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| Titel |
The 1856 Djijelli (Algeria) earthquake and tsunami: source parameters and implications for tsunami hazard in the Balearic Islands |
| VerfasserIn |
J. Roger, H. Hébert |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1561-8633
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| Digitales Dokument |
URL |
| Erschienen |
In: Natural Hazards and Earth System Science ; 8, no. 4 ; Nr. 8, no. 4 (2008-07-17), S.721-731 |
| Datensatznummer |
250005644
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| Publikation (Nr.) |
 copernicus.org/nhess-8-721-2008.pdf |
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| Zusammenfassung |
| In 1856, one (or two) destructive earthquake(s) occurred off Djijelli
(Algeria) and probably triggered a tsunami in the western Mediterranean Sea.
Following recently published results of marine campaigns along the
North-Algerian margin, a new source hypothesis for the earthquake has been
proposed, and is constituted with a set of three "en échelon" fault
segments positioned in agreement with previous studies of this earthquake
and with macroseismic data available. The geometrical parameters for this
source, in agreement with a Mw = 7.2 earthquake, display an average 40° NW dip,
a 80° strike and mean dimensions of 80 km (length) × 20 km
(width). A coseismic slip of 1.5 m is consistent with an average
convergence rate of about 5–6 mm/yr and a recurrence period of 300–400 years.
They are then introduced in the tsunami modelling code to study the
propagation across the Mediterranean Sea with a special attention towards
the Balearic Islands. A focus on the two major towns, Palma (Majorca) and
Mahon (Minorca) Harbours shows that these places are not the most exposed
(maximum water heights less than 1 m) by tsunami waves coming from this part
of the African margin. Specific amplifications revealed by modelling occur
off the southern coast of Minorca and the southeastern coast of Majorca,
mostly related to submarine bathymetric features, and are able to produce
coastal wave heights larger than 1 to 2 m as offshore Alcalfar (Minorca). A
deep submarine canyon southward Minorca leads to the amplification of waves
up to two times on both sides of the canyon. However these modellings could
not be compared to any historical observations, non-existent for these
sites. This work is a contribution to the study of tsunami hazard in western
Mediterranean based on modelling, and offers a first assessment of the
tsunami exposure in the Balearic Islands. |
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