@article{oai:kitami-it.repo.nii.ac.jp:00006367,
 author = {志保井, 利夫},
 issue = {2},
 journal = {北見工業大学研究報告},
 month = {Mar},
 note = {application/pdf, The outline of periglacial geomorphic phenomena in　the　Yubetsu　River　terrain and the ice-shove ridge along the beach of Okhotsk， observed in　1974，is　listed　in Table 1 as a supplement to those of 1972 and 1973.　　The periglacial geomorphic phenomena in the eastside of the Daisetsu Mountain mass are classified into （i） alpine features above 1400 m ；（ii） frost-shattering，concen trated between 300 and 400 m ； and （iii） verved clay， below 300 m.　　The precise connection between welded tuff and subsurface　cold　anomalies　still leaves some basic questions unsolved， and is left for the future study.　　The formation of an ice-shove　ridge along the beach of Okhotsk has reasonable connection with the cold climate of Kitami District and also with the occurrences of low level periglacial geomorphic phenomena there.},
 pages = {139--159, PL I-IX},
 title = {湧別川流域の周氷河地形現象 : オホーツク海岸のice-shove ridge},
 volume = {6},
 year = {1975}
}