EARTH TREMORS IN NIGERIA AND THE SOCIO-ECONOMIC IMPACT

Main Article Content

I. B. Osazuwa

Abstract

Earth tremor is a physical phenomenon that can originate from different sources such as the interior of the solid earth, the aqueous earth, the atmospheric earth; and from outer space. In all these, the initial effect is on the solid earth, causing it to shake. Then later, the tremor is finally transmitted to the surface of the solid earth in obedience to the principles of physics, which involve energy, force and motion. The surface structures, which could not withstand the ensuing stress/strain, will either collapse or become deformed. Quite a number of physical occurrences on the surface of the earth can be traced to earth tremors, which may not have been felt instantly until later, but the ones that attract attention are those that occur on macro scale. There are some reported cases of earth tremors in Nigeria. Areas that may be prone to earth tremor in Nigeria are those indicated by possible major active fault lines deduced from the Primary Gravity Network of Nigeria, which was established by Osazuwa in 1985. Earth tremors are not known to enhance socio-economic relief to the inhabitants in the regions at the time of their occurrence. However, when maintenance works are carried out on areas and structures affected by earth tremor, the socio-economic setback can be boosted. Efforts were made by Nigerian scientists to study the occurrence of earthquakes and earth tremors in West Africa generally and Nigeria in particular. In all sincerity, Nigerian intellectuals perform excellently well outside the Nigerian boarder, but back home in Nigeria, the story is different, probably due to frustration arising from lack of enabling infrastructure. In all the research activities that have taken place in Nigeria, the initial impetus from the appropriate government organ is often very high, but transient. In conclusion, Nigeria will continue to experience 

Downloads

Download data is not yet available.

Article Details

How to Cite
Osazuwa, I. B. (2021). EARTH TREMORS IN NIGERIA AND THE SOCIO-ECONOMIC IMPACT. Nigerian Journal of Physics, 30(2), 39–50. Retrieved from https://njp.nipngr.org/index.php/njp/article/view/93
Section
Review Articles

References

Ajakaiye, D. E., (1985). What is an Earthquake, Keynote address delivered at the first National Seminar on Earthquakes in Nigeria, held in Zaria Hotel 8th – 9th July, 1985.

Bates, Robert L. and Jackson, Julia A. (1987), (Editors): Glossary of Geology; Third Edition. Virginia, American Geological Institute, 788 p.

Ebong, M. B., Adaminda, I. I. Kolo and Osazuwa, I. B., (1991). Some aspects of the Geodetic Networks in Nigeria. AVM- International Edition, Vol. 8, pp. 16 - 26.

Egwuonwu, G. N., I. B. Osazuwa and S. O. Ibe.(2009). “Spearman’s Rank Correlation of Two Methods in Integrated Geophysical Investigation”.Pacific Journal of Science and Technology. 10(2):693-701. November 2009 (Fall), http://www.akamai university.us/PJST.htm.

Ike, E. C. Osazuwa, I. B. and Schoeneich, K., (2003a). The Achi-Ido Meteorite fall Goronyo Local Government Area, Sokoto State Nigeria, 3rd November, 2001. Abstract Proceedings of the Abuja Congress 2003, held at Abuja, from 20th to 24th May, 2003.

Ike, E. C., Osazuwa, I. B. and Schoeneich, K. (2003b). The Achi-Ido meteorite fall, Goronyo Local Government Area, Sokoto State, Nigeria. African Geoscience Review, Vol. 10, Nos. 1 & 2, pp. 127-133.

ONIKU, Adetola Sunday (1999). A Detailed Study of Teleseismic P-Wave Travel Time Residuals at Ahmadu Bello University Seismic Station Zaria.M.Sc. Thesis, Ahmadu Bello University, Zaria, Kaduna State, Nigeria.

Adetola, S. O., Ojo. S. B. and Osazuwa, I. B. (2004). Study of relative travel time residuals of P-Wave at teleseismic distance at the Ahmadu Bello University Zaria Seismic Station. Abstract Proceedings of the 27th Annual Conference of Nigerian Institute of Physics, held at Kaduna Polytechnic, Kaduna, Nigeria 15 - 18 September, p. 43.

Osazuwa, I. B. (1978): Gravity and Magnetic Survey of the Upper Benue Trough. M Sc Thesis, AhmaduBello University, Zaria, Nigeria, 113 pages.

Osazuwa, I. B. (1985a). The Establishment of a Primary Gravity Network for Nigeria.PhD Thesis, Ahmadu Bello University, Zaria, Nigeria, 320 p.

Osazuwa, I. B. (1985b). On the application of microgravity techniques for the monitoring of possible Earthquakes occurrences in Nigeria, Proceedings of National Seminar on Earthquakes in Nigeria, pp. 63 – 76.

Isaac B. Osazuwa (2006). GRAVITY: The Foundation of Geophysics and its usefulness to Mankind. - An Inaugural Lecture. Publication of the University Organized Lectures Committee, Vice Chancellor’s Office, Ahmadu Bello University, Zaria, Nigeria, 110 p.

Osazuwa, I. B. and Ajakaiye, D. E. (1986).The use of the Graphic Chart for the analysis of observations in a Gravimetric Network. Survey Review, U.K., Vol. 28, No. 221, pp. 345 - 350.

Osazuwa, I. B., Ajakaiye, D. E. and Verheijen, P.J.T. (1981).Analysis of the Structure of part of the Benue Rift Valley on the basis of new geophysical data. Earth Evolution Sciences, Vol. 2, pp. 126-135.