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GEOPHYSICAL RESEARCH LETTERS,
VOL. 31,
L19605,
4 PP., 2004
doi:10.1029/2004GL020466
Coastal uplift and thrust faulting associated with the Mw = 6.8 Zemmouri (Algeria) earthquake of 21 May, 2003
UMR 7516, Institut de Physique du Globe, Strasbourg, France
Centre de Recherche en Astrophysique et Géophysique, Algiers, Algeria
Institut National de Cartographie et de Télédétection, Alger, Algeria
UMR 7516, Institut de Physique du Globe, Strasbourg, France
Abdus Salem International Center for Theoretical Physics, SAND Group, Trieste, Italy
Centre de Recherche en Astrophysique et Géophysique, Algiers, Algeria
Abdus Salem International Center for Theoretical Physics, SAND Group, Trieste, Italy
UMR 7516, Institut de Physique du Globe, Strasbourg, France
Centre de Recherche en Astrophysique et Géophysique, Algiers, Algeria
Abdus Salem International Center for Theoretical Physics, SAND Group, Trieste, Italy
Centre du Génie Parasismique, Algiers, Algeria
Institut National de Cartographie et de Télédétection, Alger, Algeria
A shoreline uplift marked by a continuous white band visible at rocky headlands occurred during the 21 May 2003 earthquake (Mw 6.8) in northern Algeria. We measured the amount of coastal uplift on a white band (emerged algae) and harbors quays between Boumerdes and Dellys. Most of measured points were collected using tape and differential GPS on rocky headlands with σ ± 0.15 m error bar (tidal prism). Leveling lines running parallel and orthogonal to the coast also provide the precise amount of uplift in the epicentral area. The uplift distribution shows an average 0.55 m along the shoreline with a maximum 0.75 m east of Boumerdes and a minimum close to 0 near Cap Djinet. The active deformation related to a thrust fault is modeled along the ∼55 km coastline. The dislocation model predicts surface slip on a N 54°E trending reverse fault, dipping 50° SE in agreement with CMT solution and coastal uplift. The faulting characteristics imply a fault geometry with possible sea bottom ruptures between 5 to 10 km offshore.
Received 6 May 2004; accepted 1 September 2004; published 8 October 2004.
Citation: (2004), Coastal uplift and thrust faulting associated with the Mw = 6.8 Zemmouri (Algeria) earthquake of 21 May, 2003, Geophys. Res. Lett., 31, L19605, doi:10.1029/2004GL020466.
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