Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises
The interglacial marine beaches (Sicilian, Milazzian etc.) are mostly explained as signs of ancient higher ocean levels. But where we can prove the height of ancient ocean levels, this is not very different from the present one. The ancient beaches cannot be explained by sinking of the ocean level,...
| Published in: | E&G Quaternary Science Journal |
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| Format: | Text |
| Language: | English |
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2018
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| Online Access: | https://doi.org/10.3285/eg.16.1.02 https://egqsj.copernicus.org/articles/16/31/1965/ |
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ftcopernicus:oai:publications.copernicus.org:egqsj64039 |
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openpolar |
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ftcopernicus:oai:publications.copernicus.org:egqsj64039 2023-05-15T14:14:57+02:00 Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises Woldstedt, Paul 2018-09-27 application/pdf https://doi.org/10.3285/eg.16.1.02 https://egqsj.copernicus.org/articles/16/31/1965/ eng eng doi:10.3285/eg.16.1.02 https://egqsj.copernicus.org/articles/16/31/1965/ eISSN: 2199-9090 Text 2018 ftcopernicus https://doi.org/10.3285/eg.16.1.02 2020-07-20T16:28:36Z The interglacial marine beaches (Sicilian, Milazzian etc.) are mostly explained as signs of ancient higher ocean levels. But where we can prove the height of ancient ocean levels, this is not very different from the present one. The ancient beaches cannot be explained by sinking of the ocean level, but only by rise of the continents. Thus they are really „raised beaches". Text Antarktis* Copernicus Publications: E-Journals E&G Quaternary Science Journal 16 1 31 36 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
| language |
English |
| description |
The interglacial marine beaches (Sicilian, Milazzian etc.) are mostly explained as signs of ancient higher ocean levels. But where we can prove the height of ancient ocean levels, this is not very different from the present one. The ancient beaches cannot be explained by sinking of the ocean level, but only by rise of the continents. Thus they are really „raised beaches". |
| format |
Text |
| author |
Woldstedt, Paul |
| spellingShingle |
Woldstedt, Paul Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises |
| author_facet |
Woldstedt, Paul |
| author_sort |
Woldstedt, Paul |
| title |
Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises |
| title_short |
Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises |
| title_full |
Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises |
| title_fullStr |
Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises |
| title_full_unstemmed |
Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises |
| title_sort |
die interglazialen marinen strände und der aufbau des antarktischen inlandeises |
| publishDate |
2018 |
| url |
https://doi.org/10.3285/eg.16.1.02 https://egqsj.copernicus.org/articles/16/31/1965/ |
| genre |
Antarktis* |
| genre_facet |
Antarktis* |
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eISSN: 2199-9090 |
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doi:10.3285/eg.16.1.02 https://egqsj.copernicus.org/articles/16/31/1965/ |
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https://doi.org/10.3285/eg.16.1.02 |
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E&G Quaternary Science Journal |
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16 |
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1 |
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31 |
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36 |
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1766287299964829696 |