| Cover Story |
| Three types of sediment movement in the Sannoudani River, Minamiaso Village, Kumamoto Prefecture, southwestern Japan |
| -- Masayuki Torii, Mitsuru Okuno, Ken-ichi Nishiyama, Yoshito Kitazono, Toshiaki Hasenaka and Shuichiro Yokota -- 64 |
| |
| Research Reports |
| Clarification of Origin and Mechanism of Tsunami-generated Turbidity Current by a Flume Experiment |
| -- Taiki Yamamoto, Fujio Masuda and Hajime Naruse -- 65-72 |
| Tsunami deposits in the estuary-fill:Holocene drill core in Minamisoma City, Fukushima Prefecture, Northeast Japan |
| -- Yuri Kakubari, Katsuichi Ota and Koichi Hoyanagi -- 73-82 |
| |
| Note |
| Flume experimental study of the knickpoint recession and incised-channel formation in Metoba River, Matsumoto |
| -- Naomi Murakoshi and Takamitsu Hatakeyama -- 83-89 |
| |
| Conference Reports |
| An opportunity to learn the progress of sedimentology from the Plio-Pleistocene Kazusa Group: a report for the Field Seminar of the Sedimentological Society of Japan, 2015 |
| -- Tetsuya Sakai -- 91-96 |
| A report on the “Sedimentology School 2015” by the Sedimentological Society of Japan: Data analysis in sedimentary petrology (Waseda University; December 2015) |
| -- Kento Nakao -- 97-100 |
| A report on the 2016 special field trip by the Japanese Association for Petroleum Technology |
| -- Hideki Kasada and Yoshiki Sakaguchi -- 101-106 |
| |
| Book Review |
| -- 107-109 |
