This location is also part of the
basement complexes which are mainly made up of pegmatite and gneiss which have
undergone metamorphism due to relic’s structure. During this metamorphism there
is segregation of mafic and felsic minerals know to compose of
palesome, (dark
colour). Other features seen here is that texture is graphic and pegmatite compose
of quartz, mica, muscovite.
The
G.P.S of this location is as follows.s
Latitude 08o
48' 88"N
Longitude 08
31' 23"E
Elevation
261m