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Geology of Abu Zeneima's
surroundings (Western Sinai, Egypt)
In August 1999 I had the
possibility to make an internship at the Sinai Manganese
Company in Abu Zeneima, which is half on the way between
Suez and Sharm El Sheikh, right on the border of the Gulf
of Suez. About 20 kms S of Abu Zeneima, are located the
oil fields of North
Abu Rudeis.
The Sinai Manganese Company mines manganese ores
(Mn-content up to 72%) which are found as lenses in
dolomite in the so called Um Bogma Formation
(Mississippian, lower Carboniferous), silica sands (
[Fe2O3]< 0.012%) in the
Abu Durbah Formation (upper Carboniferous),
kaolinite ( [Al2O3] up to
37%) in the Malha Formation (Lower Cretaceous) and
gypsum in the Karim Formation (Miocene). I was
able to visit all the mines and quarries as well as many
other places around Abu Zeneima, where you can study
geology at its best, as the whole desert there is one big
outcrop. If you've never been to the Sinai don't hesitate
to go there, you will enjoy it for sure!
Below two pictures from the surroundings of Abu
Zeneima:
The left picture shows a black, basaltic, Oligocene dyke
in the middle of the picture. This dyke intruded between
sediments of the Oligocene (reddish sandstones) and
Eocene (white, well bedded micritic limestones) to the
right of the dyke and the Miocene (dark marin sandstones,
transformed into a massive, 0.5 m chert layer on the
contact to the dyke) on the left side of the dyke.
The right picture shows normal faults in the
fossilifereous Cretaceous (probably Santonian) associated
with the Red Sea Rifting, which started in Lower
Miocene.
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Literature
- Rushdi, Said, The
Geology of Egypt, Balkema, 1990
Egyptian geological
links
Sinai & Red Sea
links
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