2008
DOI: 10.1016/j.jvolgeores.2008.07.004
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Characterization of low-temperature pyroclastic surges that occurred in the northeastern Japan arc during the late 19th century

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Cited by 19 publications
(22 citation statements)
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“…Non-juvenile steam eruptions in Tohoku, Japan have been reported by several authors, such as Yamamoto et al (1999) for the Bandai 1888 eruption, Ohba et al (2007) for the Akita-Yakeyama 1997 eruption, andFujinawa et al (2008) for the Adatara 1900, Zao 1895, and Bandai 1888 eruptions. During the Bandai 1888 eruption event, 15-20 phreatic explosions occurred successively in one hour.…”
Section: Introductionmentioning
confidence: 93%
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“…Non-juvenile steam eruptions in Tohoku, Japan have been reported by several authors, such as Yamamoto et al (1999) for the Bandai 1888 eruption, Ohba et al (2007) for the Akita-Yakeyama 1997 eruption, andFujinawa et al (2008) for the Adatara 1900, Zao 1895, and Bandai 1888 eruptions. During the Bandai 1888 eruption event, 15-20 phreatic explosions occurred successively in one hour.…”
Section: Introductionmentioning
confidence: 93%
“…Non-juvenile steam explosions, which occur frequently in active Japanese volcanoes (Okuno, 1995), are a common style of eruption that has been causing severe volcanic hazards, particularly in proximal areas (e.g., Yamamoto et al, 1999;Fujinawa et al, 2006Fujinawa et al, , 2008. Accumulation of related volcanological and geological data is crucial for protection against such volcanic hazards.…”
Section: Introductionmentioning
confidence: 99%
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“…Phreatic eruptions pose a significant hazard to areas in proximity of the erupting crater and occasionally lead to larger-scale deadly density currents (e.g., Yamamoto et al 1999;Fujinawa et al 2006). Low-temperature pyroclastic flows (pyroclastic density currents) accompanying phreatic eruptions have been reported in Japan, Tongariro (New Zealand), and La Soufriere (Guadeloupe) (e.g., Fujinawa et al 2008;Lube et al 2014;Miura et al 2012;Nakamura and Glicken 1988;Sheridan 1980;Yamamoto et al 1999). Low-temperature pyroclastic density currents accompanying phreatic eruptions are steam driven and usually laterally directed by the phreatic explosion .…”
Section: Introductionmentioning
confidence: 98%