Geology and Archaeology

Geology

Ethiopia has a lot of resources of geological interest, among them: Dallol which is located in Afar region of northeastern Ethiopia, from west to east, the geology of the area is characterized by: Neoproterozoic metavolcanics and metasediments, Quaternary alluvial fan deposits and red beds, a transitional zone of mud and salt mixture, and evaporites, which consist of rock salt (commonly halite and potash) and sulfur/sulfides. The metavolcanic-sedimentary rocks of the area are sheared and locally affected by pervasive chloritization, silicification, and carbonatization as well as quartz-carbonate veining suggesting that it has a good potential for organic gold mineralization. The around alluvial sediments of Gehartu (5 m thick) and Musely Fans are also favorable for the occurrence of placer gold deposits. There are some studies, which reveals that industrial minerals such as kaolin and mica are also encountered in the Dallol area in addition to the already known sulfur and salt deposits. In the surrounding areas of mount Dallol, hot springs of varying temperature and extent are being erupted forming semi- circular-to-circular ponds. There are two types of hot springs, light-yellowish and yellowish brines are recognized which are contaminated with mud. In this area there is much need of geological survey and scientific study, this is an interesting area for scientists and investors. Are you interested to know more and discover the hidden treasure of the marvelous and inexplicable country contact our company: Yared Tour and Travel we will bring you there.