The Danakil Depression lies at the triple junction of three tectonic plates and has a complex geological history. It has developed as a result of Africa and Asia moving apart, causing rifting and volcanic activity. Erosion, inundation by the sea, the rising and falling of the ground have all played their part in the formation of this depression. Sedimentary rocks such as sandstone and limestone are unconformably overlain by basalt which resulted from extensive lava flows.
The Danakil Depression can be said to ‘begin’ here. It is one of the most inhospitable regions of the world, but is nonetheless spectacular, full of eye-catching colors, as in the sulphur springs. The desert has several points lying more than 100 meters (328 ft) below sea level; You pass through a small town of Berhale where the camel caravan stop before they proceed to the northern highlands. En route you see many long camel caravans coming to the salt mine and others going out of the Danakil with their salt loaded camels.(3-4 hrs drive) Camp Hamedela. After drive to reach Hamad Ela, better village with a total population about 500 people. Sun set at Dallol. Over night camping at Hamed Ela.
Morning tour Drive to Ragad (Asebo), the place where the localities are mining salt. Look the activity of breaking the salt from the ground, cutting in to rectangular pieces and loading on camels. You drive ahead to Dallol and visit the difference landscape formed by volcanic activity, Dallol + Lake Assal + camel caravans. Excursion to Dallol (116 meter below sea level, one of the lowest places in the world) colorful salts mining, visit Lake Assal, follow up camel caravans and walk with the Afar people. Drive back to Hamedela and proceed to Mekele.
