Les crues du Danube et la grande inondation de juin 1965
The Danube in spate, with particular reference to the great flood s of june 1965 (Abstract). — The Danube expériences floods which are very varied in kind. According to our classification the most powerful floods on the lower course of the river, below its confluence with the Save at Belgrade, are P...
Published in: | Annales de Géographie |
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Format: | Article in Journal/Newspaper |
Language: | French |
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PERSEE
1967
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Online Access: | http://www.persee.fr/doc/geo_0003-4010_1967_num_76_415_14998 https://doi.org/10.3406/geo.1967.14998 |
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ftpersee:oai:persee:article/geo_0003-4010_1967_num_76_415_14998 2023-05-15T16:02:57+02:00 Les crues du Danube et la grande inondation de juin 1965 273-287 1967 http://www.persee.fr/doc/geo_0003-4010_1967_num_76_415_14998 https://doi.org/10.3406/geo.1967.14998 fre fre PERSEE http://www.persee.fr/doc/geo_0003-4010_1962_num_71_388_16288 article 1967 ftpersee https://doi.org/10.3406/geo.1967.14998 2016-03-27T01:26:48Z The Danube in spate, with particular reference to the great flood s of june 1965 (Abstract). — The Danube expériences floods which are very varied in kind. According to our classification the most powerful floods on the lower course of the river, below its confluence with the Save at Belgrade, are Pannonian Carpato-Dinarics, and iheir grea-test sources are the Tisza and the Save. In Austria and again in Hungary, the most impressive floods, except those which owe iheir catastrophic heights to ice-jams (eg the disastrous flood of March 1838 at Budapest), belong to the Central European Alpine type. Thèse occur mainly in the Eastern Alps. The considérable flood of June 1965 was clearly 1. Et les débits records du Dniepr, puis encore plus ceux de la Dvina et la Petchora, l'emportent aussi de beaucoup sur ceux du fleuve de Budapest et d'Orsova. one of this sort This was an outstanding example of flood being caused by many factors that is it was due to whole series of heavy rains and consecutive elementary floods which overlapped and aggravated the situation Throughout almost all of its Hungarian reaches as far as its confluence with the Tisza it broke all known records that at Budapest by 040 that at Novi-Sad by 072 It burst the dykes in Slovakia and in Yugoslavian Vojvodina which brought about real national catastrophes Article in Journal/Newspaper dvina Persée: Portail de revues scientifiques en sciences humaines et sociales Spate ENVELOPE(76.102,76.102,-69.418,-69.418) Annales de Géographie 76 415 273 287 |
institution |
Open Polar |
collection |
Persée: Portail de revues scientifiques en sciences humaines et sociales |
op_collection_id |
ftpersee |
language |
French |
description |
The Danube in spate, with particular reference to the great flood s of june 1965 (Abstract). — The Danube expériences floods which are very varied in kind. According to our classification the most powerful floods on the lower course of the river, below its confluence with the Save at Belgrade, are Pannonian Carpato-Dinarics, and iheir grea-test sources are the Tisza and the Save. In Austria and again in Hungary, the most impressive floods, except those which owe iheir catastrophic heights to ice-jams (eg the disastrous flood of March 1838 at Budapest), belong to the Central European Alpine type. Thèse occur mainly in the Eastern Alps. The considérable flood of June 1965 was clearly 1. Et les débits records du Dniepr, puis encore plus ceux de la Dvina et la Petchora, l'emportent aussi de beaucoup sur ceux du fleuve de Budapest et d'Orsova. one of this sort This was an outstanding example of flood being caused by many factors that is it was due to whole series of heavy rains and consecutive elementary floods which overlapped and aggravated the situation Throughout almost all of its Hungarian reaches as far as its confluence with the Tisza it broke all known records that at Budapest by 040 that at Novi-Sad by 072 It burst the dykes in Slovakia and in Yugoslavian Vojvodina which brought about real national catastrophes |
format |
Article in Journal/Newspaper |
title |
Les crues du Danube et la grande inondation de juin 1965 |
spellingShingle |
Les crues du Danube et la grande inondation de juin 1965 |
title_short |
Les crues du Danube et la grande inondation de juin 1965 |
title_full |
Les crues du Danube et la grande inondation de juin 1965 |
title_fullStr |
Les crues du Danube et la grande inondation de juin 1965 |
title_full_unstemmed |
Les crues du Danube et la grande inondation de juin 1965 |
title_sort |
les crues du danube et la grande inondation de juin 1965 |
publisher |
PERSEE |
publishDate |
1967 |
url |
http://www.persee.fr/doc/geo_0003-4010_1967_num_76_415_14998 https://doi.org/10.3406/geo.1967.14998 |
op_coverage |
273-287 |
long_lat |
ENVELOPE(76.102,76.102,-69.418,-69.418) |
geographic |
Spate |
geographic_facet |
Spate |
genre |
dvina |
genre_facet |
dvina |
op_relation |
http://www.persee.fr/doc/geo_0003-4010_1962_num_71_388_16288 |
op_doi |
https://doi.org/10.3406/geo.1967.14998 |
container_title |
Annales de Géographie |
container_volume |
76 |
container_issue |
415 |
container_start_page |
273 |
op_container_end_page |
287 |
_version_ |
1766398616787746816 |