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Mineral Resources Potential - Geothermal Resources

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2 10 <strong>Mineral</strong> <strong>Resources</strong> <strong>Potential</strong> of Ethiopia<br />

consists of two major rock type!: Trap volcanies euid sedimentary<br />

rocks. The fluvid-lacustrine Delbi cod and oil shale-bring.<br />

formation is composed of mudstone, ~ ~ r ~ clay, o silt, u clay, s<br />

sand, sandstone, coal, organic shale and pyroclastic sediments. The<br />

thickness of the coal seam ranges 0.5-2.2 m. Petrographical and<br />

chemical studies conducted by the above authors revealed that the<br />

coal in Delbi has low moisture content (3.98-10.4%) and ash<br />

content 12.1-54.2 %) in fresh and 22.2% in dry), low carbon<br />

content (1,343.09 in fresh and 38.53 in dry) and low calorific<br />

value (4,000-5,000 cal/kg in fresh and 4,552 callkg in dry)<br />

(Wolela, 1 99 1 ).<br />

-<br />

Maye cod deposit (Illubabur)<br />

The Inter-Tappean continental fluvial-lacustrine sedimentary<br />

sequence of Moye is situated within the geographic coordinates 7" 1<br />

19'45" - 7' 24'7" N and 36' 48'21 " - 36" 5 1' E. It is located 59<br />

km southwest of Jimma and 14 km west of Delbi. Moye is one of<br />

the best studied coal deposit in Ethiopia by Wolela et a/., 1987; F;'7<br />

Assefa Aklilu et ul., 1987; ~inyk et al., 1988; Korean lignite<br />

exploration group, 1988. The area consists of volcanic kd I<br />

sedimentary rocks. The sediments are composed of mudstone,<br />

graded sandstone, sand y-bmcias conglomemte, carbonaceous<br />

4<br />

clay, coal and oi! shale. The volcanic rocks consist of basalt, tuff,<br />

pyroclastics and tuff breccias. The coal seams at Moye are grouped<br />

under humic coal (lignite-sub bituminous).<br />

Nejo-Meckeke coal deposit (Wollep)<br />

The fluvid-lacustrine lignite deposit of Nejo is located 9" 27'-9"<br />

33'N and 39" 19'-35" 29'E, 190 km west of the town of Nekemte.<br />

The area consists of three major lithological units: Precambrian :.-<br />

i ; c .<br />

c'-.*, 5 ..<br />

basement, pre-basaltic sediment and Trap volcanics. The basement $ :,: i, '<br />

consists of schist, phyllite, and metasediment, metavolcanic and . 13<br />

dioritic intrusion. The pre-basaltic sediment overlies the basement $ :<br />

- and cupped by trap vdcanite's. The sedimentary sequence<br />

6'4<br />

:: ,<br />

, x m , .<br />

*,*..<br />

&:,:<br />

" .

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