Landform Development of Kimotsuki Plain before Deposition of Osumi Pumice Fall, Kyushu, Japan: Formation of Buried Ata Welded Ignimbrite Plateau beneath Ito Ignimbrite

Author:

TAKANAMI Shintaro1ORCID

Affiliation:

1. JSPS Research Fellow, Graduate School of Arts and Letters, Meiji University

Publisher

Tokyo Geographical Society

Subject

Earth-Surface Processes,Geology,Geophysics,Geography, Planning and Development,Global and Planetary Change

Reference59 articles.

1. Aramaki, S. (1966): Geology and pyroclastic flow deposits of the Kokubu area, Kagoshima Prefecture. Journal of the Geological Society of Japan, 75, 425-442.

2. Aramaki, S. and Ui, T. (1966): Ata pyroclastic flows and Ata caldera in southern Kyushu, Japan. Journal of the Geological Society of Japan, 72, 337-349.

3. Endo, K., Sekimoto, K. and Takano, T. (1982): Holocene stratigraphy and paleoenvironments in the Kanto Plain, in relation to the Jomon transgression. Proceedings of Institute of Natural Sciences, Nihon University, 17, 1-16.

4. Gohara, Y. and Komori, C. (1966): Quaternary formations in the Osumi Peninsula, Kagoshima Prefecture—With special reference of the pyroclastic materials—. Miscellaneous Reports of the Research Institute for Natural Resources, 54-55, 176-190.

5. Hayakawa, Y. (1991): Volcaniclastic flows and their deposits: Pyroclastic flow, surge, lahar and debris avalanche. Bulletin of the Volcanological Society of Japan, 36, 357-370.

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