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 |
| Published: |
PERSEE
1967
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| Subjects: | |
| Online Access: | http://www.persee.fr/doc/geo_0003-4010_1967_num_76_415_14998 https://doi.org/10.3406/geo.1967.14998 |
| Summary: | 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 |
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