X Confused surface pattern SCALE OF MILES
I N A paper on arctic ice islands (Koenig et al., 1952) it was pointed out chat surface rolls are characteristic features of both the Ellesmere Ice Shelf and the floating ice islands. From this it was inferred that the ice islands almost certainly originated by calving from the Ellesmere Ice Shelf....
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.487.4916 2023-05-15T14:19:44+02:00 X Confused surface pattern SCALE OF MILES G. Hattersley-smith The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.487.4916 http://pubs.aina.ucalgary.ca/arctic/arctic10-1-32.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.487.4916 http://pubs.aina.ucalgary.ca/arctic/arctic10-1-32.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/arctic10-1-32.pdf text ftciteseerx 2016-01-08T08:16:31Z I N A paper on arctic ice islands (Koenig et al., 1952) it was pointed out chat surface rolls are characteristic features of both the Ellesmere Ice Shelf and the floating ice islands. From this it was inferred that the ice islands almost certainly originated by calving from the Ellesmere Ice Shelf. The shape of one large ice island did in fact prove its former contiguity with the ice shelf off the mouth of Markham Bay. Comparison of roll patterns of other ice islands with the roll pattern on the ice shelf may indicate the exact areas from which the ice islands have calved. It is therefore of interest to discuss the origin and evolution of these surface features. *This paper, which forms one chapter of an unpublished thesis, is published by per- Text Arctic Arctic Ellesmere Ice Shelf Ice Shelf Unknown Arctic Markham ENVELOPE(-57.358,-57.358,-64.296,-64.296) Markham Bay ENVELOPE(-71.848,-71.848,63.551,63.551) |
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Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
I N A paper on arctic ice islands (Koenig et al., 1952) it was pointed out chat surface rolls are characteristic features of both the Ellesmere Ice Shelf and the floating ice islands. From this it was inferred that the ice islands almost certainly originated by calving from the Ellesmere Ice Shelf. The shape of one large ice island did in fact prove its former contiguity with the ice shelf off the mouth of Markham Bay. Comparison of roll patterns of other ice islands with the roll pattern on the ice shelf may indicate the exact areas from which the ice islands have calved. It is therefore of interest to discuss the origin and evolution of these surface features. *This paper, which forms one chapter of an unpublished thesis, is published by per- |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
G. Hattersley-smith |
spellingShingle |
G. Hattersley-smith X Confused surface pattern SCALE OF MILES |
author_facet |
G. Hattersley-smith |
author_sort |
G. Hattersley-smith |
title |
X Confused surface pattern SCALE OF MILES |
title_short |
X Confused surface pattern SCALE OF MILES |
title_full |
X Confused surface pattern SCALE OF MILES |
title_fullStr |
X Confused surface pattern SCALE OF MILES |
title_full_unstemmed |
X Confused surface pattern SCALE OF MILES |
title_sort |
x confused surface pattern scale of miles |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.487.4916 http://pubs.aina.ucalgary.ca/arctic/arctic10-1-32.pdf |
long_lat |
ENVELOPE(-57.358,-57.358,-64.296,-64.296) ENVELOPE(-71.848,-71.848,63.551,63.551) |
geographic |
Arctic Markham Markham Bay |
geographic_facet |
Arctic Markham Markham Bay |
genre |
Arctic Arctic Ellesmere Ice Shelf Ice Shelf |
genre_facet |
Arctic Arctic Ellesmere Ice Shelf Ice Shelf |
op_source |
http://pubs.aina.ucalgary.ca/arctic/arctic10-1-32.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.487.4916 http://pubs.aina.ucalgary.ca/arctic/arctic10-1-32.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766291482825719808 |