893 Dvin earthquake
|Local date||December 28, 893|
|Areas affected||Armenia, Dvin|
|Max. intensity||IX (Violent)|
The 893 Dvin earthquake occurred on 28 December at around midnight. It had a magnitude of approximately 6 and a maximum intensity of approximately IX (Violent) on the Mercalli intensity scale. It destroyed the city of Dvin in Armenia, causing approximately 30,000 casualties. The similarity of the Arabic name for Dvin, 'Dabil' to Ardabil in northwestern Iran, has caused confusion in written records, such that the 893 Ardabil earthquake appears in several catalogues, although it is generally regarded as a false event. It was also recorded as an event during the classical period of India in several early catalogues at an unspecified capital.
Southern Armenia lies within the complex zone of continental collision between the Arabian Plate and the Eurasian Plate, which extends from the Bitlis-Zagros belt in the south to the Greater Caucasus mountains, the Apsheron-Balkan Sill and the Kopet Dag mountains in the north. In Armenia the collision is strongly oblique with a large dextral (right lateral) strike-slip component. The Sardarapat-Nakhicheven fault system is formed of four left-stepping fault segments, the Kagyzman, Sardarapat, Parackar-Dvin and Nakhichevan faults. Movement on the Parackar-Dvin segment of this fault system has been associated with a series of large earthquakes in the second half of the 9th century.
The magnitude of this earthquake has been given as 5.3 and 6, although a value of 7 or greater has been suggested. The main shock was followed by five days of damaging aftershocks. The intensity is estimated to be at least IX on the Mercalli intensity scale, with some seismologists suggesting that X would be a more appropriate value.
The city was devastated with most of its buildings destroyed, including its defensive walls, the palace of the catholicos and all the other monumental buildings; just 100 houses were left standing. The area damaged included the Artashat Plateau, where landslides were triggered. The Bishop of R'shtunik, Grigor, who was at a mountain retreat was killed with several of his followers. The death toll is variously reported as 20,000, 30,000, 70,000, 82,000, 150,000 and 180,000 in historical sources.
The earthquake had ruined the city's defenses and Dvin was taken by Muhammad ibn Abi'l-Saj, the Sajid emir of Adharbayjan, who turned it into a military base. Although the capital of Armenia was moved to Ani in 961, Dvin became prosperous once more in the 10th century following its reconstruction.
Confusion over the location and date
There has been much confusion over the location and date of this earthquake. Several Armenian sources place it clearly at Dvin in Armenia, the night after an eclipse of the moon that occurred on 27 December, 893. However, the location has been given as Ardabil in several sources, presumed to be a misreading of the Arabic name for Dvin, 'Dabil'. Almost all of the Dvin earthquake's details are repeated in these reports, although in most cases the observed lunar eclipse has become solar. One source refers to this earthquake as taking place in 'Outer India' at an unnamed capital. This report has been repeated in several other sources, with the location given as 'Daibul', near modern Karachi. It is now considered that no such earthquake occurred in India/Pakistan and that the 'well known' alleged 893 Ardabil earthquake is a phantom, despite it appearing in many modern catalogues and reference books.
In the National Geophysical Data Center earthquake database entry for this event, the date of the earthquake is variously given as March 23, March 27, December 14, December 24, with the year as 893, 894 or 895 in the quoted sources.
- Ambraseys, N.N.; Melville, C.P. (2005). A History of Persian Earthquakes. Cambridge Earth Science Series. Cambridge University Press. p. 38. ISBN 978-0-521-02187-6.
- Talebian, M.; Jackson J. (2004). "A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran" (PDF). Geophysical Journal International. Royal Astronomical Society. 156 (3): 506–526. Bibcode:2004GeoJI.156..506T. doi:10.1111/j.1365-246X.2004.02092.x. Retrieved 2 October 2011.
- Karakhanian, A.S.; Trifonov V.G.; Philip H.; Avagyan A.; Hessami K.; Jamali F.; Bayraktutan M.S.; Bagdassarian H.; Arakelian S.; Davtian V.; Adilkhanyan A. (2004). "Active faulting and natural hazards in Armenia, eastern Turkey and northwestern Iran". Tectonophysics. Elsevier. 380 (3–4): 206. Bibcode:2004Tectp.380..189K. doi:10.1016/j.tecto.2003.09.020. Retrieved 3 October 2011.
- Mkrtchian, H.K. (2000). "A major neotectonic structure within the Arabia-Eurasia collisional orogen: the Ararat-Araks conjugate fault system and its possible impact on the safety of the Metsamor nuclear power plant". In Balassanian S., Cisternas A. & Melkumyan M. Earthquake hazard and seismic risk reduction. Advances in natural and technological hazards research. 12. Springer. pp. 156–157. ISBN 978-0-7923-6390-3. Retrieved 3 October 2011.
- Hasrat'yan, M. (1995). "The medieval earthquakes of the Armenian Plateau and the historic towns of Ayrarat and Shirak (Dvin, Ani, Erevan)" (PDF). Annali di Geofisica. 38 (5–6): 719–722. Retrieved 4 October 2011.
- National Geophysical Data Center. "Comments for the Significant Earthquake". Retrieved 1 October 2011.
- Adalian, R.P. (2010). Historical Dictionary of Armenia. Historical dictionaries of Europe G – Reference, Information and Interdisciplinary Subjects. 77 (2 ed.). Scarecrow Press. pp. 287–288. ISBN 978-0-8108-6096-4. Retrieved 4 October 2011.
- Ambraseys, N.N. (2004). "Three little known early earthquakes in India". Current Science. 86 (4): 506–508. Retrieved 1 October 2011.
- Musson, R. (7 March 2001). "The ten deadliest ever earthquakes". British Geological Survey. Retrieved 1 October 2011.
- Gupta, H. (2011). Encyclopedia of Solid Earth Geophysics. Encyclopedia of Earth Sciences (2 ed.). Springer. p. 566. ISBN 978-90-481-8701-0.