• Rosengarten/Catinaccio mountain range with steep linear clinoforms in the upper unit that mark the progradation (from left (N) to right (S)), of the Triassic M-factory

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Next webinar

SOSW 14: The role of evaporites and other chemical sediments in Earth’s history

28/10/2026 4:00 pm (London)

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From the webinars library

The evolution of the Patagonian Ice Sheet from 35 ka to the Present Day (PATICE)

Dr Bethan Davies – Royal Holloway University of London

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