Rhyolitic explosive eruptions of the Central Snake River Plain, Idaho : investigations of the Lower Cassia Mountains succession and surrounding areas
The Snake River Plain of north-western U.S.A. was the site of voluminous, bimodal, hotspot volcanism in the Miocene. Between c. 12.7-6 Ma silicic volcanism produced an association of deposits so different to typical Plinian and ignimbrite deposits elsewhere it has been termed Snake River (SR)-type....
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University of Leicester
2009
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.539840 |