Abstract

Spatial-temporal variations in earthquake occurrence have been studied in many regions of the world but little can be said aboutthe Southern Africa Region in this regard. Using earthquakes of magnitudes greater than or equal to one together with theFORTRAN language and Generic Mapping Tools (GMT), spatial variations of earthquakes spanning the period 1966 to 2014were examined for the region. Similarly, the temporal variations with earthquakes of magnitudes greater than or equal to fourwere studied. The spatial analysis showed that the highest number of events (1438) in the period occurred at an average depthof around 7.5 km representing approximately 79.9 % of the total earthquakes considered. The temporal distribution of events onthe other hand showed that the highest number of events (590) were recorded in the year 1993. Three main issues were identifiedas potential factors responsible for the observed variations. Activities such as mining and failures in weak zones of the rockmass as well as increase in the number of stations were identified as the key factors responsible for the observed distributions.The third factor could not be independently verified. However, earlier studies suggest that this factor indeed have caused majorearthquakes in the region.

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