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- 青山 雅史
- 財団法人日本地図センター
書誌事項
- タイトル別名
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- Changes in the Mountain Permafrost Environment and their Effects on Geomorphic Change in the Japanese Alps, Central Japan, since the Last Glacial Maximum
- チュウブ サンガク チイキ ニ オケル サイシュウヒョウキキョクソウキ イコウ ノ サンガク エイキュウ トウド カンキョウ ノ ヘンドウ ト ソノ チケイ ヘンカ エ ノ エイキョウ
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The relationships between the formation of accumulation terraces and climatic changes, especially changes in the mountain permafrost environment, were investigated in the upper reaches of the Gamata River on the western side of the Yari-Hotaka Mountains, northern Japanese Alps. Optically stimulated luminescence (OSL) dating of these river terrace deposits is now in progress. The present distributions of mountain permafrost and permafrost-related landforms (e.g. rock glaciers) were investigated around Mt. Shirouma, located in the northern part of the northern Japanese Alps, and Mt. Suisyo, located in the central part of the northern Japanese Alps. The low bottom temperature of the winter snow cover (BTS <- 3 °C) and the negative mean annual ground surface temperature (MAST) on the blocky landform (protalus lobe) in the Suisyo C cirque indicate the presence of permafrost.
収録刊行物
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- 地学雑誌
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地学雑誌 115 (4), 524-530, 2006
公益社団法人 東京地学協会
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詳細情報 詳細情報について
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- CRID
- 1390282679206688128
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- NII論文ID
- 10020538940
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- NII書誌ID
- AN00322536
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- ISSN
- 18840884
- 0022135X
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- NDL書誌ID
- 8613121
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- Crossref
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- 抄録ライセンスフラグ
- 使用不可