Enseignements de l'étude du couloir saalien de la Haute Moselle
Relations belween the Moselle piracy al Toul and the Saalian valley of the Upper Moselle. — Between Epinal and Pont-Saint-Vincent that is from the Vosges massif to the conséquent valley through the Bajocian cuesta the Moselle river flows today along its Saalian course. We can find hère an important...
Published in: | Revue Géographique de l'Est |
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Format: | Article in Journal/Newspaper |
Language: | French |
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PERSEE
1995
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Online Access: | http://www.persee.fr/doc/rgest_0035-3213_1995_num_35_3_2304 https://doi.org/10.3406/rgest.1995.2304 |
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ftpersee:oai:persee:article/rgest_0035-3213_1995_num_35_3_2304 2023-05-15T16:41:06+02:00 Enseignements de l'étude du couloir saalien de la Haute Moselle à propos de la capture à Toul 255-268 1995 http://www.persee.fr/doc/rgest_0035-3213_1995_num_35_3_2304 https://doi.org/10.3406/rgest.1995.2304 fre fre PERSEE http://www.persee.fr/doc/rgest_0035-3213_1990_num_30_3_2196 saalian terraces glaciations sedimen- tology petrography Moselle river stream-piracy pétrographie capture terrasses saaliennes sédimentologie Moselle anzapfung saalische terrassen vereisungen sedi- mentologie petrographie Mosel article 1995 ftpersee https://doi.org/10.3406/rgest.1995.2304 2016-05-08T01:42:30Z Relations belween the Moselle piracy al Toul and the Saalian valley of the Upper Moselle. — Between Epinal and Pont-Saint-Vincent that is from the Vosges massif to the conséquent valley through the Bajocian cuesta the Moselle river flows today along its Saalian course. We can find hère an important alluvial accumulation which is cut into two terraces and can be correlated with the maximum extent of the Moselle glacier : « older glaciation » or Saalian. At Golbey this accumulation takes the shape of a large proglacial fan and downstream from Thaon-les-Vosges of two stepped fluvioglacial terraces. Thèse morphological bodies show three main internal depositional units. called Fxj. Fx9 Fx. and distinctions are made on the basis of internai sedimentary structures gra- nuîometry. petrography and morphology of the pebbles. The last unit Fx corresponds to the lower Saalian terrace which appears after the incision of both Fx : and Fx-,. It is thought that the « terrasse de la Justice » and the « terrasse d'Ecrouves ». at Toul corresponding to Fx and Fx2 deposits respectively hâve flowed through the « Val de l'Ane ». Then an overflow caused the course diversion into the Meurthe river and a régressive érosion developed in the earlier valley. After that the Fx deposits took place corresponding to the retreat of the last Saalian ice-sheet. Relations between the Moselle piracy al Toul and the Saalian valley of the Upper Moselle. — Between Epinal and Pont-Saint-Vincent that is from the Vosges massif to the conséquent valley through the Bajocian cuesta the Moselle river flows today along its Saalian course. We can find hère an important alluvial accumulation which is cut into two terraces and can be correlated with the maximum extent of the Moselle glacier : « older glaciation » or Saalian. At Golbey this accumulation takes the shape of a large proglacial fan and downstream from Thaon-les-Vosges of two stepped fluvioglacial terraces. Thèse morphological bodies show three main internal depositional units. called Fxj. Fx9 Fx. and distinctions are made on the basis of internai sedimentary structures gra- nuîometry. petrography and morphology of the pebbles. The last unit Fx corresponds to the lower Saalian terrace which appears after the incision of both Fx : and Fx-,. It is thought that the « terrasse de la Justice » and the « terrasse d'Ecrouves ». at Toul corresponding to Fx and Fx2 deposits respectively hâve flowed through the « Val de l'Ane ». Then an overflow caused the course diversion into the Meurthe river and a régressive érosion developed in the earlier valley. After that the Fx deposits took place corresponding to the retreat of the last Saalian ice-sheet. Article in Journal/Newspaper Ice Sheet Persée: Portail de revues scientifiques en sciences humaines et sociales Saint-Vincent ENVELOPE(-59.515,-59.515,50.600,50.600) Revue Géographique de l'Est 35 3 255 268 |
institution |
Open Polar |
collection |
Persée: Portail de revues scientifiques en sciences humaines et sociales |
op_collection_id |
ftpersee |
language |
French |
topic |
saalian terraces glaciations sedimen- tology petrography Moselle river stream-piracy pétrographie capture terrasses saaliennes sédimentologie Moselle anzapfung saalische terrassen vereisungen sedi- mentologie petrographie Mosel |
spellingShingle |
saalian terraces glaciations sedimen- tology petrography Moselle river stream-piracy pétrographie capture terrasses saaliennes sédimentologie Moselle anzapfung saalische terrassen vereisungen sedi- mentologie petrographie Mosel Enseignements de l'étude du couloir saalien de la Haute Moselle |
topic_facet |
saalian terraces glaciations sedimen- tology petrography Moselle river stream-piracy pétrographie capture terrasses saaliennes sédimentologie Moselle anzapfung saalische terrassen vereisungen sedi- mentologie petrographie Mosel |
description |
Relations belween the Moselle piracy al Toul and the Saalian valley of the Upper Moselle. — Between Epinal and Pont-Saint-Vincent that is from the Vosges massif to the conséquent valley through the Bajocian cuesta the Moselle river flows today along its Saalian course. We can find hère an important alluvial accumulation which is cut into two terraces and can be correlated with the maximum extent of the Moselle glacier : « older glaciation » or Saalian. At Golbey this accumulation takes the shape of a large proglacial fan and downstream from Thaon-les-Vosges of two stepped fluvioglacial terraces. Thèse morphological bodies show three main internal depositional units. called Fxj. Fx9 Fx. and distinctions are made on the basis of internai sedimentary structures gra- nuîometry. petrography and morphology of the pebbles. The last unit Fx corresponds to the lower Saalian terrace which appears after the incision of both Fx : and Fx-,. It is thought that the « terrasse de la Justice » and the « terrasse d'Ecrouves ». at Toul corresponding to Fx and Fx2 deposits respectively hâve flowed through the « Val de l'Ane ». Then an overflow caused the course diversion into the Meurthe river and a régressive érosion developed in the earlier valley. After that the Fx deposits took place corresponding to the retreat of the last Saalian ice-sheet. Relations between the Moselle piracy al Toul and the Saalian valley of the Upper Moselle. — Between Epinal and Pont-Saint-Vincent that is from the Vosges massif to the conséquent valley through the Bajocian cuesta the Moselle river flows today along its Saalian course. We can find hère an important alluvial accumulation which is cut into two terraces and can be correlated with the maximum extent of the Moselle glacier : « older glaciation » or Saalian. At Golbey this accumulation takes the shape of a large proglacial fan and downstream from Thaon-les-Vosges of two stepped fluvioglacial terraces. Thèse morphological bodies show three main internal depositional units. called Fxj. Fx9 Fx. and distinctions are made on the basis of internai sedimentary structures gra- nuîometry. petrography and morphology of the pebbles. The last unit Fx corresponds to the lower Saalian terrace which appears after the incision of both Fx : and Fx-,. It is thought that the « terrasse de la Justice » and the « terrasse d'Ecrouves ». at Toul corresponding to Fx and Fx2 deposits respectively hâve flowed through the « Val de l'Ane ». Then an overflow caused the course diversion into the Meurthe river and a régressive érosion developed in the earlier valley. After that the Fx deposits took place corresponding to the retreat of the last Saalian ice-sheet. |
format |
Article in Journal/Newspaper |
title |
Enseignements de l'étude du couloir saalien de la Haute Moselle |
title_short |
Enseignements de l'étude du couloir saalien de la Haute Moselle |
title_full |
Enseignements de l'étude du couloir saalien de la Haute Moselle |
title_fullStr |
Enseignements de l'étude du couloir saalien de la Haute Moselle |
title_full_unstemmed |
Enseignements de l'étude du couloir saalien de la Haute Moselle |
title_sort |
enseignements de l'étude du couloir saalien de la haute moselle |
publisher |
PERSEE |
publishDate |
1995 |
url |
http://www.persee.fr/doc/rgest_0035-3213_1995_num_35_3_2304 https://doi.org/10.3406/rgest.1995.2304 |
op_coverage |
255-268 |
long_lat |
ENVELOPE(-59.515,-59.515,50.600,50.600) |
geographic |
Saint-Vincent |
geographic_facet |
Saint-Vincent |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
http://www.persee.fr/doc/rgest_0035-3213_1990_num_30_3_2196 |
op_doi |
https://doi.org/10.3406/rgest.1995.2304 |
container_title |
Revue Géographique de l'Est |
container_volume |
35 |
container_issue |
3 |
container_start_page |
255 |
op_container_end_page |
268 |
_version_ |
1766031541430910976 |