Kalahari Craton Kalahari Craton The Kalahari Craton is a craton, an old and stable part of the continental lithosphere, that occupies large portions of South Africa, Botswana, Namibia and Zimbabwe. It consists of two cratons separated by the Limpopo Belt: the larger Kaapvaal Craton to the south and the smaller Zimbabwe Craton to the north. The Namaqua Belt is the southern margin of the Kaapvaal Craton. Parts of the Kalahari Craton are now located in East (the Grunehogna Craton) and West Antarctica (Haag Nunataks) and the Falkland Islands. The name was first introduced by . Following a terminology introduced in 2008, the
Maranjab Desert north of the city of Isfahan Badrod continue sabulous large sand dam, the tallest sand dunes East is about 70 meters. [3] In addition to the dunes which is the main attraction Kvyrnd , there Karshahy castle and wander the island Maranjab, about the construction of the castle and the inn next to the salt lake, is quoted by Shah Abbas caravanserai and despite creating numerous castles throughout the country, in the region defense facility was not built, because until then enemies for salt Lake and desert expanse, from this side of the capital were not attacked. Attacking Uzbeks and