Macroseismic survey of the 6 February 2016 KwaZulu-Natal, South Africa earthquake

Author:

Mapuranga V.1,Kijko A.2,Saunders I.3,Singh A.4,Singh M.5,Zulu S.5

Affiliation:

1. Geology Department, University of Pretoria, Pretoria, South Africa e-mail: victor.mapuranga@seequent.com

2. Natural Hazard Centre, University of Pretoria, Pretoria, South Africa e-mail: andrzej.kijko@up.ac.za

3. Engineering Geoscience and Geohazards, Council for Geoscience, Pretoria, South Africa e-mail: ians@geoscience.org.za

4. Maya Geophysics, Durban, South Africa e-mail: ashmeesingh777@gmail.com

5. School of Agricultural, Agricultural, Earth and Environmental Sciences, University of KwaZulu-Natal, Durban, South Africa e-mail: singhm5@ukzn.ac.za; zulusg278@gmail.com

Abstract

Abstract On the 6th of February 2016 at 11:00 hours local time (0900 UTC), KwaZulu-Natal was struck by an earthquake of local magnitude ML=3.8. The epicentre of the earthquake was located offshore in the Durban Basin. The earthquake shaking was widely felt within the province as well as in East London in the Eastern Cape province and was reported by various national media outlets. Minor structural damage was reported. A macroseismic survey using questionnaires was conducted by the Council for Geoscience (CGS) in collaboration with the University of KwaZulu-Natal (UKZN) which yielded 41 intensity data points. Additional intensity data points were obtained from the United States Geological Survey (USGS) Did You Feel It? programme. An attempt was made to define a local intensity attenuation model. Generally, the earthquake was more strongly felt in low-cost housing neighbourhoods than in more affluent suburbs.

Publisher

Geological Society of South Africa

Subject

Geology

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