A NOTE ON THE GEOMORPHOLOGY, GEOLOGY, ORIGIN AND ECONOMIC POTENTIALS OF OWU WATERFALL, OWA-KAJOLA, SOUTHWESTERN NIGERIA

Abstract

 The Omu-Aran quartzite ridge is part of the surface expression of a major, deep-seated, regional dextral fault in south-western Nigeria- the Ifewara Lineament. This structure is host to the magnificent Owu waterfall which has attracted visitors from all walks of life both locally and internationally. The geomorphology, scenery and other side attractions make the waterfall a place to visit at any period of the year. The origin of the waterfall is attributed to the inter-banding of micaceous lithologic layers with the more massive quartzite layers; multiple fractures; intense weathering; and erosion. This spectacular waterfall, which is a potential source of revenue, is grossly underutilized compared to other tourist centres in the country as a result of poor attention from governments and private investors. The great potential as a tourist attraction with its attendant side attractions as well as a source of electricity will not only serve as a source revenue generation and improving the economy of the surrounding communities, but will also generate fund for government and reduce, to a notable extent, the problem of rural-urban migration.