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Development of palsa bog in central highland, iceland
http://hdl.handle.net/10748/3540
http://hdl.handle.net/10748/3540f41953f6-5a44-46a1-9d92-5ea700fa5041
名前 / ファイル | ライセンス | アクション |
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20005-21-012.pdf (2.0 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2010-11-30 | |||||
タイトル | ||||||
タイトル | Development of palsa bog in central highland, iceland | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
著者 |
Hirakawa, Kazuomi
× Hirakawa, Kazuomi |
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著者(ヨミ) |
ヒラカワ, カズオミ
× ヒラカワ, カズオミ |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Topography and deposits in two selected bogs with permafrost in the central highland of Iceland are described. Radiocarbon dates and tephrochronological observation reaveal that development of permafrost in the bog started around 4,000 to 3,000 years B.P., succeeding to the formation of almost all deposits of bogs during the Atlantic time. Present irregularly undulating topography with slightly hilly microlandforms and varied depressions indicates that a thermokarst resulted from the more extensive development of former permafrost. That has occurred during these several hundred years since the beginning of the Middle Ages. Typical palsa, mineral palsas in most cases, formed only in such thermokarst depressions have occurred after the partial disappearence of the extensive permafrost. | |||||
書誌情報 |
Geographical Reports of Tokyo Metropolitan University 号 21, p. 111-122, 発行日 1986 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 03868710 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00200173 | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
出版者 | ||||||
出版者 | Department of Geography, Tokyo Metropolitan University |