Tectonics and Climate Readings Flashcards

1
Q

Montgomery and Willet Date ?

A

2001

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2
Q

What was Montgomery and Willet paper about?

A

The significance of exogenic processes in the Andes

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3
Q

Influence of tectonics on Andes?

A

Uplift of the Andes began 60 million years ago during late Pleistocene
Continuous uplift driven by collision of the Nazca and South American Plates
Create ‘topographic template’

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4
Q

Climate influence on geomorphology of the Andes

A

more current influences of climatic processes -
due to the Andes longitudinal span runs through range of climatic zones result in differences across the mountainous landscape

1) normal fluvial erosion in Northern Andes = high precipitation = narrow mountain range

2) glacial land sculpting = At higher latitudes glaciers preferentially erode the highest ground in the Southern Andes = excess elevation at the glacial limit and systematic decline in max elevation towards pole

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5
Q

Where is tectonics most dominant in the Andes - and why?

A

In central Andes
there is little erosion in except in big river valleys
= leads to crustal thickening by tectonic wedge propagation
Creates linear Hypsometry

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6
Q

Quote from Willet and Montgomery

A

We view tectonics and erosion as a coupled system with potential for feedback between climate driven erosion and tectonic forcing

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7
Q

Raymo and Ruddiman date?

A

1992

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8
Q

Raymo and Ruddiman - about

A

Uplift of the Tibetan plateau may have caused global cooling in the Cenozoic led the growth of large continental ice sheets in both hemispheres

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9
Q

Tibetan Plateaux description

A

elevation exceeds 4500m
surrounded by high mountain ranges - Himilayas to the South
Southwestern China
Largest area of uplifted crust on earth

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10
Q

how did Tibetan Plateau impact in Cenozoic?

A

Uplift resulted in perturbation of atmospheric circulation on a hemispheric scale
and altered weathering patterns this then resulted in a positive feedback mechanism as glacial erosion further increases erosion and cooling worldwide
Chemical weathering = Increase in drawdown of Co2 = further cooling

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11
Q

General Argument supporting Raymo and Ruddiman

A

That Tectonic processes can impact effect climate changes resulting in changes to global geomorphic landscape (Work in positive feedback cycles)

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12
Q

Hilton and West - Date

A

2020

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13
Q

Hilton and West (2020) -

A

Discusses the ways that mountain building processes effect the carbon cycle

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14
Q

How does silicate weathering effect the carbon cycle?

A

Silicate minerals, eg.olivine, react with CO₂ and water through chemical weathering.
= reaction removes CO₂ from the atmosphere and converts it into bicarbonate ions (HCO₃⁻) in solution. these are then carried to rivers = to oceans sink
Climate silicate weathering strongest in areas that have highest erosion

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15
Q

Relationship between erosion rate and co2 flux

A

Where erosion rates are low - weathering products accumulate and shield underlying rocks = weathering limited by supply as material not exposed for weathering

when erosion rates are high - surface area of rock exposed = higher removal of atmospheric Co2 = erosion limited by other factors eg, temperature, Co2 conc

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16
Q

Why do mountainous areas vary in their sink/source relationship to the carbon cycle?

A

Different mountains underlain by different geology
Sedimentary rocks = carbon rich= carbon source
volcanic rocks = not carbon rich = carbon sink

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17
Q

Molnar et al - date

A

2007

18
Q

Molnar et al (2007) -

A

tectonic fracturing of rock can result in an increased rate of erosion

19
Q

How does fractured rock increase erosion rate?

A

reduced rock strength = lower resistance to erosion
broadens the surface area available to erode
disintegration = breaks up into smaller blocks that are easier to transport

20
Q

Evidence demonstrating the significance of fracturing as an endogenic erosive process-

A

places where tectonic activity lies dormant rapid erosion does not occur despite high rainfall

21
Q

Brain - date?

A

2010

22
Q

Brain (2010)

A

new evidence suggests that earths topography is actually cased by viscous stresses from flow in the underlying mantle not just plate movement

23
Q

Impact of mantle movement on topography -

A

upward mantle flow = positive topography = high relief
Downward mantle flow = = negative topography depressions
Height of topography = direct proportion to intensity and depth of mantle flow
driven by gravitational force

24
Q

Where can we study effects of mantle flow? and why?

A

Australia
Has been tectonically stable since separation from Antarctica
can study how mantle dynamics effect shoreline and surface features
Drowned Reefs in North eastern Australia = resulted due to subsidence during Miocene as result of mantle flow from Subduction north of Papa New Guinea

25
Q

BLAG Hypothysis - who

A

Berner et al (1983)

26
Q

what is Blag hypothesis

A

Co2 governs the global climate and weathering of silicate rocks
Higher Co2 = increased rainfall = greater chemical weathering potential = removes co2 from atmosphere
Inversely - loss tectonic activity - less co2 release - less weathering = colder climate - icehouse system

27
Q

Dissolution reaction

A

calcite + co2 + water —> calcium + bicarbonates

28
Q

What type of landscapes illustrate the interplay of tectonics and climate acting over a range of spatial and temporal scales?

A

Karst landscapes
Eg - Dolines

29
Q

What are Dolines?

A

natural enclosed depression in karst landscapes
range from metres to tens of meteres in both diameter and depth
Found in - kentucky, Namibia, Temperate UK

30
Q

exogenic

A

formed or occurring on the surface of the earth

31
Q

endogenic

A

formed or occurring internally, geology. formed or occurring within the earth.

32
Q

weathering

A

physical or chemical breakdown of rocks and soil in place

33
Q

erosion

A

The process of transporting weathered rock and soil away from where it was broken down.

34
Q

erosivity

A

potential of the erosive force

35
Q

erodibility

A

resistance of the material being eroded

36
Q

Denudation

A

denudation is the sum of all processes that lower the Earth’s surface

37
Q

exogenic factors that influence weathering

A

Climate
Vegetation
topography
soil composition
biological activity

38
Q

Endogenic factors that effect weathering

A

mineral composition
structural features - eg fractures and faults
geological age
tectonic activity

39
Q

key drivers of exogenic processes -

A

Solar energy - atmospheric and oceanic circulation, influencing weather patterns and temperatures, which affect weathering and erosion.
Gravity - mass movements
water - rainfall rivers and glacier
Wind - aeolian erosion

40
Q

key drivers of endogenic processes -

A
  • Heat from earths interior - Geothermal heat drives processes like mantle convection,
  • Radioactive decay - decay of radioactive isotopes generates hear contributes to thermal dynamics
  • Movement of tectonic plates
    Pressure - due to overlaying rock layers can lead to metamorphism and formation of new minerals
41
Q

Time scales of exogenic and endogenic processes

A

Exogenic often much shorter but both can operate at range

42
Q
A