Authour:
Kazuo KONAGAI1, Takashi KIYOTA2, Masataka SHIGA3, Hikaru TOMITA4, Hiroki OKUDA5, Kazuhiro KAJIHARA6
1Fellow, JSCE, Professor, Institute of Urban Innovation, Yokohama National University
2Member of JSCE, Assoc. Professor, Institute of Industrial Science, University of Tokyo
3Graduate student, Institute of Urban Innovation, Yokohama National University
4Graduate student, Institute of Urban Innovation, Yokohama National University
5Graduate student, Institute of Urban Innovation, Yokohama National University
6Graduate student, Institute of Urban Innovation, Yokohama National University
Key Facts:
・ Hazard Type: Earthquake
・ Date of disaster:April 14th and 16th, 2016
・ Location of Survey:Northwestern part of Aso caldera, Kumamoto, Japan
・ Date of the field survey: April 29th to May 2nd, 2016
・ Survey tools: Unmanned aerial vehicle (UAV), GPS
Key findings:
1) A swath of ground depression extends fragmentally over about a 10 km distance in the Aso Caldera Basin.
2) Detail features of the ground depression observed by using UAV photos showed neither clear indication of soil liquefaction nor lateral offset of the ground.
Key Words:
Kumamoto Earthquake, surface ruptures, UAV photogrammetry