Recently, a major alluvial occurrence was discovered in the southern region of Ruvuma, Mtwara and Lindi. Varieties of such include chrysoberyl, spinels, sapphire, garnets, zircons and diamonds.
Coal, uranium, and various industrial minerals such as soda, kaolin, tin, gypsum, phosphate and dimension stones are plentiful across different geographical areas in Tanzania. Coal resources similar in quality to the Gondwana coals of southern Africa occur in the Ruhuhu and Songwe-Kiwira basins in Limestone and dolomite-good resources of high purity occur in the white marble deposit of the Morogoro Region. Potential for dimension stone and refractory grade limestone is therefore excellent. Varieties of clays – bentonite, kaolin and fullers earth – in size-able deposits have been identified and are only scantily exploited. The Pugu kaolin deposit located some 30 kms West of Dar es Salaam has a great potential for development. Evaporates and saline deposits of economic significance are associated with the rift valley lakes. Investigations of the Soda ash deposits at Lake Natron revealed a potential recovery of over one million tonnes a year.
Graphite occurs in high-grade gneisses mainly in the Usagaran system. Sufficient reserves have been identified at Merelani, northern Tanzania, for a 40 year operation at a mining rate of 15,000 tonnes per year of high grade flake graphite of 97-98% purity. Basemetals are found in a belt running from Kagera through Kigoma to Mbeya, Ruvuma and Mtwara regions: recent evaluations have so far outlined contained resources of 500,000 tonnes nickel, 75,000 tonnes copper and 45,000 tonnes cobalt.
Gold and diamonds have always been the mainstay of the country’s mineral production. In fact Tanzania has been a significant diamond producer for several decades, with the bulk of production coming from the Mwadui area where commercial production began in 1925. But gold is the resource currently offering one of the best areas for investment.
The current perceived opportunities range from former mines in the Archaean Greenstone belts around Lake Victoria and Proterozoic rocks as well as conceptual grass root plays in Karoo and younger rocks. Investigation has mainly been focused on the greenstone belts around Lake Victoria with particular attention on the shear hosted gold mineralization associated with banded iron formations (BIF), tufts and volcano-sedimentary exhalative. Several “world class” gold deposits have already been discovered in the Lake Victoria Goldfields and are at different stages of development. These deposits have reached various stages of development. So you are welcome to experience minerals tourism as well as establishing mining business in Tanzania.