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What is rheology in geology?

Updated: 11/1/2022
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13y ago

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Rheology in a geological context deals with the flow / deformation of the extremely viscous fluids that compose the asthenosphere and mantle (fluid in this context means that it flows but only on a geological time scale where strain rates are measured in metres / million years).

In fact a better way may be to think of them as soft solids but that only act like they are soft way because of the very high temperatures and pressures they are under inside the earth.

For more information on Rheology and rheology in a geological / geophysical context, please see the related link.

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The difference is in the rheology of the rocks, or, how they react under pressure. The lithosphere exhibits brittle rheology which means it will break or crack while the asthenosphere exhibits ductile rheology meaning it will deform or "flow in the solid state" not unlike silly putty. The lithosphere includes the crust and the upper part of the mantle and is approximately the upper 100km of the Earth.


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