Abstract
Afar being a dry region heavily affected by climate change, water and energy is a major issue for its population. Hopefully, favourable geothermal conditions developped because of its geological context. The border faults along the rift promotes the flow of meteoric water from the high plateaus into the faulted rift floor, where crustal thinning and upwelling of the hot mantle lead to exceptionally high heat flow. Furthermore, active fauulting along the rift axis favour the creation of convective hydrothermal systems. Moreover, when magma chambers develop at shallow depth (2–5 km) conditioned by central volcanic units, large high-enthalpy geothermal systems naturally arise. All conditions are combined in these structures to favour the development of fractured reservoir and impermeable cover. Basic ingredients for “classic” high-enthalpy geothermal systems are thus available in numerous places. This chapter describes some of the most relevant geothermal sites that are open for development, particularly when the needs of the local population will be considered as a priority target for the investors.
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Notes
- 1.
- 2.
OPEC Fund for International Development.
- 3.
United Nation Development and Environment Programs; Global Environmental Fund.
- 4.
Organic Rankin Cycle or “binary” plants.
- 5.
AGAPI, Afar Geothermal Development Company, a community based initiative, was created in 2015.
- 6.
The Afar name is “Boina” meaning fumarole, erroneously given to Dabbahu.
- 7.
Electromagnetics
- 8.
Magnetotellutics-Transient Electromagnetics
- 9.
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Varet, J. (2018). Geological Resources and Socio-Economic Issues. In: Geology of Afar (East Africa). Regional Geology Reviews. Springer, Cham. https://doi.org/10.1007/978-3-319-60865-5_12
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