@article{oai:niigata-u.repo.nii.ac.jp:00028084, author = {大木, 靖衛 and 鈴木, 幸治 and 青木, 滋}, 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 = {Mar}, note = {Cuesta, strike ridge structurally controlled landform with gentle dip plane is recognized in the eastern foot of the Higashi-kubiki Hills 300 to 500m high, Niigata Prefecture. The studied area is composed of the middle Uwonuma formation, lower Pleistocene submarine to deltatic sedments. The main ride trending N-S direction is uprifted by the development of the Katagai-Matto anticline, in the eastern wing of which the cuesta is formed. Several large blocks of landslide with one square km wide are developed in the hills, considerably destructing cuesta geomorphology. Sharp landform of micro-graben treversing the landslide may suggest that the landslide is active one needing caution for next hazard.}, pages = {1--7}, title = {新潟県東頸城丘陵川西町南部のケスタと地すべり地形}, volume = {13}, year = {1992} }