Thermal structure and energy of the Hakone volcano, Japan

descriptionPublicationkeyboard_double_arrow_right Article , Part of book or chapter of book 01 Jan 1978 English Publisher:Springer Science and Business Media LLCJournal:pure and applied geophysics, volume 117, pages 331-337 (issn: 0033-4553, eissn: 1420-9136,

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Authors: Jun Iriyama; Yasue Ōki;

doi: 10.1007/bf00879758 , 10.1007/978-3-0348-6525-8_29

Thermal structure and energy of the Hakone volcano, Japan

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Abstract

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. An area with extremely low heat flow is observed in the western side of the caldera showing the presence of percolating meteoric water. The hydrothermal activity is intense in the eastern half of the caldera.

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Hot Springs Research Institute of Kanagawa Prefecture
Japan

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