2009 Karonga earthquakes
|A: 2009-12-06 17:36:36|
|B: 2009-12-08 03:08:57|
|C: 2009-12-12 02:27:03|
|D: 2009-12-19 23:19:15|
|A: December 6, 2009|
|B: December 12, 2009|
|C: December 8, 2009|
|D: December 20, 2009|
|A: 19:36 (CAT, UTC+2.0)|
|A: Mw 5.8|
|B: Mw 5.9|
|C: Mw 5.5|
|D: Mw 6.0|
|A: 9.0 km|
|B: 8.0 km|
|C: 10.0 km|
|D: 6.0 km|
List of shocks
|December 6, 2009||19:36||5.8||10.16°S||33.82°E||10 km|
|December 8, 2009||05:08||5.9||9.948°S||33.878°E||8 km||1|
|December 12, 2009||04:27||5.4||9.96°S||33.88°E||10 km|
|December 19, 2009||15:02||6.0||10.108°S||33.818°E||6 km||3|
Over 1000 houses collapsed, 4 people were killed and 300 people were wounded in this earthquake sequence. The majority of the building collapse was caused by liquefaction that occurred within a shallow layer of saturated unconsolidated lake sediments along the shoreline. The locations of ground damage and liquefaction align with the fault that ruptured the earthquake.
Being in the southern East African Rift, the 100 km-long Livingstone Fault marks the limit of the Karonga Basin. The earthquakes, located at about 50 km west of the Livingstone Fault, occurred along previously unknown buried faults beneath the Quaternary unconsolidated sediments. Satellite-based geophysical investigations indicated that one of the west dipping faults which cut the Karonga Basin might have ruptured during the earthquakes. The studies also estimated a maximum slip of about 120 cm at 3–5 km depth with no evidence of dike-injection related activity associated with many earthquakes in Eastern Africa. Another study utilized aeromagnetic data to image the basement structure around the rupture area and found that multiple buried faults ruptured during the earthquake among which are the St. Mary Fault (extending over 37 km in length) and the Kaporo Fault which is 36 km long and is buried beneath Lake Malawi. Scientists have proposed that the dominance of seismicity in this part of northern Malawi may be due to the presence of pre-existing planes of weakness in the basement rocks that are favorably oriented to the tectonic stress field of the East African Rift.
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- "PAGER - M 6.0 - MALAWI". Earthquake.usgs.gov. Retrieved 2010-08-01. CS1 maint: discouraged parameter (link)
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- Hamiel, Y.; Baer, G.; Kalindekafe, L.; Dombola, K.; Chindandali, P. (October 2012). "Seismic and aseismic slip evolution and deformation associated with the 2009-2010 northern Malawi earthquake swarm, East African Rift". Geophysical Journal International. 191 (3): 898. Bibcode:2012GeoJI.191..898H. doi:10.1111/j.1365-246x.2012.05673.x. ISSN 0956-540X.
- Kolawole, F.; Atekwana, E. A.; Laó-Dávila, D. A.; Abdelsalam, M. G.; Chindandali, P. R.; Salima, J.; Kalindekafe, L. (March 2018). "Active Deformation of Malawi Rift's North Basin Hinge Zone Modulated by Reactivation of Preexisting Precambrian Shear Zone Fabric". Tectonics. 37 (3): 683–704. Bibcode:2018Tecto..37..683K. doi:10.1002/2017tc004628. ISSN 0278-7407.