Deglaciation and drainage-pattern development in the eastern Uckermark, Brandenburg, Germany
After retreat from the Angermünde Ice Margin, the Weichselian inland ice sheet fell apart into different independently acting ice tongues in the eastern Uckermark. In this region (bordering Poland), between the Angermünde and Penkun Ice Margins only the Schönermark Intermediate Ice Margin has been d...
Main Author: | |
---|---|
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Humboldt-Universität zu Berlin
2015
|
Subjects: | |
Online Access: | http://edoc.hu-berlin.de/18452/18702 https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/18702-0 https://doi.org/10.18452/18038 |
id |
fthuberlin:oai:edoc.hu-berlin.de:18452/18702 |
---|---|
record_format |
openpolar |
spelling |
fthuberlin:oai:edoc.hu-berlin.de:18452/18702 2023-05-15T16:41:40+02:00 Deglaciation and drainage-pattern development in the eastern Uckermark, Brandenburg, Germany Deglaziation und die Entwicklung der Entwässerungsbahnen im Osten der Uckermark, Brandenburg, Deutschland Boer, Wierd Mathijs de Wutzke, Ulrich 2015-07-30 application/pdf http://edoc.hu-berlin.de/18452/18702 https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/18702-0 https://doi.org/10.18452/18038 eng eng Humboldt-Universität zu Berlin 0303-4534 http://edoc.hu-berlin.de/18452/18702 urn:nbn:de:kobv:11-110-18452/18702-0 http://dx.doi.org/10.18452/18038 Uckermark eastern Uckermark Welse South Ice Margin Welse North Ice Margin Welse Randow Oder Welse Valley Randow Valley Oder Valley Schönow-Tantow Valley Salvey Stream Ucker Ücker Angermünde Ice Margin Zichow-Golm Ice Margin Gerswalde Ice Margin Penkun Ice Margin Ucker Ice Margin Rosenthal Ice Margin Schwarze Berge Weichselian Late Weichselian Holocene glaciers ice margin push moraine nunatak glacial spillways outwash plain outwash terraces Netze-Randow Ice-Marginal Valley Schmölln- Grünz Glacier Mouth Bagemühl Terrace Meyenburg Terrace Stendell Terrace Schwedt Terrace kame terraces subglacial valleys esker varved clays dead-ice holes kettle holes dunes inland dunes arable escarpments Brandenburg Mecklenburg-Vorpommerania Germany Penkun article doc-type:article acceptedVersion 2015 fthuberlin https://doi.org/10.18452/18038 2022-08-22T13:06:00Z After retreat from the Angermünde Ice Margin, the Weichselian inland ice sheet fell apart into different independently acting ice tongues in the eastern Uckermark. In this region (bordering Poland), between the Angermünde and Penkun Ice Margins only the Schönermark Intermediate Ice Margin has been described before. This paper postulates two more ice margins: a Welse North Ice Margin and a Welse South Ice Margin. The Welse South Ice Margin is a ridge in the area northwest and south of the Welse stream (lower course) and can be followed over the villages Zehnebeck - Wendemark - Passow - Herrenhof - Berkholz. The Welse South Ice Margin is seen as a possible simultaneous continuation of the Zichow-Golm Ice Margin. Subglacial valleys developed, but unique drainage paths and sander at the Zichow-Golm Ice Margin and at the Welse South Ice Margin could not be found. In the area of Wartin - Schönow - Kunow - Hohenfelde a distinct ridge can also be seen, here named Welse North Ice Margin. It is conceived as a possible simultaneous continuation of the Gerswalde Ice Margin. An exposure in the gravel pit south of Kunow shows exemplary the different push phases of the inland ice and periglacial phenomena in this area. The main meltwater direction was from north to south and between Wartin and Blumberg a sander terrace was formed at a level of 50 - 60 m above NHN in the Randow Valley. Nach Auflösung der Angermünder Eisrandlage kam es im Weichselspätglazial zu verschiedenen unabhängig voneinander wirken- den Gletscherzungen in der östlichen Uckermark. Zwischen der Angermünder Staffel und der Penkuner Staffel ist bisher nur der Schönermarker Zwischenstaffel beschrieben worden. In dieser Arbeit werden zwei weitere Eisrandlagen postuliert: eine Welsesüdrandlage und eine Welsenordrandlage. Die Welsesüdrandlage ist ein Höhenzug im Raum nordwestlich und südlich des Welse-Flusses und ist über die Orte Zehnebeck - Wendemark - Passow - Herrenhof - Berkholz zu verfolgen. Sie wird als eine Art (und möglich zeitgleiche) Fortsetzung der ... Article in Journal/Newspaper Ice Sheet Open-Access-Publikationsserver der Humboldt-Universität: edoc-Server Rosenthal ENVELOPE(-64.283,-64.283,-64.600,-64.600) South Ice ENVELOPE(-29.867,-29.867,-81.950,-81.950) |
institution |
Open Polar |
collection |
Open-Access-Publikationsserver der Humboldt-Universität: edoc-Server |
op_collection_id |
fthuberlin |
language |
English |
topic |
Uckermark eastern Uckermark Welse South Ice Margin Welse North Ice Margin Welse Randow Oder Welse Valley Randow Valley Oder Valley Schönow-Tantow Valley Salvey Stream Ucker Ücker Angermünde Ice Margin Zichow-Golm Ice Margin Gerswalde Ice Margin Penkun Ice Margin Ucker Ice Margin Rosenthal Ice Margin Schwarze Berge Weichselian Late Weichselian Holocene glaciers ice margin push moraine nunatak glacial spillways outwash plain outwash terraces Netze-Randow Ice-Marginal Valley Schmölln- Grünz Glacier Mouth Bagemühl Terrace Meyenburg Terrace Stendell Terrace Schwedt Terrace kame terraces subglacial valleys esker varved clays dead-ice holes kettle holes dunes inland dunes arable escarpments Brandenburg Mecklenburg-Vorpommerania Germany Penkun |
spellingShingle |
Uckermark eastern Uckermark Welse South Ice Margin Welse North Ice Margin Welse Randow Oder Welse Valley Randow Valley Oder Valley Schönow-Tantow Valley Salvey Stream Ucker Ücker Angermünde Ice Margin Zichow-Golm Ice Margin Gerswalde Ice Margin Penkun Ice Margin Ucker Ice Margin Rosenthal Ice Margin Schwarze Berge Weichselian Late Weichselian Holocene glaciers ice margin push moraine nunatak glacial spillways outwash plain outwash terraces Netze-Randow Ice-Marginal Valley Schmölln- Grünz Glacier Mouth Bagemühl Terrace Meyenburg Terrace Stendell Terrace Schwedt Terrace kame terraces subglacial valleys esker varved clays dead-ice holes kettle holes dunes inland dunes arable escarpments Brandenburg Mecklenburg-Vorpommerania Germany Penkun Boer, Wierd Mathijs de Deglaciation and drainage-pattern development in the eastern Uckermark, Brandenburg, Germany |
topic_facet |
Uckermark eastern Uckermark Welse South Ice Margin Welse North Ice Margin Welse Randow Oder Welse Valley Randow Valley Oder Valley Schönow-Tantow Valley Salvey Stream Ucker Ücker Angermünde Ice Margin Zichow-Golm Ice Margin Gerswalde Ice Margin Penkun Ice Margin Ucker Ice Margin Rosenthal Ice Margin Schwarze Berge Weichselian Late Weichselian Holocene glaciers ice margin push moraine nunatak glacial spillways outwash plain outwash terraces Netze-Randow Ice-Marginal Valley Schmölln- Grünz Glacier Mouth Bagemühl Terrace Meyenburg Terrace Stendell Terrace Schwedt Terrace kame terraces subglacial valleys esker varved clays dead-ice holes kettle holes dunes inland dunes arable escarpments Brandenburg Mecklenburg-Vorpommerania Germany Penkun |
description |
After retreat from the Angermünde Ice Margin, the Weichselian inland ice sheet fell apart into different independently acting ice tongues in the eastern Uckermark. In this region (bordering Poland), between the Angermünde and Penkun Ice Margins only the Schönermark Intermediate Ice Margin has been described before. This paper postulates two more ice margins: a Welse North Ice Margin and a Welse South Ice Margin. The Welse South Ice Margin is a ridge in the area northwest and south of the Welse stream (lower course) and can be followed over the villages Zehnebeck - Wendemark - Passow - Herrenhof - Berkholz. The Welse South Ice Margin is seen as a possible simultaneous continuation of the Zichow-Golm Ice Margin. Subglacial valleys developed, but unique drainage paths and sander at the Zichow-Golm Ice Margin and at the Welse South Ice Margin could not be found. In the area of Wartin - Schönow - Kunow - Hohenfelde a distinct ridge can also be seen, here named Welse North Ice Margin. It is conceived as a possible simultaneous continuation of the Gerswalde Ice Margin. An exposure in the gravel pit south of Kunow shows exemplary the different push phases of the inland ice and periglacial phenomena in this area. The main meltwater direction was from north to south and between Wartin and Blumberg a sander terrace was formed at a level of 50 - 60 m above NHN in the Randow Valley. Nach Auflösung der Angermünder Eisrandlage kam es im Weichselspätglazial zu verschiedenen unabhängig voneinander wirken- den Gletscherzungen in der östlichen Uckermark. Zwischen der Angermünder Staffel und der Penkuner Staffel ist bisher nur der Schönermarker Zwischenstaffel beschrieben worden. In dieser Arbeit werden zwei weitere Eisrandlagen postuliert: eine Welsesüdrandlage und eine Welsenordrandlage. Die Welsesüdrandlage ist ein Höhenzug im Raum nordwestlich und südlich des Welse-Flusses und ist über die Orte Zehnebeck - Wendemark - Passow - Herrenhof - Berkholz zu verfolgen. Sie wird als eine Art (und möglich zeitgleiche) Fortsetzung der ... |
author2 |
Wutzke, Ulrich |
format |
Article in Journal/Newspaper |
author |
Boer, Wierd Mathijs de |
author_facet |
Boer, Wierd Mathijs de |
author_sort |
Boer, Wierd Mathijs de |
title |
Deglaciation and drainage-pattern development in the eastern Uckermark, Brandenburg, Germany |
title_short |
Deglaciation and drainage-pattern development in the eastern Uckermark, Brandenburg, Germany |
title_full |
Deglaciation and drainage-pattern development in the eastern Uckermark, Brandenburg, Germany |
title_fullStr |
Deglaciation and drainage-pattern development in the eastern Uckermark, Brandenburg, Germany |
title_full_unstemmed |
Deglaciation and drainage-pattern development in the eastern Uckermark, Brandenburg, Germany |
title_sort |
deglaciation and drainage-pattern development in the eastern uckermark, brandenburg, germany |
publisher |
Humboldt-Universität zu Berlin |
publishDate |
2015 |
url |
http://edoc.hu-berlin.de/18452/18702 https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/18702-0 https://doi.org/10.18452/18038 |
long_lat |
ENVELOPE(-64.283,-64.283,-64.600,-64.600) ENVELOPE(-29.867,-29.867,-81.950,-81.950) |
geographic |
Rosenthal South Ice |
geographic_facet |
Rosenthal South Ice |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
0303-4534 http://edoc.hu-berlin.de/18452/18702 urn:nbn:de:kobv:11-110-18452/18702-0 http://dx.doi.org/10.18452/18038 |
op_doi |
https://doi.org/10.18452/18038 |
_version_ |
1766032122306363392 |