Zur letzten Eiszeit im alpinen und nordeuropäischen Raum
On the last Glaciation of the Alps and Fennoscandia. During the Pleistocene the Alps and the Fennoscandian Shield were covered several times with extensive ice caps. During the last Ice Age. the Würm or Weichsel Glaciation, the maximum extent of the glaciers occurred at the end of the Ice Age, as la...
| Published in: | Geographica Helvetica |
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| Format: | Text |
| Language: | English |
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2018
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| Online Access: | https://doi.org/10.5194/gh-42-93-1987 https://gh.copernicus.org/articles/42/93/1987/ |
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ftcopernicus:oai:publications.copernicus.org:gh44743 |
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openpolar |
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ftcopernicus:oai:publications.copernicus.org:gh44743 2023-05-15T16:11:41+02:00 Zur letzten Eiszeit im alpinen und nordeuropäischen Raum Glückert, G. 2018-01-15 application/pdf https://doi.org/10.5194/gh-42-93-1987 https://gh.copernicus.org/articles/42/93/1987/ eng eng doi:10.5194/gh-42-93-1987 https://gh.copernicus.org/articles/42/93/1987/ eISSN: 2194-8798 Text 2018 ftcopernicus https://doi.org/10.5194/gh-42-93-1987 2020-07-20T16:28:22Z On the last Glaciation of the Alps and Fennoscandia. During the Pleistocene the Alps and the Fennoscandian Shield were covered several times with extensive ice caps. During the last Ice Age. the Würm or Weichsel Glaciation, the maximum extent of the glaciers occurred at the end of the Ice Age, as late as 20.000 years ago. The main retreat phases during deglaciation were marked as distinct ice marginal zones and dated between 20,000 and 9,000 BP. Text Fennoscandia Fennoscandian Copernicus Publications: E-Journals Geographica Helvetica 42 2 93 98 |
| institution |
Open Polar |
| collection |
Copernicus Publications: E-Journals |
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ftcopernicus |
| language |
English |
| description |
On the last Glaciation of the Alps and Fennoscandia. During the Pleistocene the Alps and the Fennoscandian Shield were covered several times with extensive ice caps. During the last Ice Age. the Würm or Weichsel Glaciation, the maximum extent of the glaciers occurred at the end of the Ice Age, as late as 20.000 years ago. The main retreat phases during deglaciation were marked as distinct ice marginal zones and dated between 20,000 and 9,000 BP. |
| format |
Text |
| author |
Glückert, G. |
| spellingShingle |
Glückert, G. Zur letzten Eiszeit im alpinen und nordeuropäischen Raum |
| author_facet |
Glückert, G. |
| author_sort |
Glückert, G. |
| title |
Zur letzten Eiszeit im alpinen und nordeuropäischen Raum |
| title_short |
Zur letzten Eiszeit im alpinen und nordeuropäischen Raum |
| title_full |
Zur letzten Eiszeit im alpinen und nordeuropäischen Raum |
| title_fullStr |
Zur letzten Eiszeit im alpinen und nordeuropäischen Raum |
| title_full_unstemmed |
Zur letzten Eiszeit im alpinen und nordeuropäischen Raum |
| title_sort |
zur letzten eiszeit im alpinen und nordeuropäischen raum |
| publishDate |
2018 |
| url |
https://doi.org/10.5194/gh-42-93-1987 https://gh.copernicus.org/articles/42/93/1987/ |
| genre |
Fennoscandia Fennoscandian |
| genre_facet |
Fennoscandia Fennoscandian |
| op_source |
eISSN: 2194-8798 |
| op_relation |
doi:10.5194/gh-42-93-1987 https://gh.copernicus.org/articles/42/93/1987/ |
| op_doi |
https://doi.org/10.5194/gh-42-93-1987 |
| container_title |
Geographica Helvetica |
| container_volume |
42 |
| container_issue |
2 |
| container_start_page |
93 |
| op_container_end_page |
98 |
| _version_ |
1765996848268443648 |