Über erste postglaziale Bodenbildung, nach einem Vergleich der Bodenbildung in Skandinavien und im deutschen Raum

The most important soils of Scandinavia are compared with those of Germany. In Scandinavia the formation of soil can be traced back from the presence (at the Svartisen) until some 10 000 years ago, and this may be based as well on wet as on dry soils. A special feature in Skandinavia is a very soft...

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Published in:E&G Quaternary Science Journal
Main Author: Ostendorff, Eberhard
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.3285/eg.15.1.04
https://egqsj.copernicus.org/articles/15/54/1964/
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spelling ftcopernicus:oai:publications.copernicus.org:egqsj64059 2023-05-15T18:29:54+02:00 Über erste postglaziale Bodenbildung, nach einem Vergleich der Bodenbildung in Skandinavien und im deutschen Raum Ostendorff, Eberhard 2018-09-27 application/pdf https://doi.org/10.3285/eg.15.1.04 https://egqsj.copernicus.org/articles/15/54/1964/ eng eng doi:10.3285/eg.15.1.04 https://egqsj.copernicus.org/articles/15/54/1964/ eISSN: 2199-9090 Text 2018 ftcopernicus https://doi.org/10.3285/eg.15.1.04 2020-07-20T16:28:38Z The most important soils of Scandinavia are compared with those of Germany. In Scandinavia the formation of soil can be traced back from the presence (at the Svartisen) until some 10 000 years ago, and this may be based as well on wet as on dry soils. A special feature in Skandinavia is a very soft Brown Earth. Very much the same soil can be found in Germany, but only on lateglacial sediments of the late Dryas-age. Both are of almost the same age. They are alike in their character of sediment and content of carbonate. Therefore this type may probably be considered as the first important formation of soils under wood on sandy grounds in Germany. Text Svartisen Copernicus Publications: E-Journals Svartisen ENVELOPE(13.698,13.698,66.642,66.642) E&G Quaternary Science Journal 15 1 54 65
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collection Copernicus Publications: E-Journals
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language English
description The most important soils of Scandinavia are compared with those of Germany. In Scandinavia the formation of soil can be traced back from the presence (at the Svartisen) until some 10 000 years ago, and this may be based as well on wet as on dry soils. A special feature in Skandinavia is a very soft Brown Earth. Very much the same soil can be found in Germany, but only on lateglacial sediments of the late Dryas-age. Both are of almost the same age. They are alike in their character of sediment and content of carbonate. Therefore this type may probably be considered as the first important formation of soils under wood on sandy grounds in Germany.
format Text
author Ostendorff, Eberhard
spellingShingle Ostendorff, Eberhard
Über erste postglaziale Bodenbildung, nach einem Vergleich der Bodenbildung in Skandinavien und im deutschen Raum
author_facet Ostendorff, Eberhard
author_sort Ostendorff, Eberhard
title Über erste postglaziale Bodenbildung, nach einem Vergleich der Bodenbildung in Skandinavien und im deutschen Raum
title_short Über erste postglaziale Bodenbildung, nach einem Vergleich der Bodenbildung in Skandinavien und im deutschen Raum
title_full Über erste postglaziale Bodenbildung, nach einem Vergleich der Bodenbildung in Skandinavien und im deutschen Raum
title_fullStr Über erste postglaziale Bodenbildung, nach einem Vergleich der Bodenbildung in Skandinavien und im deutschen Raum
title_full_unstemmed Über erste postglaziale Bodenbildung, nach einem Vergleich der Bodenbildung in Skandinavien und im deutschen Raum
title_sort über erste postglaziale bodenbildung, nach einem vergleich der bodenbildung in skandinavien und im deutschen raum
publishDate 2018
url https://doi.org/10.3285/eg.15.1.04
https://egqsj.copernicus.org/articles/15/54/1964/
long_lat ENVELOPE(13.698,13.698,66.642,66.642)
geographic Svartisen
geographic_facet Svartisen
genre Svartisen
genre_facet Svartisen
op_source eISSN: 2199-9090
op_relation doi:10.3285/eg.15.1.04
https://egqsj.copernicus.org/articles/15/54/1964/
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container_title E&G Quaternary Science Journal
container_volume 15
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container_start_page 54
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