1755 Meknes earthquake
  | |
| Local date | 27 November 1755 |
|---|---|
| Magnitude | 6.5–7.0 Mw |
| Epicenter | 34°04′48″N 5°00′00″W / 34.080°N 5.000°W |
| Areas affected | Morocco |
| Max. intensity | MMI X (Extreme) |
| Casualties | 15,000 dead |
The 1755 Meknes earthquake affected Morocco on 27 November 1755. The earthquake had a moment magnitude (Mw ) estimated at between 6.5 and 7.0. It devastated the cities of Fes and Meknes—killing at least 15,000 people in both cities. The earthquake struck less than a month after another earthquake that devastated Morocco and Lisbon on 1 November. Previously regarded as an aftershock, this earthquake likely represented rupture of a separate fault due to changes in tectonic stress following their first event.
Tectonic setting
The western Eurasian–Africa plate boundary is dominated by the Gloria Fault System which lies between the Azores Triple Junction and Gibraltar Arc. The plate boundary around the Gibraltar Arc and Alboran Sea area is less defined and characterized by a broad zone of seismicity. The African and Eurasian plates converge in a N–S to NNW–SSE direction. The convergence is related to uplift and thrust tectonics along the Rif mountains.[1]
Earthquake
The shock came just days after another earthquake affected Lisbon (1 November)—it was mistakenly identified as an aftershock of that event, and misdated to 18 November. Arab sources attribute the earthquake to 27 November and mezoseismal area to Fes and Meknes. A seismic rupture was also reported but poorly documented.[2]
During a field survey of the area in 2017,
Damage
The earthquake caused great devastation in Fes and Meknes; tens of thousands were killed. It was followed by strong aftershocks that continued for months.[3] At Meknes, only a few homes remained standing but were badly damaged. Of the 16,000 Jews in the city, only 8,000 survived—an additional 4,000 Muslims perished. In Fez, 3,000 people died.[4] Significant damage occurred at the Roman archeological site Volubilis. Several kilometers south of Volubilis, Moulay Idriss Zerhoun was badly affected by a major landslide. The documentation of surface ruptured led geologists to conclude the event was localized and this was a local earthquake. Surface ruptures associated with an E–W fault at Jebel Zerhoun and Jebel Zalagh, north of Fes and Meknes were studied.[1]
See also
References
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Further reading
- Habibou, E.H.; Bouya, N.; El-Ouardi, H.; Mercier, E. (2012). "Ramp folds and fracturing in the Southern Rifian Ridges between autochthonous Atlasic domain and allochthonous formations of the Rif Cordillera (Northern Morocco)" (PDF). Mineralia Slovaca. 44: 65–70. ISSN 1338-3523.