HR: 1330h
AN: V32B-1015    [PDF]
TI: GPS Observations in Anatahan Island, Northern Mariana Islands, Before and After the Eruption of May 10, 2003
AU: * Kato, T
EM: teru@eri.u-tokyo.ac.jp
AF: Earthq. Res. Inst., Univ. Tokyo, 1-1, Yayoi 1, Bunkyo-ku, Tokyo, 113-0032 Japan
AU: Matsushima, T
EM: mat@sevo.kyushu-u.ac.jp
AF: Inst. Seismol. Volcanol., Faculty Sci., Kyushu Univ., 5643-29, Shinzan 2, Shimabara, Nagasaki, 855-0843 Japan
AU: Nakada, S
EM: nakada@eri.u-tokyo.ac.jp
AF: Earthq. Res. Inst., Univ. Tokyo, 1-1, Yayoi 1, Bunkyo-ku, Tokyo, 113-0032 Japan
AU: Watanabe, T
EM: glposys@cc.kochi-u.ac.jp
AF: Faculty of Sci., Kochi Univ., 5-1, Akebono 2, Kochi, 780-8520 Japan
AU: Tabei, T
EM: tabei@cc.kochi-u.ac.jp
AF: Faculty of Sci., Kochi Univ., 5-1, Akebono 2, Kochi, 780-8520 Japan
AU: Camacho, J T
EM: juantcamacho@hotmail.com
AF: Emerg. Manag. Office, Capitol Hill, Saipan, MP96950 Northern Mariana Islands
AU: Chong, R
EM: rcchongemo@hotmail.com
AF: Emerg. Manag. Office, Capitol Hill, Saipan, MP96950 Northern Mariana Islands
AB: A GPS observation project in the Northern Mariana Islands started in 1992 by a joint team of Japan, US and Saipan, CNMI. We have repeated surveys in the area for several times until 2003. Previous results until 1999 showed clear evidence of back arc spreading at the Mariana Trough with velocities of 4-6cm/yr with respect to the Philippine Sea plate. There was no significant volcanic activity in this time periods. Anatahan Island erupted about three months after the latest resurvey of January 2003. In order to investigate crustal deformations of the island related to this eruption, we established a permanent site in Anatahan (ANAT). The site is located about 7km WNW of the active crater in the eastern caldera. Solar panel and a lead battery are used for power and a small PC is used for automatic data archive. A special stainless pillar was designed to set up right above the pre-occupied benchmark. We also established a new permanent site in Saipan on the roof of EMO (EMO1). For a tie to the old site in Saipan, we conducted a survey at MPLC site that have been repeatedly occupied. For a preliminary analysis, we used data sets of 1994, 1998, 1999 and January and July of 2003 for a baseline MPLC - ANAT. The obtained results suggest that Anatahan has linearly drifted to northwest relative to Saipan at least until January 2003 with a rate of about 6.5mm/yr. There was no clear long-term vertical motion of Anatahan Island until January 2003. Comparison of position of ANAT relative to MPLC between January and July, 2003 suggests about 19cm subsidence of the island. Horizontal displacement may not be significant though a few centimeters of offset toward north could be visible. Large subsidence may be due to the spouting of magma. In order to monitor the crustal deformation during the volcanic activity, we are continuing GPS tracking at the established two permanent sites for a while.
DE: 1243 Space geodetic surveys
DE: 8150 Plate boundary--general (3040)
DE: 8414 Eruption mechanisms
DE: 8419 Eruption monitoring (7280)
SC: Volcanology, Geochemistry, Petrology [V]
MN: 2003 Fall Meeting