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eros weath

Silicate chemical weathering rate versus physical erosion rate. A key observation is that in catchments with low erosion rates, chemical weathering is nearly complete (weathering rates in such catchments give a linear relationship with erosion rates) and chemical weathering rates in such ‘transport limited’ catchments do not respond to changes in climate
eros weath
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Earth Sciences at Cambridge

Saturday 22 September 2018: A one-day conference bringing together international scientists to mark 200 years since Adam Sedgwick was appointed to the Woodwardian Chair of Geology.

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