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Volcanic inflation of Mount Hokkaido‐Komagatake, Japan, determined from a dense GPS array
Author(s) -
Iwashita Satoshi,
Takahashi Hiroaki,
Okazaki Noritoshi,
Miyamura Jun'ichi,
Kasahara Minoru,
Ichiyanagi Masayoshi,
Takahashi Ryo,
Nakagawa Mitsuhiro
Publication year - 2005
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2005gl023438
Subject(s) - volcano , geology , mount , magma , seismology , global positioning system , volcanology , magma chamber , extensional definition , summit , physical geography , tectonics , geography , telecommunications , computer science , operating system
We installed and have been operating a dense GPS array with low power consumption single frequency GPS receivers around Mount Hokkaido‐Komagatake volcano, southwestern Hokkaido, Japan, since 2000. Data were collected continuously and analyzed together with the Geographical Survey Institute of Japan's nationwide continuous GPS network data. The analysis of daily baseline length changes for two years indicate a steady inflation of the volcanic body with 10 −7 /yr extensional strain. A pressure source was estimated at 2.4 km depth beneath the summit area with a volumetric increase rate of 4.86 × 10 5 m 3 /yr. The depth of the pressure source is in good agreement with the one expected from petrological study. Integrated magma volume has reached up to 2.6 × 10 7 m 3 if the inflation rate is possibly extrapolated back to the last magmatic eruption. Our results strongly suggest a steady magma accumulation at the reservoir beneath this volcano and an increasing potential to the next eruption near future.