Geothermal Exploration in Eritrea

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Outline geologyof Nabro-Dubbiarea• Nabro Lies 2218m asl and• 600m above Mabda• Trachytic lava flows andpyroclastic emplaceprimarily on the Nabro• WNW faults and fracturesdissects the horst• Dubbi – the largestreported historical 1861eruption in Africa• Extensive basaltic lavafields cover wide area• The major transversestructure separates theDanakil blocks into twogeological set up
• Nabro Lies 2218m asl and 600m aboveMabda• Trachytic lava flows and pyroclasticemplace primarily on the Nabro• The major transverse structureseparates the Danakil blocks into twogeological set up
Page 1 and 2: Geothermal Exploration in EritreaSh
Page 5 and 6: Introduction- Previous worksGeother
Page 7: Low temperature areas - springs
Page 12 and 13: Geological and Geothermal Setting-A
Page 14 and 15: A SECTION OF THE WESTERN SIDE OF AL
Page 16 and 17: Assessment from Lineament
Page 18 and 19: Resistivity map at 3500 metres belo
Page 20 and 21: ConclusionThe tectonic setting and
Page 22: Conceptual model of Alid geothermal

Geothermal Exploration in Eritrea

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