Research Journal of Physics1819-3463xxxx-xxxxScience International10.3923/rjp.2012.1.18AdeotiL. AlileO.M. UchegbulamO. AdegbolaR.B. 1201261The seismic refraction investigation was carried out using the seismograph and it involved twenty-two profiles spread over three traverses with 24 spreads per profile along the major path that passes through the Golden Heritage Estate. A distance of 72 m per profile was utilized for seismic refraction survey. The result shows that the seismic refraction layers delineated were three and first one have an average velocity of 736 m sec-1 and thickness of 2-6 m, indicating topsoil. Seismic layer 2 on its part has an average velocity of 1468.18 m sec-1 and thickness 3-8 m, indicating laterite. Then the third seismic layer has an average velocity of 2272.73 m sec-1 and thickness of 5-12 m, indicating sand. These layers delineated by seismic refraction are characterized by velocity increase with depth. The sand units in the layers delineated acts as the aquifer units. Also the seismic refraction survey could not image the second, third and subsequent aquifers due to the weaker energy source used, hence, it is suggested that for future studies in order to be able to map deeper horizons, stronger energy source should be used.]]>Adegoke, S.O., T.F.J. Dessauvagie and A.J. Whiteman,19701970pp: 269276Birch, F.,19661966pp: 97-173pp: 97-173Haeni, F.P.,198651236249Kogbe, C.A.,19892nd Edn.,Pages: 538Pages: 538Lennox, D.H. and V. Carlson,196732331362Ogbe, F.A.G.,19701970pp: 305-324pp: 305-324Van Overmeeren, R.A.,19814613041313Ackermann, H.D., L.W. Pankrate and D. Danserean,198651223235Philip, A.O.,2001Hunter, J.A. and S.E. Pullan,1990559296Tearpock, D.J. and R.E. Bischke,1991pp: 94-96pp: 94-96Watts, R.D., A.W. England, R.S. Vickers and M.F. Meier,197515459461Slansky, M.,196211270270