Topic 1 Flashcards

1
Q

active tectonics

A

ongoing deformation of earth’s crust

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2
Q

passive tectonics

A

indirect influence on processes and forms through spatial distribution of lithology and structure

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3
Q

does lithology and structure play an important role in active tectonics?

A

no

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4
Q

magnitude of isostatic compensation of erosion and the spatial scale is related to ___ of the crust

A

flexural rigidity

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5
Q

Secondary uplift through flexure

A

load is added at a distance away, resulting in lowering of the crust underneath the load and elevation of the crust

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6
Q

what do climate cycles do across the globe?

A

they distribute climate systems

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7
Q

attributes of a climate system are

A

precipitation, temperature, wind speed and relative humidity (RH)

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8
Q

glacial geomorphology

A

glacial moraines, trimlines, polished surfaces, forebuldges and isostatic response.

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9
Q

coastal geomorphology

A

sea level RISE: marine terraces

sea level FALL: barrier islands

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10
Q

fluvial geomorphology

A

fluvial terraces, river knickpoints

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11
Q

how does a river respond to a lowering sea level?

A

by incising. incision propagates upstream; causing a narrowing of the river valley and formation of terraces

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12
Q

plate tectonics

A

controls distribution of landmasses and ocean circulation through opening and closing of passages

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13
Q

ice sheets and glaciers

A

increases albedo

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14
Q

mountain topography

A

windward side: precipitation, increased runoff, increased mass wasting and lower snow line
leeward side: decreased runoff, rain shadow

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15
Q

volcanic eruptions

A

brings matter, aerosols, CO2 into the atmosphere. Increasing cloud coverage and decreases solar radiation coming in.

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16
Q

weathering

A

removal of carbon from the atmosphere, soluble cations and bicarbonate carried into rivers and calcium carbonate formation in the ocean.

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17
Q

weathering

A

physical and chemical break down of materials

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18
Q

importance of weathering is due to the production of ____, ____ and ____

A

sediment, by products and soils

19
Q

what makes weathering a disequilibrium response?

A

conditions at the surface are very different from those during rock formation

20
Q

what are 6 types of physical weathering?

A

pressure release, freeze thaw, thermal expansion, salt crystal growth, biotic, hydration

21
Q

what are 4 types of chemical weathering?

A

solution, oxidation, hydrolysis, ion exchange

22
Q

physical weathering is

A

the break down of materials into smaller pieces, allowing more surface area for weathering. No chemical composition change.

23
Q

chemical weathering is

A

decomposition of minerals through chemical alteration.

24
Q

driving forces of physical weathering

A

water and temperature. (climate controlled)

25
resisting forces of physical weathering
lithology and structure. (rock controlled)
26
driving forces of chemical weathering
water and temperature
27
resisting forces of chemical weathering
silicates (look at bowens reaction series)
28
chemical weathering is strongest with
high precipitation and temperature
29
physical weathering is strongest with
low precipitation and moderate temperature
30
soil mantled landscapes form when
rate of soil production > erosion rate
31
bedrock landscapes form when
rate of soil production < erosion rate
32
mass movements
form of dominant transport for how weathered materials make it way down to the valley floor
33
shear strength
magnitude of shear stress that a soil can sustain or overall resistance to movement/deformation.
34
what happens when water fills the pore spaces?
normal stress decreases
35
factor of safety
stability of a slope and is the ratio between the forces resisting movement to those drivers
36
what are 3 types of stresses?
tensile, compressive and shearing
37
what are 3 common types of strain-stress responses?
elastic, plastic and viscous fluid
38
dilatant
viscosity increases with shear stress
39
pseudoplastic
flows as grains re-arrange and pore water escapes
40
liquefaction
loss of soil strength under shock and leads to fluid behaviour
41
toppling
brittle failure or plastic rotational stability depends on aspect ratio
42
slides
failure on distinct shear surfaces with little internal deformation
43
spreads
more cohesive material sinks into deformable layers underneath
44
creep
upward heave with downslope displacement