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Jan 27 / Ron Schott

Rapid Mountain Uplift

Cerro Aconcogua, Argentine Andes

An article by Ghosh et al. in this month’s Science magazine describes a new stable isotope technique to derive paleoaltimetry data that indicate extremely rapid uplift of a region of the Bolivian Andes. They hypothesize that the data might be explained by detachment of the dense lithospheric root of the mountain belt, as previously demonstrated in the Sierra Nevada range in California.

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