残雪砂礫地の表面礫の移動--飯豊山における1977～1979年の測定
デジタルデータあり（科学技術振興機構）
すぐに読む
J-STAGE
全国の図書館の所蔵
国立国会図書館以外の全国の図書館の所蔵状況を表示します。
所蔵のある図書館から取寄せることが可能かなど、資料の利用方法は、ご自身が利用されるお近くの図書館へご相談ください
その他
J-STAGE
デジタルCiNii Research
検索サービスデジタル連携先のサイトで、CiNii Researchが連携している機関・データベースの所蔵状況を確認できます。
書誌情報
この資料の詳細や典拠（同じ主題の資料を指すキーワード、著者名）等を確認できます。
- 資料種別
- 記事
- 著者・編者
- 山中 英二
- 著者標目
- タイトル（掲載誌）
- 東北地理 / 東北地理学会 編
- 巻号年月日等（掲載誌）
- 32(2) 1980.04
- 掲載巻
- 32
- 掲載号
- 2
- 掲載ページ
- p81～85
- 掲載年月日（W3CDTF）
- 1980-04
- ISSN（掲載誌）
- 0387-2777
- ISSN-L（掲載誌）
- 0387-2777
- 出版事項（掲載誌）
- 仙台 : 東北地理学会
- 出版地（国名コード）
- JP
- 本文の言語コード
- jpn
- NDLC
- 対象利用者
- 一般
- 記事種別、記事分類
- 記事分類: 地球科学--気象--大気現象 ; 地球科学--地質・地史
- 所蔵機関
- 国立国会図書館
- 請求記号
- Z8-383
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館雑誌記事索引
- 書誌ID（NDLBibID）
- 2178367
- 整理区分コード
- 632
- 要約等
- Downslope stone movements were measured on Iide Mountaines from 1977 to 1979. Painted stones were set along the experimental lines on the nonvegetated and debris-mantled slope, with gradient between 21° and 36°, in a nivation hollow near the peak of Mt. Iide (Fig. 1 and Photo 1). After the first setting on October, 1977, displacements of the painted stones were measured repeatedly on September, 1978 and September, 1979.<br>These measurements revealed that each painted stone was moved 0 to 170cm for a year, and that on each experimental line the movements of the stones, including standing ones, averaged between 0.1 and 3.0cm per year (Table 1). If the stone was moved, generally speaking, the smaller the stone is, the farther likely to be moved.<br>At some part predominant in fine materials on the experimental lines, especially on the lines 4 and 5, almost all the stones moved somewhat uniformly in small range (below 5cm/yr. in general). On the other hand, some stones often displaced 10cm or more in some tiny rills across the experimental lines. Some great displacements were also found apart from the rills. Small range movements are perhaps due to solifluction, and rather large range movements are due to rill-wash and/or sheet-wash.<br>At the experimental lines 6 and 7 where crevasses often happen in snow-patch during the ablation season, the painted stones were lost except one probably because of complete destruction of the experimental lines due to snow creep. At the lines 1-5, on the contrary, stone movements dragged by snow creep have not been recognized.
- DOI
- 10.5190/tga1948.32.81
- オンライン閲覧公開範囲
- インターネット公開
- 連携機関・データベース
- 科学技術振興機構 : J-STAGE
- 要約等
- Downslope stone movements were measured on Iide Mountaines from 1977 to 1979. Painted stones were set along the experimental lines on the nonvegetated and debris-mantled slope, with gradient between 21° and 36°, in a nivation hollow near the peak of Mt. Iide (Fig. 1 and Photo 1). After the first setting on October, 1977, displacements of the painted stones were measured repeatedly on September, 1978 and September, 1979.<br>These measurements revealed that each painted stone was moved 0 to 170cm for a year, and that on each experimental line the movements of the stones, including standing ones, averaged between 0.1 and 3.0cm per year (Table 1). If the stone was moved, generally speaking, the smaller the stone is, the farther likely to be moved.<br>At some part predominant in fine materials on the experimental lines, especially on the lines 4 and 5, almost all the stones moved somewhat uniformly in small range (below 5cm/yr. in general). On the other hand, some stones often displaced 10cm or more in some tiny rills across the experimental lines. Some great displacements were also found apart from the rills. Small range movements are perhaps due to solifluction, and rather large range movements are due to rill-wash and/or sheet-wash.<br>At the experimental lines 6 and 7 where crevasses often happen in snow-patch during the ablation season, the painted stones were lost except one probably because of complete destruction of the experimental lines due to snow creep. At the lines 1-5, on the contrary, stone movements dragged by snow creep have not been recognized.
- DOI
- 10.5190/tga1948.32.81
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- Japan Link Center雑誌記事索引データベースCrossrefCiNii Articles
- 書誌ID（NDLBibID）
- 2178367
- NII論文ID
- 130001075513