Recent discoveries related to ores from Kestel Mine in the Taurus Mountains
of Turkey show how prehistoric miners used the magnetic properties of the
black iron oxide to accomplish the difficult separation of cassiterite (tin
oxide) from low-grade cassiterite ores. Excavations at the site of Goltepe
, dating to the third millenium BC, have yielded hematite ore nodules conta
ining a few percent, or less, of cassiterite and a sequence of processed, g
round, and separated minerals. Laboratory experiments showed that reduction
at temperatures as low as 700-850 degreesC converted hematite to the black
magnetic oxide, which could be much more easily crushed than the hematite
ore. On grinding and panning this material, the magnetic oxide clumped toge
ther effectively to yield almost complete separation of the cassiterite gra
ins, a separation which, without automatic magnetic clumping, would be extr
emely difficult to accomplish due to the similar densities of cassiterite a
nd magnetite minerals. The deliberate production of magnetic oxide may expl
ain the shallow crucible bowl furnaces, the vast quantities of stone grindi
ng tools, the large amount of residual magnetite at the site, and the fine
particle sizes (which were necessary for the magnetic separation). These fi
ndings establish Kestel/Goltepe as a viable cassiterite (ore) production si
te. (C) 2001 Elsevier Science Inc. All rights reserved.