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On the Topography and Bottom Sediment of Kamogawa Submarine Canyon, Boso Peninsula
1960
The Quaternary Research (Daiyonki-Kenkyu)
The results of surveying of Kamogawa Submarine Canyon are as follows; a) Drainage system is very simple; the canyon is nearly straight in the area deeper than 300m, and is divided into three tributaries in shallower than 300m. b) Transverse profiles are V-shaped and are without terraces. c) Longitudinal profile does not show the equilibrium curve. d) In the upper stream, wall is rocky or covered thin mud sediment, and valley bottom is muddy. In the down stream, it is generally muddy. e) The
doi:10.4116/jaqua.1.228
fatcat:qgtdggds2raw5mexmtnbvzozo4