@article{oai:kumadai.repo.nii.ac.jp:00028193,
 author = {Aramaki, Shojiro and Kitazono, Yoshito and Nakayama, Hiroshi and 鈴木, 敦巳 and Suzuki, Atsumi and Kajiwara, Mitsuhisa and 荒牧, 昭二郎 and 北園, 芳人 and Kitazono, Yoshito and 中山, 洋 and 鈴木, 敦巳 and 梶原, 光久},
 issue = {2},
 journal = {応用地質},
 month = {Jun},
 note = {application/pdf, 論文(Article), Recently, many papers and reports on landslides or slope failure have been published. However, we have few useful reports on prediction of landslides or slope failure, because there are many factors relating complicatedly with these phenomena. In some areas, typical cases of landslides are often found. Fox example, in most of landslides in Amakusa which occurred in area of tertiary sedimentary rocks sliding mass moved along thin clay layer on bed rock. Then, it was tried to draw the hazard map in Amakusa Islands concidering slope angles, dip-strike and friction angle, and we got the result that slopes of sedimentary rock could be classified into five ranks in hazard map.},
 pages = {47--58},
 title = {熊本県天草上,下島の地すべり型斜面崩壊危険図について},
 volume = {25},
 year = {1984},
 yomi = {スズキ, アツミ and キタゾノ, ヨシヒト}
}