Erik Thomas Swedenstierna, On the Corundum of Gellivara (1816)
“ If we except the red felspar, which at small distances runs parallel with the ore and sometimes crosses its layers, the whole forms almost a solid mass of iron, of a very considerable extent, and of an unknown depth. In those places where the ore is of a loose texture and either coarse or fine-grained, a large quantity can in an hours time be dug up by a spade. ”
