V.—Sketch of the Geology of Ice Sound and Bell Sound, Spitzbergen

VI. Jura.—In all probability the strata which form the summit of the mountain north of Reindeer Valley in Saurie Hook belong to the Jurassic formation, which besides occupies a considerable extent on Spitzbergen, from the entrance of Ice Sound to Cape Agardh in Stor Fiord. To judge from the beds at...

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Bibliographic Details
Published in:Geological Magazine
Main Author: Nordenskiöld, A. E.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1876
Subjects:
Geology
Jura
Reindeer Valley
Spitzbergen
Online Access:http://dx.doi.org/10.1017/s0016756800154214
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800154214
id crcambridgeupr:10.1017/s0016756800154214
record_format openpolar
spelling crcambridgeupr:10.1017/s0016756800154214 2024-03-03T08:48:57+00:00 V.—Sketch of the Geology of Ice Sound and Bell Sound, Spitzbergen Nordenskiöld, A. E. 1876 http://dx.doi.org/10.1017/s0016756800154214 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800154214 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 3, issue 3, page 118-127 ISSN 0016-7568 1469-5081 Geology journal-article 1876 crcambridgeupr https://doi.org/10.1017/s0016756800154214 2024-02-08T08:29:13Z VI. Jura.—In all probability the strata which form the summit of the mountain north of Reindeer Valley in Saurie Hook belong to the Jurassic formation, which besides occupies a considerable extent on Spitzbergen, from the entrance of Ice Sound to Cape Agardh in Stor Fiord. To judge from the beds at the latter place, the only one that I know of which affords a comprehensive section of the different strata belonging to this formation, the Jurassic strata of Spitzbergen consist of— Article in Journal/Newspaper Spitzbergen Cambridge University Press Jura ENVELOPE(13.501,13.501,68.062,68.062) Reindeer Valley ENVELOPE(-36.333,-36.333,-54.300,-54.300) Geological Magazine 3 3 118 127
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Nordenskiöld, A. E.
V.—Sketch of the Geology of Ice Sound and Bell Sound, Spitzbergen
topic_facet Geology
description VI. Jura.—In all probability the strata which form the summit of the mountain north of Reindeer Valley in Saurie Hook belong to the Jurassic formation, which besides occupies a considerable extent on Spitzbergen, from the entrance of Ice Sound to Cape Agardh in Stor Fiord. To judge from the beds at the latter place, the only one that I know of which affords a comprehensive section of the different strata belonging to this formation, the Jurassic strata of Spitzbergen consist of—
format Article in Journal/Newspaper
author Nordenskiöld, A. E.
author_facet Nordenskiöld, A. E.
author_sort Nordenskiöld, A. E.
title V.—Sketch of the Geology of Ice Sound and Bell Sound, Spitzbergen
title_short V.—Sketch of the Geology of Ice Sound and Bell Sound, Spitzbergen
title_full V.—Sketch of the Geology of Ice Sound and Bell Sound, Spitzbergen
title_fullStr V.—Sketch of the Geology of Ice Sound and Bell Sound, Spitzbergen
title_full_unstemmed V.—Sketch of the Geology of Ice Sound and Bell Sound, Spitzbergen
title_sort v.—sketch of the geology of ice sound and bell sound, spitzbergen
publisher Cambridge University Press (CUP)
publishDate 1876
url http://dx.doi.org/10.1017/s0016756800154214
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800154214
long_lat ENVELOPE(13.501,13.501,68.062,68.062)
ENVELOPE(-36.333,-36.333,-54.300,-54.300)
geographic Jura
Reindeer Valley
geographic_facet Jura
Reindeer Valley
genre Spitzbergen
genre_facet Spitzbergen
op_source Geological Magazine
volume 3, issue 3, page 118-127
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800154214
container_title Geological Magazine
container_volume 3
container_issue 3
container_start_page 118
op_container_end_page 127
_version_ 1792506018660352000

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