The volcaniclastic deposits of the main caldera and the evolution of the Galluccio Tuff of Roccamonfina volcano, Southern Italy
The south-west portion of the main caldera was mapped and a stratigraphy for the caldera-fill was constructed. The exact timing of formation of the main caldera is unclear; However, caldera collapse either predates or was synchronous with the eruption of the Campagnola Tuff. The proximal facies of t...
Main Author: | Cole, Paul David |
---|---|
Published: |
University of Bedfordshire
1990
|
Subjects: | |
Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.254408 |
Similar Items
-
Pyroclastic density currents associated with the 2015 phreatomagmatic eruption of the Kuchinoerabujima volcano
by: Nobuo Geshi, et al.
Published: (2018-07-01) -
Large volume explosive silicic volcanism in the Central Andes of N. Chile
by: De Silva, Shanaka Lilath
Published: (1987) -
Volcanological and Geochemical Features of the Products of Sabalan’s Last Eruption, NW Iran
by: Reza Fahim Guilany, et al.
Published: (2019-03-01) -
A geophysical study of volcanic processes at a persistently active volcano and at two calderas in a state of unrest
by: De Zeeuw-van Dalfsen, Elske
Published: (2005) -
Ignimbrite Analyses of Batur Caldera, Bali, based on 14C Dating
by: Igan S. Sutawidjaja
Published: (2014-06-01)