P06 Groundwater and borehole strain monitoring for the prediction research of the Tonankai and Nankai earthquakes Norio Matsumoto (
[email protected]) , Naoji Koizumi, Makoto Takahashi, Yuichi Kitagawa, Satoshi Itaba, Ryu Ohtani and Tsutomu Sato Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (GSJ, AIST) 1. Nankai and Tonankai earthquakes Great earthquakes about magnitude 8 or more along the Nankai trough, off central to southwest Japan have been recognized nine times since 684 by ancient writings. Recent events were the 1944 Tonankai (M 7.9) and the 1946 Nankai (M 8.0) earthquakes along the Nankai trough after 90 - 92 years from the 1854 Ansei Tokai (M 8.4) and the 1854 Ansei Nankai (M 8.4) earthquakes. 2. Groundwater anomalies before and after the Nankai and Tonankai earthquakes Hydrological anomalies related to the past Nankai-Tonankai Preseismic hydrological anomalies at fifteen wells several days before the 1946 earthquakes were repeatedly reported in and around Shikoku Nankai earthquake were reported by Hydrographic Bureau (1948). Reported and Kii Peninsula by ancient writings. In particular, discharges anomalies were turbid groundwater and/or decreases of groundwater level or hot of hot spring stopped or decreased at the Dogo and Yunomine spring discharge. The manuscript also reported that there were legends in which hot springs after four and five of the nine Nankai-Tonankai decreases of groundwater level might happen before the occurrence of the Nankai- earthquakes, respectively. The 1946 Nankai earthquake caused Tonankai earthquakes around the wells where the preseismic anomalies were 11.2 m drop of well water level at the Dogo hot spring.