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Preliminary report on a Gravimetric Survey on Volcano Hakone, Japan

Preliminary report on a Gravimetric Survey on Volcano Hakone, Japan
openaire   +1 more source

Magma-hydrothermal System of Hakone Volcano

Journal of Geography (Chigaku Zasshi), 2021
Kazutaka Mannen
exaly   +3 more sources

Eastward Inclination of Hakone Volcano and Tanna Fault

Journal of Geography (Chigaku Zasshi), 2011
It is demonstrated that the eastern side of the Tanna fault has subsided relative to the western side using digital mesh data of geographic altitudes. The estimated subsidence is concordant with accumulated displacements of the Tanna fault and the fault slip at the 1930 Kita-Izu earthquake.
Masatake Harada, Kei Odawara
exaly   +3 more sources

Numerical simulation of the hydrothermal system of Hakone volcano

Journal of Volcanology and Geothermal Research
Kazutaka Mannen
exaly   +2 more sources

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The geothermal system of the Hakone volcano

Geothermics, 1970
The isothermal map of the Hakone volcano at sea level shows that the geothermal area now 12 by 13 km in diameter is clearly related with the present volcanic activity in central cones. Four zones are recognized in the distribution of thermal waters.
Y Oki, T Hirano
openaire   +1 more source

Thermal structure and energy of the Hakone volcano, Japan

pure and applied geophysics, 1978
The thermal energy balance and the temperature profile of the Hakone volcano are considered quantitatively. Across the Hakone volcano and its surroundings the heat flow values vary from 10-1 to 103 mW/m2, due to thermal conduction and mass flow involving volcanic steam and hot spring discharge.
Jun Iriyama, Yasue Ōki
openaire   +1 more source

Post-caldera geology of Gora Region in Hakone Volcano Group, Japan

Journal of the Geological Society of Japan, 2014
Kazutaka Mannen
exaly   +3 more sources

Solid sulfur spherules near fumaroles of Hakone volcano, Japan

International Journal of Earth Sciences, 2018
Occurrence of sulfur spherules near subaerial fumaroles is relatively uncommon and their mineralogical characteristics and formation mechanisms are still incompletely understood. Yellow to greenish-gray solid sulfur spherules were observed near a fumarole that was formed in the fumarolic area (Owakudani) during the 2015 eruption of Hakone volcano ...
Jun-Ichiro Ishibashi, Kazutaka Mannen
exaly   +2 more sources

Futagoyama lava dome of Hakone volcano: an edifice formed by multiple eruptions

Journal of the Geological Society of Japan, 2010
The Futagoyama lava dome, one of the post-caldera central cones of Hakone volcano (Kanagawa, Japan), is though to have formed by a single eruption at 5 ka. However, in this study, we show that the dome formed over the course of at least three eruptions.
Mitsuru Okuno, Kazutaka Mannen
exaly   +2 more sources

PETROLOGY OF HAKONE VOLCANO AND THE ADJACENT AREAS, JAPAN

Bulletin of the Geological Society of America, 1950
Rocks of Hakone volcano and adjacent areas cover a wide range from basalt to dacite approximate to soda-rhyolite. They were erupted from various different centers during the period from older Miocene to Recent. Two different rock series are recognized, one characterized by the occurrence of monoclinic-pyroxene (a solid solution series from augite to ...
exaly   +2 more sources