deforested mountain sides, steepened cliffs of unconsolidated fine sediment

44
Q

True or False; Pyroclastc flows (ash, hot gases, sediment) turn into mudflows (sediment and water) downstream

A

true

45
Q

Quickclays

A
  • clays deposited in laciomarine environments

- decreased stability when salt is leached out by freshwater

46
Q

Clay mineral formation

A

orthoclase feldspar + acid+ water = clay + potassium + soluble silica
(2KAlSi3O8 + 2H+ + 9H2O = Al2Si2O5(OH)4 + 2K+ + 4H4SiO4)

47
Q

What is the relative rate of weathering of common minerals?

A

most stable to least stable;
Iron oxide, aluminum hydroxides, quartz, clay minerals, musovite mica, potassium feldspar, boilite, albite, amphiboles, pyroxene, anorthite, olivine, calcite, halite.