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Mineral Resources Potential - Geothermal Resources

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142 <strong>Mineral</strong> Resourocs <strong>Potential</strong> of Ethiopia<br />

golf-clubs, and bicycle frames, and have been successfully<br />

employsd in reinforced concrete (Noetstaller, 1 98 8).<br />

Graphite deposits in Ethiopia<br />

The meta-sedimentary rocks in Sidarno, Haramghe, Wollega and<br />

Tigray are potential sources for graphite. A series of Iong belts of<br />

graphitic schist extends for tens of kms through the Kenticha and<br />

Kibre Mengist areas of the Adola Belt and in Soka, and Kunni<br />

valley of the Chercher Mountain with large greenschist series. The<br />

graphite in Moyale area is hosted by quartz-feldsp-mica schists<br />

and quartzites which gendl y form continuous bodies extending<br />

for hundreds of meters, The .Moyale graphite deposit has an<br />

estimated reserve of 0.46 Mt of graphite (Mengistu and Fentaw,<br />

2000).<br />

- - 4.11 Silica<br />

The chemical compund silicon dioxide, also known as silica, is<br />

the oxide of silicon, chemical formula Si@. Siliceous is an<br />

adjective meaning "referri6 to silica". Silica is found in nature in<br />

( aB$; several forms, including quartz and opal. In fact, it has 17<br />

I . .I'<br />

crystalline forms. The most oornmon constituent of sand in inland<br />

continental settings and non-mpical coastal settings is silica,<br />

usually in the form of quartz because the considerable hardness of<br />

this mineral resists erosion, However, the composition of sand<br />

varies according to local rock sources and conditions. Variants<br />

found in high-pressure impacts are mite and stishovite. Many<br />

rrns of life contain silica structures (Biogenic Silica), including<br />

icro-organisms such as diatoms, plants such as horsetail, and<br />

mds such as hexactinellid sponges. It is present in the cell walls<br />

virious plants (including edible ones) to strengthen their<br />

ctural integrity. '

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