Results 11 to 20 of about 132,852 (226)

On the occurrence of phreatic eruptions at Ruapehu: statistics and probabilistic hazard forecast for ballistics [PDF]

open access: yesJournal of Applied Volcanology, 2017
Phreatic eruptions, although posing a serious threat to people in crater proximity, are often underestimated and have been comparatively understudied. The detailed eruption catalogue for Ruapehu Volcano (New Zealand) provides an exceptional opportunity ...
Gottsmann, J.   +4 more
core   +9 more sources

Short-period volcanic gas precursors to phreatic eruptions: Insights from Poás Volcano, Costa Rica

open access: yesEarth and Planetary Science Letters, 2016
Volcanic eruptions involving interaction with water are amongst the most violent and unpredictable geologic phenomena on Earth. Phreatic eruptions are exceptionally difficult to forecast by traditional geophysical techniques. Here we report on short-term
Alessandro Aiuppa   +2 more
exaly   +6 more sources

Effects of extreme rainfall on phreatic eruptions: A case study of Mt. Ontake in Japan

open access: yesAIMS Geosciences
Sometimes, natural disasters caused by volcanic eruptions have tragic consequences. Phreatic eruptions are large explosions of steam rocks and hot water caused by the sudden evaporation of water to steam. The September 2014 eruption of Mt.
Nobuo Uchida
doaj   +2 more sources

Phreatic eruptions and deformation of Ioto Island (Iwo-jima), Japan, triggered by deep magma injection

open access: yesEarth, Planets and Space, 2018
On Ioto Island (Iwo-jima), 44 phreatic eruptions have been recorded since 1889, when people began to settle there. Four of these eruptions, after the beginning of continuous observation by seismometers in 1976, were accompanied by intense seismic ...
Hideki Ueda   +2 more
doaj   +2 more sources

Phreatic and Hydrothermal Eruptions: From Overlooked to Looking Over

open access: yesBulletin of Volcanology, 2022
Over the last decade, field investigations, laboratory experiments, geophysical exploration and petrological, geochemical and numerical modelling have provided insight into the mechanisms of phreatic and hydrothermal eruptions. These eruptions are driven
C. Montanaro   +8 more
semanticscholar   +2 more sources

Fluid flow of CO2-driven geyser activity as inferred from tilt and self-potential observations of the Kibedani Geyser Japan [PDF]

open access: yesScientific Reports
We conducted multi-parameter, multi-site observations at the Kibedani Geyser, Japan, where cold spring-water eruptions (20 °C) are driven by underground CO2 pressure.
Harutou Tanabe   +2 more
doaj   +2 more sources

Geological study of phreatic eruptions

open access: yesThe Journal of the Geological Society of Japan, 2018
Phreatic (non-juvenile) eruptions are the most common type of magmatic activity on Earth. Here we review the characteristics of phreatic eruptions, which occur when overheated water is rapidly vaporized.
T. Oikawa   +3 more
semanticscholar   +3 more sources

Special issue “Towards forecasting phreatic eruptions: examples from Hakone volcano and some global equivalents”

open access: yesEarth, Planets and Space, 2019
© The Author(s) 2019. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creat iveco mmons .org/licen ses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any ...
Kazutaka Mannen   +4 more
doaj   +2 more sources

Kusatsu-Shirane volcano as a site of phreatic eruptions

open access: yesThe Journal of the Geological Society of Japan, 2018
This paper reviews the hydrothermal systems of Kusatsu-Shirane volcano, Japan, which are associated with phreatic eruptions. The existence of hydrothermal systems at this volcano is easily explained: hot springs are derived from unique thermal water that
A. Terada
semanticscholar   +3 more sources

A numerical model for precursory time sequences of the phreatic eruptions of Mt. Ontake, central Japan

open access: yesEarth, Planets and Space
The 2014 phreatic eruption of Mt. Ontake was preceded by increased volcano-tectonic (VT) seismicity, but all other types of precursors were obscure. A subsurface process leading to eruption with few precursors has yet to be identified.
Yuta Maeda
doaj   +2 more sources

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