Shemang, E.M. and Molwalefhe, L.N. (2011) Geomorphic Landforms and Tectonism along the Eastern Margin of the Okavango Rift Zone, North Western Botswana as Deduced From Geophysical Data in the Area. Department of Geology, University of Botswana, Gaborone Botswana.

has been cited by the following article:

• TITLE: Seismicity Study of Botswana from 1966 to 2012

  AUTHORS: Bokani Nthaba, Rapelang E. Simon, Ghebrebrhan M. Ogubazghi

  KEYWORDS: b-Value, Catalogue, Completeness Magnitude, Okavango Delta Region, Seismicity

  JOURNAL NAME: International Journal of Geosciences, Vol.9 No.12, December 29, 2018

  ABSTRACT: The history of Botswana’s major seismic events has been initiated by two earthquakes that occurred on the 11th of September and 11th of October 1952 with ML Richter magnitudes of 6.1 and 6.7, respectively, in the Okavango Delta Region (ODR). Not much is known and well documented about the seismicity of a larger coverage of Botswana primarily because over the years, local seismic stations were biased to the north-western part of Botswana, to monitor the more seismogenic ODR. The objective of this study is to use data from the International Seismological Centre (ISC) bulletin for the period 1966-2012 to estimate the relative size distribution of seismic events (b-value), the rate of seismic activity (a-value), and associated stress condition prevailing in Botswana to assist in the quest of hazard mitigation. This study shows that micro-seismic activities of magnitude ranging from 1.3 to 5.7 are distributed not only on the northern part of Botswana, but also in other parts of the country such as the Southern (including Kweneng East and West), Central and Eastern Botswana. Based on 327 events extracted from data compiled by the ISC, the frequency-magnitude distribution (FMD) of earthquakes in Botswana from 1966 to 2012 was estimated with b-value and a-value for the entire catalogue found to be 1.2 and 6.3, respectively, implying a region of low stress dominated by small to moderate events. The minimum completeness magnitude (MC), a value that indicates the lowest magnitude above which all seismic events are reliably recorded was found to be 3.8. From this analysis, annual probabilities of occurrence for M4 and M5 events were found to be 67.2% and 4.3%, respectively, while M6 or larger event has an annual probability of 0.3%.