Holocene geomorphic development in drainage areas of River Maruyama and River Wada, Boso Peninsula, Japan.

K. Kashima

doi:10.4157/grj1984a.58.11_734

Holocene geomorphic development in drainage areas of River Maruyama and River Wada, Boso Peninsula, Japan.

K. Kashima

Research output: Contribution to journal › Article › peer-review

Abstract

Along both rivers, one Pleistocene terrace and three Holocene terrace series can be observed. Field evidence shows that the terrace topography of this area had been formed by three cyclic changes of depositional and erosional processes of both rivers in the Holocene. And those changes were presumed to be caused by rapid sea level rise in early Holocene and seismo-tectonical movement during the Holocene. -from English summary

Original language	English
Pages (from-to)	734-743
Number of pages	10
Journal	Geographical Review of Japan, Series A
Volume	58
Issue number	11
DOIs	https://doi.org/10.4157/grj1984a.58.11_734
Publication status	Published - 1985
Externally published	Yes

All Science Journal Classification (ASJC) codes

Geography, Planning and Development
Earth-Surface Processes

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10.4157/grj1984a.58.11_734

Cite this

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title = "Holocene geomorphic development in drainage areas of River Maruyama and River Wada, Boso Peninsula, Japan.",

abstract = "Along both rivers, one Pleistocene terrace and three Holocene terrace series can be observed. Field evidence shows that the terrace topography of this area had been formed by three cyclic changes of depositional and erosional processes of both rivers in the Holocene. And those changes were presumed to be caused by rapid sea level rise in early Holocene and seismo-tectonical movement during the Holocene. -from English summary",

author = "K. Kashima",

year = "1985",

doi = "10.4157/grj1984a.58.11_734",

language = "English",

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pages = "734--743",

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T1 - Holocene geomorphic development in drainage areas of River Maruyama and River Wada, Boso Peninsula, Japan.

AU - Kashima, K.

PY - 1985

Y1 - 1985

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AB - Along both rivers, one Pleistocene terrace and three Holocene terrace series can be observed. Field evidence shows that the terrace topography of this area had been formed by three cyclic changes of depositional and erosional processes of both rivers in the Holocene. And those changes were presumed to be caused by rapid sea level rise in early Holocene and seismo-tectonical movement during the Holocene. -from English summary

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JF - Geographical Review of Japan, Series A

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ER -

Holocene geomorphic development in drainage areas of River Maruyama and River Wada, Boso Peninsula, Japan.

Abstract

All Science Journal Classification (ASJC) codes

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