書誌事項
- タイトル別名
-
- Holocene Advance of Rock Glaciers in Yabusawa Cirque on Mount Senjogatake, Central Japan, Inferred from the Spatial Variations in Rock Weathering Rind Thickness.
- センジョウガタケ ヤブサワ ケンコク ニ オケル レキ ノ フウカ ヒマクアツ カラ ミタ カンシンセイ ノ ガンセキ ヒョウガ リュウドウ ノ カノウセイ
この論文をさがす
抄録
Weathering rind thickness of stones was measured on a crescentic ridge and on its surrounding low ridges and slopes in Yabusawa cirque (35° 43' N, 138° 11' E, 2, 885 m a.s.l.; est. MAAT-2.3°C) in the Akaishi Mountains, central Japan. Although a numerical time scale has not been established, the crescentic ridge, which is most likely of rock glacier origin, is considered to be the oldest at the study site from weathering rind data. Meanwhile, the debrismantled valley floor is estimated to be younger in the late Holocene. This fact suggests that more recent movement of rock glacier is proposed for the occurrence on landforms of the debrismantled valley floor.
収録刊行物
-
- 地学雑誌
-
地学雑誌 111 (4), 594-600, 2002
公益社団法人 東京地学協会
- Tweet
詳細情報 詳細情報について
-
- CRID
- 1390282679206121984
-
- NII論文ID
- 10009483257
-
- NII書誌ID
- AN00322536
-
- ISSN
- 18840884
- 0022135X
-
- NDL書誌ID
- 6277527
-
- 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