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Contents

   



(Top)
 


1 Tectonic summary  





2 Details  





3 See also  





4 References  





5 External links  














2008 Lake Kivu earthquake






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Coordinates: 2°1850S 28°5346E / 2.314°S 28.896°E / -2.314; 28.896
 

From Wikipedia, the free encyclopedia
 


2008 Lake Kivu earthquake
UTC time2008-02-03 07:34:11
ISC event13213409
USGS-ANSSComCat
Local dateFebruary 3, 2008 (2008-02-03)
Local time09:34:11 CAT
Magnitude5.9 Mw
Depth10 km (6 mi)
Epicenter2°18′50S 28°53′46E / 2.314°S 28.896°E / -2.314; 28.896
TypeNormal
Areas affectedRwanda
DR Congo
Total damageSevere [1]
Max. intensityMMI VIII (Severe)
Casualties44 dead, 349+ injured [2][3]

The 2008 Lake Kivu earthquake shook several countries in Africa's Great Lakes region at 07:34:12 (GMT) on February 3. It measured 5.9 on the moment magnitude scale. The epicentre was 20 kilometres (12 mi) north of BukavuatLake Kivu in the Democratic Republic of Congo.[4]

Tectonic summary

[edit]

According to the USGS,[5]

The earthquake occurred in the Western Rift of the East African rift system. The East African rift system is a diffuse, approximately 3000-km-long, zone of crustal extension that passes through eastern Africa from Djibouti and Eritrea on the north to Malawi on the south and that constitutes the boundary between the Africa plate on the west and the Somalia plate on the east. At the earthquake's latitude, the Africa and Somalia plates are spreading apart at a rate of about four millimeters per year. The earthquake occurred near Lake Kivu, the basin of which was created by normal faulting similar to that which produced the February 3 earthquake. The largest earthquake to have occurred in the rift system since 1900 had a magnitude of about 7.6. The epicenter of the February 3, 2008, earthquake is within several tens of kilometres (miles) of the epicenter of a magnitude 6.2 earthquake that killed two people in Goma in October 2002. Earthquakes within the East African rift system occur as the result of both normal faulting and strike-slip faulting.

Details

[edit]

At least 25 people were confirmed dead in Rwanda, with a further 200 seriously injured. Ten people were killed when a church collapsed in the Rusizi DistrictofWestern Province in Rwanda, according to Rwanda radio.[6] In the Democratic Republic of Congo at least 5 died and 149 were seriously injured.[7]

See also

[edit]

References

[edit]
  1. ^ National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Database (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K
  • ^ "Earthquakes kill 39 in Rwanda, Congo - CNN.com". Archived from the original on September 26, 2008.
  • ^ "Deaths from Earthquakes in 2008". Archived from the original on 2015-10-03. Retrieved 2014-02-13.
  • ^ "Deadly earthquake shakes Rwanda". BBC Online. 2008-02-03. Archived from the original on 4 February 2008. Retrieved 2008-02-03.
  • ^ "Magnitude 5.9 - LAC KIVU REGION, DEM. REP. OF THE CONGO". earthquake.usgs.gov. Archived from the original on February 6, 2008.
  • ^ "23 dead in Rwanda earthquake: radio". Australian Broadcasting Corporation. 2008-02-03. Archived from the original on 6 February 2008. Retrieved 2008-02-03.
  • ^ "Death toll from Rwanda, Congo quakes hits 30". Reuters. 2008-02-03. Archived from the original on 13 February 2008. Retrieved 2008-02-03.
  • [edit]


    Retrieved from "https://en.wikipedia.org/w/index.php?title=2008_Lake_Kivu_earthquake&oldid=1212092050"

    Categories: 
    2008 in Rwanda
    2008 earthquakes
    2008 in the Democratic Republic of the Congo
    Earthquakes in Africa
    Natural disasters in Rwanda
    Earthquakes in the Democratic Republic of the Congo
    Lake Kivu
    February 2008 events in Africa
    2008 disasters in Africa
    History of Bukavu
    Hidden categories: 
    Pages using gadget WikiMiniAtlas
    Articles with short description
    Short description matches Wikidata
    Articles using Mw magnitude scale
    Coordinates on Wikidata
     



    This page was last edited on 6 March 2024, at 03:37 (UTC).

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