Caldera Inflation
Caldera Inflation is a geophysical phenomenon characterized by the gradual uplift or swelling of a caldera floor due to the accumulation of magma or hydrothermal fluids in a underlying reservoir, distinguishing it from other forms of volcanic deformation by its spatial scale and association with resurgence rather than immediate eruptive activity.
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Experimental studies of collapse calderas
G. J. Ablay, L. T. REDSHAW, R. S. J. Sparks · Journal of the Geological Society · 1994 · 202 citations
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United States Geological Survey
Reston, United States
14 h-index
40 publications
2.7K citations
University of Iceland
Reykjavik, Iceland
8 h-index
21 publications
932 citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
7 h-index
31 publications
2.5K citations

University of Alaska Fairbanks
Fairbanks, United States
7 h-index
10 publications
434 citations
Cascades Volcano Observatory
Vancouver, United States
5 h-index
12 publications
669 citations
California Institute of Technology
Pasadena, United States
5 h-index
8 publications
181 citations
Stanford University
Stanford, United States
5 h-index
10 publications
268 citations

University of Bristol
Bristol, United Kingdom
4 h-index
12 publications
1.1K citations
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19 publications · 991 citations
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JGR · 14 publications · 1.1K citations
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12 publications · 772 citations
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9 publications · 334 citations
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5 publications · 151 citations
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