01 · Geology · 6 min read
Geology: why every mine begins with rock
A mine is a geological accident that happens to be economic. Understanding how mineral deposits form is the first discipline of mining.
Mineral deposits are rare. Ordinary crustal rock contains gold at roughly four parts per billion; an economic gold deposit concentrates that metal by a factor of hundreds or thousands. That concentration is the product of specific geological processes — magmatic fluids rising through fractures, hydrothermal circulation along shear zones, weathering that strips away waste and leaves resistant metals behind, or sedimentary systems that sort heavy minerals into layers.
In Tanzania, the Archaean greenstone belts of the Lake Victoria goldfields are the classic example. Ancient volcanic and sedimentary sequences were deformed, intruded and then plumbed by gold-bearing fluids that deposited metal in quartz veins and altered wall rock. Elsewhere in the country, the Karagwe-Ankole belt hosts pegmatite-related tin, tantalum and lithium, while the Mozambique belt supplies gemstones and graphite.
The practical consequence is that geology dictates everything downstream. It controls where you drill, how deep the ore continues, how hard the rock is to break, whether the metal will respond to gravity, flotation or leaching, and how much waste you must move for every tonne of ore. A mine plan written without a defensible geological model is a schedule of expensive guesses.
Good geological practice is therefore cumulative rather than heroic. Mapping, sampling, geophysics and drilling each reduce uncertainty in a different way, and the model is revised every time new evidence arrives. The best exploration teams are not the ones with the strongest opinions — they are the ones who change their minds fastest when the rock tells them to.

