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Gravity Changes and Internal Processes: Some Results Obtained from Observations at Three Volcanoes

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Geodetic and Geophysical Effects Associated with Seismic and Volcanic Hazards

Part of the book series: Pageoph Topical Volumes ((PTV))

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Abstract

Temporal gravity changes provide information about mass and/or density variations within and below the volcano edifice. Three active volcanoes have been under investigation; each of them related to a plate boundary: Mayon/Luzon/Philippines, Merapi/Java/Indonesia, and Galeras/Colombia. The observed gravity changes are smaller than previously expected but significant. For the three volcanoes under investigation, and within the observation period, mainly the increase of gravity is observed, ranging from 1,000 nm−2to 1,600 nms−2. Unexpectedly, the gravity increase is confined to a rather small area with radii of 5 to 8 km around the summit.

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Jentzsch, G., Weise, A., Rey, C., Gerstenecker, C. (2004). Gravity Changes and Internal Processes: Some Results Obtained from Observations at Three Volcanoes. In: Fernández, J. (eds) Geodetic and Geophysical Effects Associated with Seismic and Volcanic Hazards. Pageoph Topical Volumes. Birkhäuser, Basel. https://doi.org/10.1007/978-3-0348-7897-5_8

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  • DOI: https://doi.org/10.1007/978-3-0348-7897-5_8

  • Publisher Name: Birkhäuser, Basel

  • Print ISBN: 978-3-7643-7044-2

  • Online ISBN: 978-3-0348-7897-5

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