An Esker-Like Ridge in Process of Formation, Flatisen, Norway
A ridge of drift emerging from the snout of Flatisen resembles a small esker. It originates in a subglacial tunnel. The source of the material forming the ridge was a number of thrust planes exposed in the sides and roof of the tunnel. The main features of the tunnel and the ridge are described and...
| Published in: | Journal of Glaciology |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1958
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s0022143000023935 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023935 |
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crcambridgeupr:10.1017/s0022143000023935 |
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| record_format |
openpolar |
| spelling |
crcambridgeupr:10.1017/s0022143000023935 2024-03-03T08:46:00+00:00 An Esker-Like Ridge in Process of Formation, Flatisen, Norway Stokes, J. C. 1958 http://dx.doi.org/10.1017/s0022143000023935 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023935 en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 24, page 286-289 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1958 crcambridgeupr https://doi.org/10.1017/s0022143000023935 2024-02-08T08:32:56Z A ridge of drift emerging from the snout of Flatisen resembles a small esker. It originates in a subglacial tunnel. The source of the material forming the ridge was a number of thrust planes exposed in the sides and roof of the tunnel. The main features of the tunnel and the ridge are described and the mode of formation of the ridge suggested. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Norway Flatisen ENVELOPE(13.889,13.889,66.597,66.597) Journal of Glaciology 3 24 286 289 |
| institution |
Open Polar |
| collection |
Cambridge University Press |
| op_collection_id |
crcambridgeupr |
| language |
English |
| topic |
Earth-Surface Processes |
| spellingShingle |
Earth-Surface Processes Stokes, J. C. An Esker-Like Ridge in Process of Formation, Flatisen, Norway |
| topic_facet |
Earth-Surface Processes |
| description |
A ridge of drift emerging from the snout of Flatisen resembles a small esker. It originates in a subglacial tunnel. The source of the material forming the ridge was a number of thrust planes exposed in the sides and roof of the tunnel. The main features of the tunnel and the ridge are described and the mode of formation of the ridge suggested. |
| format |
Article in Journal/Newspaper |
| author |
Stokes, J. C. |
| author_facet |
Stokes, J. C. |
| author_sort |
Stokes, J. C. |
| title |
An Esker-Like Ridge in Process of Formation, Flatisen, Norway |
| title_short |
An Esker-Like Ridge in Process of Formation, Flatisen, Norway |
| title_full |
An Esker-Like Ridge in Process of Formation, Flatisen, Norway |
| title_fullStr |
An Esker-Like Ridge in Process of Formation, Flatisen, Norway |
| title_full_unstemmed |
An Esker-Like Ridge in Process of Formation, Flatisen, Norway |
| title_sort |
esker-like ridge in process of formation, flatisen, norway |
| publisher |
Cambridge University Press (CUP) |
| publishDate |
1958 |
| url |
http://dx.doi.org/10.1017/s0022143000023935 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023935 |
| long_lat |
ENVELOPE(13.889,13.889,66.597,66.597) |
| geographic |
Norway Flatisen |
| geographic_facet |
Norway Flatisen |
| genre |
Journal of Glaciology |
| genre_facet |
Journal of Glaciology |
| op_source |
Journal of Glaciology volume 3, issue 24, page 286-289 ISSN 0022-1430 1727-5652 |
| op_doi |
https://doi.org/10.1017/s0022143000023935 |
| container_title |
Journal of Glaciology |
| container_volume |
3 |
| container_issue |
24 |
| container_start_page |
286 |
| op_container_end_page |
289 |
| _version_ |
1792501795685138432 |