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A Geothermal Resource for Eritrea, an Energy-Poor African Nation

Duffield W.A. , Clynne M.A. , Foumier R O., Janik C. J. , Lowenstern J., Smith J. G. , Giorgis L.W., Kahsai G., Mariam K.W. and Tesfai T.

Location
Alid, Eritrea
Conference
New Zealand Geothermal Workshop
Year
1996
Session
Geology
Language
English

Full text

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Abstract

Eritrea badly needs electrical energy to power an emerging economy. Geothermal resources associated with volcanoes may be able to provide the energy needed to launch this new nation's development plans. We have undertaken a pre-drilling assessment of the geothermal potential of Alid volcanic center as a step toward realizing this possibility. Alid volcanic center is a 700-meter-tall structural dome astride the axis of a crustal spreading center (the Danakil Depression) in eastern Eritrea. This mountain has many fumaroles whose gas compositions suggest an underlying hydrothermal system of about 250?C or hotter. Many of the volcanic rocks at Alid are rhyolite, which suggests an upper crustal silicic ma,oma reservoir beneath the mountain. The growth of this magma reservoir probably produced the structural dome by arching up overlying rocks. The process of dome formation and the ongoing crustal spreading probably produced and help maintain permeability in the hydrothermal system.

Copyright 1996, University of Auckland. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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