Tarso Voon on a satellite image from NASA
The summit of the mountain is dominated by its 14 x 18 km wide and relatively shallow caldera. At its north-eastern side of the mountain lie in a 180 - degree arc extensive basalt fields and a neighboring crater Ehi Mosgau. Provisions resulted in a rock formation in the Quaternary period. Deposits of pyroclastic clouds are found within a radius of 15 to 35 km around the caldera. The massif of Tarso Voon rises above a layer of rock known as the Precambrian schist.
The well-known Soborom - Solfatarenfeld, the largest in the Tibesti Mountains of the summit caldera lies around 5 km to the west in an area caused by tectonic uplift. Its fumaroles, active mud pots and hot springs are frequented by the population of the Tibesti for medical purposes.
- Tarso Voon in the Global Volcanism Program of the Smithsonian Institution (English)
- Mountain in Africa
- Mountain in Chad
- Three thousand
- Geology of Africa
- Tibesti region