XXVII.—Stratigraphical Observations in the Stor Fjord Region of Spitsbergen

The Stor Fjord is the great bight which is situated on the eastern side of the mainland of Spitsbergen, and separates it from the large Barents and Edge Islands which lie farther east (see map, fig. 1). It is widest towards the south, the distance between the South Cape of Spitsbergen and Negro Poin...

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Published in:Transactions of the Royal Society of Edinburgh
Main Author: Tyrrell, G. W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1934
Subjects:
Online Access:https://doi.org/10.1017/s0080456800016914
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0080456800016914
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author Tyrrell, G. W.
author_facet Tyrrell, G. W.
author_sort Tyrrell, G. W.
collection Unknown
container_issue 3
container_start_page 675
container_title Transactions of the Royal Society of Edinburgh
container_volume 57
description The Stor Fjord is the great bight which is situated on the eastern side of the mainland of Spitsbergen, and separates it from the large Barents and Edge Islands which lie farther east (see map, fig. 1). It is widest towards the south, the distance between the South Cape of Spitsbergen and Negro Point on Edge Island being 107 miles. At its northern end the Stor Fjord narrows considerably and terminates in Heley (or Helis) Sound, which connects it with the Barents Sea by way of Olga Strait.
format Article in Journal/Newspaper
genre Barents Sea
Edge Island
Spitsbergen
genre_facet Barents Sea
Edge Island
Spitsbergen
geographic Barents Sea
South Cape
geographic_facet Barents Sea
South Cape
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institution Open Polar
language English
long_lat ENVELOPE(-84.449,-84.449,76.302,76.302)
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op_doi https://doi.org/10.1017/s0080456800016914
op_rights https://www.cambridge.org/core/terms
op_source Transactions of the Royal Society of Edinburgh
volume 57, issue 3, page 675-697
ISSN 0080-4568 2053-5945
publishDate 1934
publisher Cambridge University Press (CUP)
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spelling crcambridgeupr:10.1017/s0080456800016914 2026-04-26T13:57:56+00:00 XXVII.—Stratigraphical Observations in the Stor Fjord Region of Spitsbergen Tyrrell, G. W. 1934 https://doi.org/10.1017/s0080456800016914 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0080456800016914 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Transactions of the Royal Society of Edinburgh volume 57, issue 3, page 675-697 ISSN 0080-4568 2053-5945 journal-article 1934 crcambridgeupr https://doi.org/10.1017/s0080456800016914 2026-04-06T23:52:21Z The Stor Fjord is the great bight which is situated on the eastern side of the mainland of Spitsbergen, and separates it from the large Barents and Edge Islands which lie farther east (see map, fig. 1). It is widest towards the south, the distance between the South Cape of Spitsbergen and Negro Point on Edge Island being 107 miles. At its northern end the Stor Fjord narrows considerably and terminates in Heley (or Helis) Sound, which connects it with the Barents Sea by way of Olga Strait. Article in Journal/Newspaper Barents Sea Edge Island Spitsbergen Unknown Barents Sea South Cape ENVELOPE(-84.449,-84.449,76.302,76.302) Transactions of the Royal Society of Edinburgh 57 3 675 697
spellingShingle Tyrrell, G. W.
XXVII.—Stratigraphical Observations in the Stor Fjord Region of Spitsbergen
title XXVII.—Stratigraphical Observations in the Stor Fjord Region of Spitsbergen
title_full XXVII.—Stratigraphical Observations in the Stor Fjord Region of Spitsbergen
title_fullStr XXVII.—Stratigraphical Observations in the Stor Fjord Region of Spitsbergen
title_full_unstemmed XXVII.—Stratigraphical Observations in the Stor Fjord Region of Spitsbergen
title_short XXVII.—Stratigraphical Observations in the Stor Fjord Region of Spitsbergen
title_sort xxvii.—stratigraphical observations in the stor fjord region of spitsbergen
url https://doi.org/10.1017/s0080456800016914
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0080456800016914