Geomorphic development of the alluvial plain facing the inner Suruga Bay.

A. Matsubara

doi:10.4157/grj1984a.57.1_37

Geomorphic development of the alluvial plain facing the inner Suruga Bay.

A. Matsubara

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

5 Citations (Scopus)

Abstract

An alluvial plain develops along the head of Suruga Bay which is surrounded with Quaternary volcanoes such as Mts. Fuji, Ashitaka, and Hakone to the north, and volcanic groups in the Izu Peninsula to the east. This plain comprises the Tagata Plain, the Mishima Fan, the Kano River Delta, the Ukishimagahara and the Fuji River Fan. The aim is to clarify the stratigraphy and the distribution of the recent formations in each area, and to reconstruct their palaeo-sedimentary environments. The geomorphic development of the region during the latest Pleistocene to the Holocene is summarized.-from English summary

Original language	English
Pages (from-to)	37-56
Number of pages	20
Journal	Geographical Review of Japan
Volume	57
Issue number	1
DOIs	https://doi.org/10.4157/grj1984a.57.1_37
Publication status	Published - 1984
Externally published	Yes

ASJC Scopus subject areas

Geography, Planning and Development
Earth-Surface Processes

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abstract = "An alluvial plain develops along the head of Suruga Bay which is surrounded with Quaternary volcanoes such as Mts. Fuji, Ashitaka, and Hakone to the north, and volcanic groups in the Izu Peninsula to the east. This plain comprises the Tagata Plain, the Mishima Fan, the Kano River Delta, the Ukishimagahara and the Fuji River Fan. The aim is to clarify the stratigraphy and the distribution of the recent formations in each area, and to reconstruct their palaeo-sedimentary environments. The geomorphic development of the region during the latest Pleistocene to the Holocene is summarized.-from English summary",

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AB - An alluvial plain develops along the head of Suruga Bay which is surrounded with Quaternary volcanoes such as Mts. Fuji, Ashitaka, and Hakone to the north, and volcanic groups in the Izu Peninsula to the east. This plain comprises the Tagata Plain, the Mishima Fan, the Kano River Delta, the Ukishimagahara and the Fuji River Fan. The aim is to clarify the stratigraphy and the distribution of the recent formations in each area, and to reconstruct their palaeo-sedimentary environments. The geomorphic development of the region during the latest Pleistocene to the Holocene is summarized.-from English summary

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Geomorphic development of the alluvial plain facing the inner Suruga Bay.

Abstract

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