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,...

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Bibliographic Details
Published in:E&G Quaternary Science Journal
Main Author: P. Woldstedt
Format: Article in Journal/Newspaper
Language:German
English
Published: Copernicus Publications 1965
Subjects:
Geology
QE1-996.5
Antarktis*
Online Access:https://doi.org/10.3285/eg.16.1.02
https://doaj.org/article/053f81566137492a81375d42e1254e43
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spelling ftdoajarticles:oai:doaj.org/article:053f81566137492a81375d42e1254e43 2023-05-15T14:15:17+02:00 Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises P. Woldstedt 1965-12-01T00:00:00Z https://doi.org/10.3285/eg.16.1.02 https://doaj.org/article/053f81566137492a81375d42e1254e43 DE EN ger eng Copernicus Publications https://www.eg-quaternary-sci-j.net/16/31/1965/egqsj-16-31-1965.pdf https://doaj.org/toc/0424-7116 https://doaj.org/toc/2199-9090 doi:10.3285/eg.16.1.02 0424-7116 2199-9090 https://doaj.org/article/053f81566137492a81375d42e1254e43 Eiszeitalter und Gegenwart, Vol 16, Pp 31-36 (1965) Geology QE1-996.5 article 1965 ftdoajarticles https://doi.org/10.3285/eg.16.1.02 2022-12-31T14:00:59Z 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". Article in Journal/Newspaper Antarktis* Directory of Open Access Journals: DOAJ Articles E&G Quaternary Science Journal 16 1 31 36
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language German
English
topic Geology
QE1-996.5
spellingShingle Geology
QE1-996.5
P. Woldstedt
Die interglazialen marinen Strände und der Aufbau des antarktischen Inlandeises
topic_facet Geology
QE1-996.5
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 Article in Journal/Newspaper
author P. Woldstedt
author_facet P. Woldstedt
author_sort P. Woldstedt
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
publisher Copernicus Publications
publishDate 1965
url https://doi.org/10.3285/eg.16.1.02
https://doaj.org/article/053f81566137492a81375d42e1254e43
genre Antarktis*
genre_facet Antarktis*
op_source Eiszeitalter und Gegenwart, Vol 16, Pp 31-36 (1965)
op_relation https://www.eg-quaternary-sci-j.net/16/31/1965/egqsj-16-31-1965.pdf
https://doaj.org/toc/0424-7116
https://doaj.org/toc/2199-9090
doi:10.3285/eg.16.1.02
0424-7116
2199-9090
https://doaj.org/article/053f81566137492a81375d42e1254e43
op_doi https://doi.org/10.3285/eg.16.1.02
container_title E&G Quaternary Science Journal
container_volume 16
container_issue 1
container_start_page 31
op_container_end_page 36
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