The volcanic response to deglaciation: Evidence from glaciated arcs and a reassessment of global eruption records
Several lines of evidence have previously been used to suggest that ice retreat after the last
glacial maximum (LGM) resulted in regionally-increased levels of volcanic activity. It has …
glacial maximum (LGM) resulted in regionally-increased levels of volcanic activity. It has …
Lateral edifice collapse and volcanic debris avalanches: A post-1980 Mount St. Helens perspective
L Siebert, ME Reid - Bulletin of Volcanology, 2023 - Springer
Abstract The 1980 eruption of Mount St. Helens was instrumental in advancing
understanding of how volcanoes work. Lateral edifice collapses and the generation of …
understanding of how volcanoes work. Lateral edifice collapses and the generation of …
Geological mapping of volcanic terrains: Discussion on concepts, facies models, scales, and resolutions from New Zealand perspective
Geological mapping in volcanic terrains is a challenging task as there needs to be input from
various geologists' groups and only limited, often ambiguous guidelines exist. Volcanoes …
various geologists' groups and only limited, often ambiguous guidelines exist. Volcanoes …
Terminology and strategy to describe large volcanic landslides and debris avalanches
B Bernard, S Takarada, SD Andrade… - … debris avalanches: From …, 2021 - Springer
Large volcanic landslides and debris avalanches are rapid, water unsaturated, gravity-
driven mass movements produced by the failure of one (or more) portion (s) of a volcanic …
driven mass movements produced by the failure of one (or more) portion (s) of a volcanic …
Factors contributing to volcano lateral collapse
Many factors can lead to volcano lateral collapse, which can produce devastating debris
avalanches that travel up to several tens to over 100 km and cover hundreds to more than a …
avalanches that travel up to several tens to over 100 km and cover hundreds to more than a …
The historical (218±14 aBP) explosive eruption of Tutupaca volcano (Southern Peru)
P Samaniego, P Valderrama, J Mariño… - Bulletin of …, 2015 - Springer
The little known Tutupaca volcano (17° 01′ S, 70° 21′ W), located at the southern end of
the Peruvian arc, is a dacitic dome complex that experienced a large explosive eruption …
the Peruvian arc, is a dacitic dome complex that experienced a large explosive eruption …
Late formative flooding of Izapa after an eruption of Tacaná volcano
Between the years of 30 bc to ad 80, during the Late Formative period, the site of Izapa was
flooded by lahars associated with an explosive eruption of the San Antonio volcano (part of …
flooded by lahars associated with an explosive eruption of the San Antonio volcano (part of …
Evidence of volcanic activity in the growth rings of trees at the Tacaná volcano, Mexico–Guatemala border
T Carlón Allende, JL Macías… - Canadian Journal of …, 2020 - cdnsciencepub.com
Volcanic activity can have a significant effect on the growth and survival of trees. The
objective of our research was to analyze the effects of the 1855–1856 eruption of the Tacaná …
objective of our research was to analyze the effects of the 1855–1856 eruption of the Tacaná …
Petrology of two contrasting Mexican volcanoes, the Chiapanecan (El Chichón) and Central American (Tacaná) volcanic belts: the result of rift- versus subduction …
JL Arce, J Walker, JD Keppie - International Geology Review, 2014 - Taylor & Francis
The alkaline El Chichón and calc-alkaline Tacaná volcanoes, located in southern Mexico,
form parts of the Chiapanecan Volcanic Belt and Central American Volcanic Arc …
form parts of the Chiapanecan Volcanic Belt and Central American Volcanic Arc …
Integrated hazards maps of the Tacaná Volcanic complex, Mexico-Guatemala: Ashfall, block-and-ash flows, and lahars
Abstract The Tacaná Volcanic Complex (TVC) is an active volcano, located on the border
between Mexico and Guatemala, in the westernmost part of the Central American Volcanic …
between Mexico and Guatemala, in the westernmost part of the Central American Volcanic …