A Cryopediment, Jutokuji Surface, in Sendai City

Wako, Tatsuo

doi:10.5190/tga1948.17.164

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1989

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“…It is noteworthy that evidence of involution related to the cold climate and modified gentle slopes of the Last Glacial age were discovered at the lowland, even in areas lower than the latitude of the southernmost limit (Wako, 1963b(Wako, , 1963c(Wako, , 1964(Wako, , 1965Sugawara and Takahashi, 1974;Inoue and Konuma, 1981;Ishii et al, 1987 (after ltagakl et al, 1951) area (Figs. 1 and 2).…”

Section: Introductionmentioning

confidence: 97%

Slope Modification during the Late Pleistocene in the Natori River Drainage Basin

Maung

Toyoshima

1989

Annals of The Tohoku Geographycal Asocciation

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This study tephrochronologically eludidates that front and back slopes of the terrace III (before. ca. 30,000 yr B.P.) had been modified into gentle ones in a slope declining process under the Late Pleistocene cold climatic condition even in the lowland of the mid-temperate or southern cool temperate zone, Japan and that in the active modification of slopes there existed a hiatus of 40,000 yr B.P. to 30,000 yr B.P., when a weathered horizon and gully erosion occurred.

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Section: Introductionmentioning

confidence: 97%