Tectonics and Climate Readings Flashcards
Montgomery and Willet Date ?
2001
What was Montgomery and Willet paper about?
The significance of exogenic processes in the Andes
Influence of tectonics on Andes?
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’
Climate influence on geomorphology of the Andes
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
Where is tectonics most dominant in the Andes - and why?
In central Andes
there is little erosion in except in big river valleys
= leads to crustal thickening by tectonic wedge propagation
Creates linear Hypsometry
Quote from Willet and Montgomery
We view tectonics and erosion as a coupled system with potential for feedback between climate driven erosion and tectonic forcing
Raymo and Ruddiman date?
1992
Raymo and Ruddiman - about
Uplift of the Tibetan plateau may have caused global cooling in the Cenozoic led the growth of large continental ice sheets in both hemispheres
Tibetan Plateaux description
elevation exceeds 4500m
surrounded by high mountain ranges - Himilayas to the South
Southwestern China
Largest area of uplifted crust on earth
how did Tibetan Plateau impact in Cenozoic?
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
General Argument supporting Raymo and Ruddiman
That Tectonic processes can impact effect climate changes resulting in changes to global geomorphic landscape (Work in positive feedback cycles)
Hilton and West - Date
2020
Hilton and West (2020) -
Discusses the ways that mountain building processes effect the carbon cycle
How does silicate weathering effect the carbon cycle?
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
Relationship between erosion rate and co2 flux
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
Why do mountainous areas vary in their sink/source relationship to the carbon cycle?
Different mountains underlain by different geology
Sedimentary rocks = carbon rich= carbon source
volcanic rocks = not carbon rich = carbon sink