Critical Evaluation of Seismic Activities in Africa and Curtailment Policies – a Review Kenneth Kanayo Alaneme* and Eloho Anita Okotete

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Critical Evaluation of Seismic Activities in Africa and Curtailment Policies – a Review Kenneth Kanayo Alaneme* and Eloho Anita Okotete Alaneme and Okotete Geoenvironmental Disasters (2018) 5:24 Geoenvironmental Disasters https://doi.org/10.1186/s40677-018-0116-2 REVIEW Open Access Critical evaluation of seismic activities in Africa and curtailment policies – a review Kenneth Kanayo Alaneme* and Eloho Anita Okotete Abstract The present paper discusses the seismicity of Africa and the need for the implementation of vibration control strategies in Africa, erroneously considered as aseismic. The review catalogues information on the seismicity of Africa, attesting that virtually every region in the African continent has come under the threat of some form of seismic event. The magnitudes and intensities of these seismic activities has resulted in devastations, including: loss of lives, building and civil structures collapse, displacements of people, economic losses, psychological traumatization, and grave fear. Evidences available show that most of the devastations are accentuated by tremor induced collapse of buildings and civil structures. It is thus imperative for substantive, simply implementable, and sustainable proactive measures for controlling the threats of seismic events be discussed within the African context. Current mitigation strategies in Africa include the establishment of seismic codes which govern the design of civil structures. The challenge to the implementation and the effectiveness of the existing African seismic codes was briefly discussed, and new measures which can reduce seismic risks were also highlighted The submissions of the paper is envisaged will create awareness on the budding seismic activities in Africa and awaken relevant authorities on the need for timely and practicable mitigation strategies to be in place to avert the attendant catastrophes associated with seismic occurrences. Keywords: Seismicity, Structural design, Civil structures, Mitigation strategies, Africa Introduction had devastating effects on human lives (the quality of liv- It is a common knowledge among earth scientists that dif- ing) and technological advancement in the world. ferent parts of the world experience varying intensities of Earthquake is one major disaster that has had cata- seismic related activities and natural disasters. The inten- strophic consequences in the world today. It has been sities of these events which include volcanic eruptions, reported that about 40 disastrous earthquakes have oc- landslides, earthquakes and tsunamis depend on the geo- curred in the world since the end of the twentieth century, physical and geological features of the region where they and these events claimed an estimated 1.7 million lives occur (Akpan et al. 2015). Tectonic activities occurring (Guo 2010). Earthquakes mostly occur in the oceans, and beneath the earth’s surface are the major causative factors when the quakes occur in large magnitudes, it results in of these events resulting in disturbances which have dev- tsunamis which have led to mass destruction of lives and astating effects on the earth surface (Elnashai and Sarno properties all over the world. What are referred to as con- 2008). Aside these natural factors, man’s activities such as tinental earthquakes are also prevalent: these are earth- mining, deep quarrying, hydro-geological extraction or quakes which occur on land within the earth’s crust and at fluid disposal and other underground operations have also boundaries of continental plates and active blocks, usually been known to trigger quakes and other seismic events in having relatively lower magnitudes than those occurring some parts of the world (Farahani 2014), which are in the ocean (Elnashai and Sarno 2008). Earthquake events referred to as induced seismicity. The occurrence of seis- (land or sea) occur suddenly without prior warning; hence mic events, regardless its source of manifestation, have responses to earthquake events are often delayed, chaotic, unplanned, and unscientific, thus resulting in even greater * Correspondence: [email protected] loss (Guo 2010;Shelly2010). The consequences of Department of Metallurgical and Materials Engineering, Federal University of earthquakes are long-lasting social, environmental, and Technology, Akure PMB 704, Nigeria © The Author(s). 2018 Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. Alaneme and Okotete Geoenvironmental Disasters (2018) 5:24 Page 2 of 17 economic problems. It is therefore imperative to improve of such quakes. These terms facilitate ease of under- the means and methods of responses to seismic events to standing of the event by technical and non-technical curb the extent of damage per event. Most importantly, experts. Two frequently used terms in seismic studies, there is a great need to improve mitigation strategies to are magnitude and intensity. reduce the impacts of earthquakes and other seismic ac- tivities on structures. This would save lives and reduce the Magnitude amount of economic loss incurred during such events. This is a quantitative measure which is used to compare The African continent though not always associated the size of earthquakes worldwide irrespective of geo- with seismic events, is currently considered as a seismic graphical and geological settings. The magnitude of an prone region. This is because of the rising magnitude and earthquake is therefore the logarithmic measurement of intensities of seismic activities in the continent within the the amount of energy released by an earthquake past century. For the technical experts and well informed, (Hammed et al. 2016). This parameter was established to it is an issue of grave concern and imperatively requiring provide a basis for engineering and geophysical analysis of awareness and proactive measures to improve the means earthquakes (Kanamori 1983). Richter scale was the fore- and methods of responses to curb the extent of its devas- most approach introduced for assessing the size of earth- tations. For the ill-informed or superstitious, it could be quakes and laid the foundation for development of viewed as a “malady” of the big nations/ non-African earthquake magnitude. This was derived from maximum countries. The arbitration of nature to “create a balance” amplitudes recorded at different epicentral distances from between the well-organized advanced nations with pros- the point of rupture within the earth crust (Richter 1935). perous economies and poor African nations characterized The Richter magnitude also known as local magnitude with a history of poor governance and deadly health epi- ML, is thus a number characteristic of the earthquake, demics. Thus when seismic events happen within some and independent of the location of the recording station. African communities, non-scientific, superstition-laden Later, body-wave magnitude (mB), was introduced to ad- root causes may be advanced as reason for the occurrence. dress the inadequacies of ML. mB is computed from the Worrisome also is the tendency for proffered solutions to amplitude and the period of seismic body and its main ad- follow similar lines of thought. No matter how they are vantage is the applicability for both shallow and deep seis- construed, the fact remains that these events have had ter- mic events (Kanamori 1983). Body wave magnitude is rible effect on the citizens and economies of the affected denoted by mB for long period body wave magnitude and African nations, and consequently it has become neces- mb for short period body wave magnitudes (Liu et al. sary for greater awareness of the seismicity of Africa to be 2007). Another magnitude for shallow and distant earth- brought to the fore. quakes, is surface wave magnitude Ms. Moment magni- This review intends to provide detailed evidence of the tude scale (M W), is a relatively new scale which has the reality of seismic activities in Africa; highlight some of advantage of being used for measurement of larger the underlying factors responsible for their occurrence; earthquakes, unlike the Richter amplitude based scales report the level of intervention by various governments (Baruah et al. 2012). to address the issues of seismic activities in their do- main; and recommend pro-active, cost effective and Intensity technically implementable structural design schemes The effect of an earthquake on the Earth’s surface is which could be applied within Africa to reduce the called the intensity. It is a qualitative measure of the effects of earthquakes and other seismic activities in the actual shaking at a location during an earthquake, and is continent. The intention is to boost awareness of seismic assigned with Roman Capital Numerals (Hammed et al. activities in Africa, using a language that even 2016). Intensity scales were originally developed to non-technical experts can easily comprehend, as from extract observation data from an earthquake event. The hindsight, such people are better positioned in Africa first record scale is the Rossi-Forel scale which used ten than earth science experts to influence government degrees to describe earthquake effects in a place commitment and policies to issues related to seismic (Musson et al. 2010). The intensity scale consists of a threats and curtailment. Presently, there are sparsely
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