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October 2012 Vol. 1(1)
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Pubmed for articles by:
Aga T
Baba J
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Global Advanced Research Journal of
Geology and Mining Research
October 2012 Vol. 1(1), pp 007-013
Copyright © 2012 Global Advanced Research Journals
Full Length Research Paper
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The Geology and Geotourism Potential of the Mayes
Water Fall, North Central Nigeria
Aga, T1, Atane, G1. and Baba,
J2
1Department
of Geology and Mining, University of Jos, Jos-Nigeria.
2National
Metallurgical Development Centre. Jos-Nigeria.
*Corresponding
Author’s
E-mail:tergaus@yahoo.com
Accepted 08 October, 2012
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Abstract |
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Detailed geological mapping was carried out on some
parts of the Sha-Kaleri Younger Granite Complex
which lies between latitudes 090 3.51N
and 090 8.51N and longitudes
080 431E and 080 451E
and forms part of Kurra Sheet 189SW. The area
designated for the research project is underlain by
the Basement Complex in the western part and extends
to the southeastern part of the study area. These
Basement Complex rocks were emplaced during the Pan
African Orogeny before the Jurassic Younger Granites
intruded through peripheral ring structures. Within
the confines of the research project the gabbros are
well represented occurring within the migmatite-gneiss
of the Basement Complex and along river channels.
They also occur as dykes intruding the Basement
Complex. This depicts the end of the Pan-African
Orogeny as they cross-cut the Basement Complex.
Petrographic examination and laboratory assay showed
the presence of the dominant rock forming minerals
which include plagioclase and alkali feldspars,
quartz, biotite and olivine as observed within the
field of view under a polarized light when plane and
crossed. Structural study carried out within the
confines of the project area reveal the presence of
dykes, veins, foliations, xenoliths and joints. The
field tectonic studies and analyses of these
structures were simply descriptive, that is done as
a sequence of recognizing and describing their
attitudes which are essentially defined by strike
and dip. With the use of a circular histogram which
displays directional data a consistent dominant
structural trend of NE-SW was envisaged.
Geologically, this essentially suggests that all the
rocks underwent a uniform post emplacement tectonic
episode as revealed from the relationship to other
processes and geologic history of the project area.
The geotourism potentials of the study area as
keenly observed show the presence of a colossal
waterfall known as the Mayes water fall, captivating
hills, scenic environment and an alluring vegetation
which can be developed into a tourism haven.
Keywords:
Geology and Geotourism, Mayes Water Fall, North
Central Nigeria.
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