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Mineral Resources Potential - Geothermal Resources

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152 M i d hums P d a l of Ethiopia<br />

4.17 Potash (Fertilizer mw materials)<br />

Potash is an impure form of potassium carbonate (K2C03) mixed<br />

with other potassium salts. Potash is used as a fertilizer, while the<br />

pwe carbonate is used in medicine, in the chemical industry and to<br />

produce decorative colour effects on brass, bronze and nickel.<br />

Production<br />

The worId's largest potash producer is the Potash Corporation of<br />

Saskatchewan (North America). Many other mas, however, have<br />

the resources for potash production. Today, 14 countries produce<br />

the world's supply of potash. The main producers are North<br />

America (mainly Saskatcbewa, with two-thirds of the world's<br />

recoverable potash located there), Russia, Belarus, Germany, Israel<br />

and Jordan, (the later two both using solar mporaPion pans at the<br />

Dad Sea to produce camallite from which potassium chloride is<br />

' produced). In Ethiopia, some 3,578 short tons and 2,500 short tons<br />

were mined by small-scale extraction techniqua in 1917 and 1927<br />

respectively (EGS, 1989).<br />

Potash deposits h Ethiopia<br />

There are large potash resources in Ethiopia in the extremely hot<br />

and arid Danakil depssion near Dallol. The potash deposit is par?<br />

of a Quaternary evaporite sequence that covers an area of about<br />

1,150 km2, of which only a small portion has been explored.<br />

Exploration work by the US-based Ralph M. Pmns Company<br />

included drilling of more than 300 lmreholes, seismic work and<br />

shaft sinking to 100 m depths, as well as approximately 600 m<br />

underground openings (EGS, 1989). The company delineated two<br />

ore bodies in the Dallol area; the Crescent ore body and the Mudey<br />

ore body. In this area the evaporite sequence is greater than 1,000<br />

m thick and includes Iarge potagh reserves. Most of the potassium<br />

salt is in the form of sylvite (KCI), but carnallite and kainite are

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