The space “guest” fell in 1931 near the Tunisian city of the same name. Nowadays, it has been found out that the meteorite is a diogenite, that is, it belongs to the type of objects made of solidified magma. The formation of the latter takes place inside the asteroid, and then, as a result of slow cooling, rather large crystals are formed.
In Tataouine, the size of crystals reaches up to 5 millimetres, and black veins speak about the impact of high temperature and pressure on them in the past. According to scientists, Tataouine was subjected to a pressure of about 25 GPa. At the bottom of the Mariana Trench, for example, this figure reaches only 0.1 gigapascal.