The Great Tunisian Flood
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Abstract
In the autumn of 1969, unusual meteorological conditions over Europe and northern Africa caused an enormous persistent desert storm in Tunisia and eastern Algeria. Poorly developed drainage patterns and gypsum-encrusted surfaces of these desert regions intensified effects of the storm and contributed to the heavy loss of life and property. Destruction of Roman bridges suggests that such storms may have recurrence probabilities of several thousands of years. The event also suggests that, although desert storms are less frequent than those of temperate regions, they can be similar in magnitude.
Study Area
Publication type | Article |
---|---|
Publication Subtype | Journal Article |
Title | The Great Tunisian Flood |
Series title | Journal of Research of the U.S. Geological Survey |
Volume | 1 |
Issue | 1 |
Year Published | 1973 |
Language | English |
Publisher | U.S. Geological Survey |
Publisher location | Reston, VA |
Description | 4 p. |
First page | 121 |
Last page | 124 |
Country | Algeria, Tunisia |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |