飛騨山脈白馬岳東面の岩岳期モレーン上における立山Ｅテフラの発見とその意義

• 川澄 隆明

  東京都立三宅高等学校

書誌事項

タイトル別名

• Chronological Significance of Tateyama E Tephra on the Lowest Moraine (Iwatake Stage) on the Eastern Side of Mt. Shiroumadake, Hida Range, Central Japan
• ヒダ サンミャク シロウマダケ ヒガシメン ノ イワタケキ モレーン ジョウ ニ オケル タテヤマ Eテフラ ノ ハッケン ト ソノ イギ

抄録

 The timing of the maximum glacial advance during the last glacial period has been determined on the basis of stratigraphic relationships between marker tephras and ridges that form the lowest moraine of Mt. Shiroumadake (2,932 m), at the northern part of the Hida Range in central Japan, extending in the north-south direction for approximately 100 km. The glacier attained its maximum advance in early MIS 4 immediately before the fall of Tateyama E tephra (Tt-E, 70 MIS ka) and retreated with repetitive stagnation. When compared to published information on the northwest and southern parts of the range, glacial fluctuations on Mt. Shiroumadake and other high mountains were common around the fall of Tt-E. The glaciers appear to have attained their maximum advances synchronously in early MIS 4 over the Hida Range.

収録刊行物

• 地学雑誌

  地学雑誌 118 (4), 717-725, 2009

  公益社団法人 東京地学協会

キーワード

• 飛騨山脈
• 白馬岳
• 最終氷期
• 氷河最拡大
• 立山Eテフラ

詳細情報

• CRID: 1390282679207443712
• NII論文ID: 10030366226
• NII書誌ID: AN00322536
• DOI: 10.5026/jgeography.118.717
• ISSN: 18840884
• ISSN: 0022135X
• NDL書誌ID: 10415123
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I10415123
• 本文言語コード: ja
• データソース種別:
  • JaLC
  • NDL
  • Crossref
  • CiNii Articles
• 抄録ライセンスフラグ: 使用不可