When George Harrison discovered the Main Reef of gold at Langlaagte farm in 1886, it was believed by many to be an old river that had been turned on its side. They therefore believed the gold could not continue for more than about 30 to 50 meters underground.
That this was wrong was soon revealed by pioneers like J.B. Robinson who proving that the reef dipped far underground. The next theory was that this was a deep lake, that had filled with gold-bearing debris over the ages, from rivers entering at various points. However no such rivers or traces of them exist.
Another theory became popular, that the gold had come up in volcanic activity, the volcanoes being eroded away over time, and releasing gold rich rock into an inland sea. This view of how the Witwatersrand gold fields developed held sway until recently, when imagery from space became available.
Portion of the Main Reef at George Harrison Park (Gavin Whitfield)
Before time
Before time was as we know it, a great inland sea or lake existed where today the Witwatersrand lies, and stretched out right across the Orange Free State.
Along the shoreline, mostly along what would become the Witwatersrand, but stretching away towards Potchefstroom...