@article{oai:niigata-u.repo.nii.ac.jp:00028185,
 author = {高浜, 信行},
 journal = {新潟大学積雪地域災害研究センター研究年報, 新潟大学積雪地域災害研究センター研究年報},
 month = {Jan},
 note = {In this paper, the author discussed the outlines of the geometrical scales and characteristics of landslide. Most of the present active landslides are secondary landslide derived from the older primary landslide deposits. It was pointed out already by many workers, but a few confusion remains yet. 1. A landslide, especially primary landslide, is the movement which is generated in a deep part, several tens to more than one hundred meters of bed rock. 2. The distance of landslide migration is relatively smaller than other mass movements; the major portion of the moving materials, in the state of fluctured and disintegrated into blocks, remains on the mountain slope in unstable condition. 3. A landslide repeatedly removed on various scales and over a long period of time …… secondary landslide. These characteristics of landslide are more crearer by recent studies about the Quaternary geohistorical examination of landslide.},
 pages = {43--52},
 title = {初生的古斯大規模地すべりについて},
 volume = {5},
 year = {1984}
}