濃尾平野北東部における埋積浅谷の発達と地形環境の変化

書誌事項

タイトル別名
  • Landform Evolution of Shallow Buried Valleys in the Alluvial Lowland in the Northeastern Part of the Nobi Plain, Central Japan.
  • ノウビ ヘイヤ ホクトウブ ニ オケル タイセキセンコク ノ ハッタツ ト チケイ カンキョウ ノ ヘンカ

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抄録

The authors clarified the evolution of shallow buried valleys in the Nobi plain, especially in the archaeological sites of Kadomanuma and Mabikiyokote where these valleys typically develop.<br>The sites are located in the central Nobi plain near the boundary of the alluvial fan and the floodplain area; the buried shallow valleys dissect and develop on the well-developed sand layer which is related to the “upper sand layer” in the coastal region.<br>Based on close observation and the radiocarbon ages of sediments, the following results are clarified: The sand layer was dissected at ca. 3, 000-2, 400yrs BP, and shallow valleys were formed. These valleys were buried by ca. 2, 400-2, 200yrs BP.<br>In addition to these results, the authors clarified the geoenvironmental change in the region based on the geomorphic and geologic information from the surrounding areas. The geoenvironmental change in the region surrounding the Kadomanuma and Mabikiyokote sites is divided into the following four stages:<br>Stage I (3, 300-3, 000yrs BP): End of the deposition of the sand layer which is related to the “upper sand layer” in the coastal region.<br>Stage II (3, 000-2, 400yrs BP): Formation of shallow valleys on the sand layer. Flood sediments can be seen in the valleys, but the surrounding areas are in a stable condition that is characterized by humic or peaty sediments.<br>Stage III (2, 400-2, 200yrs BP): Deposition of sediments in the shallow valleys ceases at the end of this period. Environment of the surrounding area is relatively stable and there is less flooding.<br>Stage IV (2, 200yrs BP-): Active flooding occurs in the region, and the shallow valleys are buried completely.

収録刊行物

  • 第四紀研究

    第四紀研究 40 (4), 345-352, 2001

    日本第四紀学会

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