*Mitsuhiro Yoshimoto1, Ryuta FURUKAWA2,3, Yoshihiro Ishizuka2, Yusuke Minami2, Masashi NAGAI4, Shuichi Hosokawa3, Ryo Honda1, Taisuke Yasuda1, Akihiko Terada5, Tatsuji Nishizawa5, Yasuhiro Ishimine6, Kenichi Arai7, Hisashi Sasaki7, Shino Naruke7, Yuko Sekiguchi3, Takahiro Yanada3, Yasuo Ishizaki8, Nobuko Kametani8, Fukashi Maeno9
(1.Mount Fuji Research Institute, Yamanashi Prefectural Government, 2.Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, 3.Japan Meteorological Agency, 4.Volcano Research Department, National Research Institute for Earth Science and Disaster Resilience, 5.Volcanic Fluid Research Center, Tokyo Institute of Technology, 6.Research and Education Center for Natural Hazards, Kagoshima University, 7.Asia Air Survey Co., Ltd., 8. Graduate School of Science and Engineering, University of Toyama, 9.Earthquake Research Institute, University of Tokyo)
Keywords:ballistic ejecta, Kusatsu-Shirane volcano, phreatic eruption
Moto-Shirane volcano, which is part of Kusatsu-Shirane volcano, erupted on 23 January 2018 after 1500 years dormancy. One parson died and 11 other people were injured by the ballistic ejecta of this phreatic eruption. We report the results of a survey on the distribution of ballistic rocks around the crater and climbing trails and ski courses on May 10 - 12, 2018 and October 23 - 25, 2018.The maximum size of the ballistic rocks was measured at a total of 191 sites and the number density of the rocks (>64mm) was measured at a total of 64 sites. Ballistic rocks of the eruption are distributed within 500 meters around the main crater and is mainly distributed from north to northeast. The maximum size of ballistic rock was 4.8 m which fell to the western crater rim, and near the main crater was 3.4 m. The flight-distance of ballistic rocks with a major axis of about 20 cm, 50 cm, 100 cm, 200 cm are 400 to 650 m, 400 m, 350 m, 150 m, respectively. It suggests that the initial velocity of ballistic rocks of each size is different.