• Login
    • Login
    Advanced Search
    View Item 
    •   UoN Digital Repository Home
    • Journal Articles
    • Faculty of Science & Technology (FST)
    • View Item
    •   UoN Digital Repository Home
    • Journal Articles
    • Faculty of Science & Technology (FST)
    • View Item
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Active fault mapping in Karonga-Malawi after the December 19, 2009 Ms 6.2 seismic event

    Thumbnail
    Date
    2015-02
    Author
    Macheyeki, AS
    Mdala, H
    Chapola, LS
    Manhiça, VJ
    Chisambi, J
    Feitio, P
    Ayele, A
    Barongo, J
    Ferdinand, RW
    Ogubazghi, G
    Goitom, B
    Hlatywayo, JD
    Kianji, GK
    Marobhe, I
    Mwano, JM
    Shumba, B
    Tumwikirize, I
    Type
    Article; en
    Language
    en
    Metadata
    Show full item record

    Abstract
    The East African Rift System (EARS) has natural hazards – earthquakes, volcanic eruptions, and landslides along the faulted margins, and in response to ground shaking. Strong damaging earthquakes have been occurring in the region along the EARS throughout historical time, example being the 7.4 (Ms) of December 1910. The most recent damaging earthquake is the Karonga earthquake in Malawi, which occurred on 19th December, 2009 with a magnitude of 6.2 (Ms). The earthquake claimed four lives and destroyed over 5000 houses. In its effort to improve seismic hazard assessment in the region, Eastern and Southern Africa Seismological Working Group (ESARSWG) under the sponsorship of the International Program on Physical Sciences (IPPS) carried out a study on active fault mapping in the region. The fieldwork employed geological and geophysical techniques. The geophysical techniques employed are ground magnetic, seismic refraction and resistivity surveys but are reported elsewhere. This article gives findings from geological techniques. The geological techniques aimed primarily at mapping of active faults in the area in order to delineate presence or absence of fault segments. Results show that the Karonga fault (the Karonga fault here referred to as the fault that ruptured to the surface following the 6th–19th December 2009 earthquake events in the Karonga area) is about 9 km long and dominated by dip slip faulting with dextral and insignificant sinistral components and it is made up of 3–4 segments of length 2–3 km. The segments are characterized by both left and right steps. Although field mapping show only 9 km of surface rupture, maximum vertical offset of about 43 cm imply that the surface rupture was in little excess of 14 km that corresponds with Mw = 6.4. We recommend the use or integration of multidisciplinary techniques in order to better understand the fault history, mechanism and other behavior of the fault/s for better urban planning in the area.
    URI
    http://www.sciencedirect.com/science/article/pii/S1464343X14003525
    http://hdl.handle.net/11295/81019
    Citation
    Journal of African Earth Sciences Volume 102, February 2015, Pages 233–246
    Publisher
    University of Nairobi
    Subject
    December 2009 seismic event; Active fault mapping; Fault segment; Karonga; Malawi
    Collections
    • Faculty of Science & Technology (FST) [4284]

    Copyright © 2022 
    University of Nairobi Library
    Contact Us | Send Feedback

     

     

    Useful Links
    UON HomeLibrary HomeKLISC

    Browse

    All of UoN Digital RepositoryCommunities & CollectionsBy Issue DateAuthorsTitlesSubjectsThis CollectionBy Issue DateAuthorsTitlesSubjects

    My Account

    LoginRegister

    Copyright © 2022 
    University of Nairobi Library
    Contact Us | Send Feedback