Source of Ash Zone 1 in the North Atlantic

Geochemical evidence shows that the silicic component of the widespread Ash Zone 1 in the North Atlantic is derived from a major ignimbrite-forming eruption which occurred at the Katla caldera in southern Iceland during the transition from glacial to interglacial conditions in Younger Dryas time. Bo...

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Bibliographic Details
Published in:Bulletin of Volcanology
Main Authors: Lacasse, C., Sigurdsson, H., Jóhannesson, H., Paterne, M., Carey, S.
Format: Text
Language:unknown
Published: DigitalCommons@URI 1995
Subjects:
Online Access:https://digitalcommons.uri.edu/gsofacpubs/1081
https://doi.org/10.1007/BF00298704