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Process of dissection of initial form of large-scale pyroclastic flow deposits

Research Project

Project/Area Number 60580202
Research Category

Grant-in-Aid for General Scientific Research (C)

Allocation TypeSingle-year Grants
Research Field 自然地理学
Research InstitutionKumamoto University

Principal Investigator

YOKOYAMA Shozo  Faculty of Education , Kumamoto University, Professor, 教育学部, 教授 (40015847)

Project Period (FY) 1985 – 1987
Project Status Completed (Fiscal Year 1987)
Budget Amount *help
¥1,900,000 (Direct Cost: ¥1,900,000)
Fiscal Year 1987: ¥900,000 (Direct Cost: ¥900,000)
Fiscal Year 1986: ¥300,000 (Direct Cost: ¥300,000)
Fiscal Year 1985: ¥700,000 (Direct Cost: ¥700,000)
Keywordslarge-scale pyroclastic flow deposit / シラス / 開析過程 / 河成段丘 / シラス台地
Research Abstract

Large-scale pyroclastic flows constitute extensive depositional landform, i.e. initial form for the subsequent dissection. The initial form is considered to suffer intensive dissection immediately sfter its formation, because of loose unwelded material forming upper portion of individual deposits and absence of vegetational cover. This is strongly and typically supported by the study in the field of Ito pyroclastic flow deposit, the product of a big eruption which occurred about 22,000 yr B.P. and constitutes extensive ignimbrite plateaus around Aira caldera in Southern Kyushu, Japan.
River terraces are well preserved along rifers such as Hishida river, Kimotsuki river, Manose river in southern Kyushu, the drainage basins of which are mostly occupied by Ito pyroclastic flow deposit. Also preserved are many paleovalley networks, which were formed at the same age as the river terraces. Both river terraces and paleovalleys stand purely within the upper unwelded portion of Ito pyroclastic flow deposit, and are uniformly covered with tephra layers of several meters in thickness.
Taking it into account that the age of the oldest (bottom) tephra layer is older than some ten thousand years, the erodibility of the unwelded deposit is extremely high, and the vegetation was absent on the depositional surface immediately after its formation, it is interpreted that the river terraces and the paleovalley networks were formed very rapidly during incipient dissection in a short period immediately after he emplacement of Ito pyroclastic flow. This indicates that the formation of most of the present landforms of Ito pyroclastic flow deposit was accomplished by the concentrated incipient dissection. The time for the incipient dissection is considered to have been no more than 100 years and probably less than 10 years.

Report

(2 results)
  • 1987 Final Research Report Summary
  • 1986 Annual Research Report
  • Research Products

    (10 results)

All Other

All Publications (10 results)

  • [Publications] 渡辺一徳: 熊本大学教育学部紀要, 自然科学. 35. 57-71 (1986)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] 横山勝三: 地形. 8. 249-267 (1987)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] Shozo Yokoyama: Geological Society of America Bulletin.

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] Kazunori Watanabe: "Pyroclastic flow deposits in the western part of Kyushu Mountains" Memoirs of the Faculty of Education, Kumamoto University. No.35. 57-71 (1986)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] Shozo Yokoyama: "Large-scale pyroclastic flows and their deposits in Kyushu, Japan" Transactions, Japanese Geomorphological Union. 8. 249-267 (1987)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] Shozo Yokoyama: "Formation of river terraces in the unwelded ignimbrite field along the Hishida river, southern Kyushu, Japan" Geological society of America Bulletin.

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] 横山勝三: 火山(第2集). 30. 309 (1985)

    • Related Report
      1986 Annual Research Report
  • [Publications] 横山勝三: 拡散型大規模火砕流の流動・堆積機構に関する研究〔昭和59-60年度科学研究費補助金(一般研究C)研究成果報告書〕(渡辺一徳). 17-22 (1986)

    • Related Report
      1986 Annual Research Report
  • [Publications] 渡辺一徳: 熊本大学教育学部紀要,自然科学. 35号. 57-71 (1986)

    • Related Report
      1986 Annual Research Report
  • [Publications] 横山勝三: 1986年日本地形学連合秋季大会シンポジウム資料集. 24-45 (1986)

    • Related Report
      1986 Annual Research Report

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Published: 1987-03-31   Modified: 2016-04-21  

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