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

Research output: Contribution to journalArticle

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 languageEnglish
Pages (from-to)734-743
Number of pages10
JournalGeographical Review of Japan, Series A
Volume58
Issue number11
DOIs
Publication statusPublished - Jan 1 1985
Externally publishedYes

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river
Japan
Holocene
drainage
terrace
geography
evidence
topography
Pleistocene

All Science Journal Classification (ASJC) codes

  • Geography, Planning and Development
  • Earth-Surface Processes

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 = "Kaoru Kashima",
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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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