Late Holocene. evolution of the Treskelen Peninsula (Hornsund, Spitsbergen)
The studies over sediments and landforms of the Treskelen Peninsula found them to occupy a considerably larger area and to be more varying than considered previously. A mutual relation of these features enabled to fix the successive phases of their formation, dependent on a rate of the Hyrne Glacier...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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Faculty of Geology University of Warsaw
1983
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| Online Access: | https://gq.pgi.gov.pl/agp/article/view/9421 |
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ftjgq:oai:geojournals.pgi.gov.pl:article/9421 2024-09-15T18:10:57+00:00 Late Holocene. evolution of the Treskelen Peninsula (Hornsund, Spitsbergen) Marks, Leszek 1983-12-15 application/pdf https://gq.pgi.gov.pl/agp/article/view/9421 eng eng Faculty of Geology University of Warsaw https://gq.pgi.gov.pl/agp/article/view/9421/7969 https://gq.pgi.gov.pl/agp/article/view/9421 Acta Geologica Polonica; Vol. 33 No. 1-4 (1983); 159-168 Acta Geologica Polonica; Tom 33 Nr 1-4 (1983); 159-168 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1983 ftjgq 2024-07-30T03:29:09Z The studies over sediments and landforms of the Treskelen Peninsula found them to occupy a considerably larger area and to be more varying than considered previously. A mutual relation of these features enabled to fix the successive phases of their formation, dependent on a rate of the Hyrne Glacier retreat. A critical approach to Heintz's (1953) and Birkenmajer's (1964) glacier extents and the occurrence of a glint lake at the peninsula during the Little Ice Age is also presented. Article in Journal/Newspaper Hornsund Spitsbergen Geological Quarterly |
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Open Polar |
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Geological Quarterly |
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ftjgq |
| language |
English |
| description |
The studies over sediments and landforms of the Treskelen Peninsula found them to occupy a considerably larger area and to be more varying than considered previously. A mutual relation of these features enabled to fix the successive phases of their formation, dependent on a rate of the Hyrne Glacier retreat. A critical approach to Heintz's (1953) and Birkenmajer's (1964) glacier extents and the occurrence of a glint lake at the peninsula during the Little Ice Age is also presented. |
| format |
Article in Journal/Newspaper |
| author |
Marks, Leszek |
| spellingShingle |
Marks, Leszek Late Holocene. evolution of the Treskelen Peninsula (Hornsund, Spitsbergen) |
| author_facet |
Marks, Leszek |
| author_sort |
Marks, Leszek |
| title |
Late Holocene. evolution of the Treskelen Peninsula (Hornsund, Spitsbergen) |
| title_short |
Late Holocene. evolution of the Treskelen Peninsula (Hornsund, Spitsbergen) |
| title_full |
Late Holocene. evolution of the Treskelen Peninsula (Hornsund, Spitsbergen) |
| title_fullStr |
Late Holocene. evolution of the Treskelen Peninsula (Hornsund, Spitsbergen) |
| title_full_unstemmed |
Late Holocene. evolution of the Treskelen Peninsula (Hornsund, Spitsbergen) |
| title_sort |
late holocene. evolution of the treskelen peninsula (hornsund, spitsbergen) |
| publisher |
Faculty of Geology University of Warsaw |
| publishDate |
1983 |
| url |
https://gq.pgi.gov.pl/agp/article/view/9421 |
| genre |
Hornsund Spitsbergen |
| genre_facet |
Hornsund Spitsbergen |
| op_source |
Acta Geologica Polonica; Vol. 33 No. 1-4 (1983); 159-168 Acta Geologica Polonica; Tom 33 Nr 1-4 (1983); 159-168 |
| op_relation |
https://gq.pgi.gov.pl/agp/article/view/9421/7969 https://gq.pgi.gov.pl/agp/article/view/9421 |
| _version_ |
1810448550576783360 |