Portal logo
120
PRECIOUS STONES.
Lapland, close to the Norwegian frontier, in a valley near Yaranger Fjord. The whole district consists of gneiss traversed by bands of pegmatite, and it was in sand derived from these rocks that the discovery was made. Of the associated minerals, Velain gives (the most abundant coming first) Garnet, Zircon, Hornblende, Glaucophane, Kyanite, green Augite, Quartz, Corundum, Eutile, Magnetite, Stauro-lite, Andalusite, Tourmaline, Epidote and Oligoclase felspar, and he believes the Diamond originated in the pegmatite, and at the same time as that rock was formed.
It is of interest to note that Professor Heddle obtained a specimen of rock from three miles north-east of Ben Hope, in Sutherland, Scotland, containing a "red Mica, red Zircons and either colourless Garnets or Diamonds," and it is recorded in the "Mineralogy of Scotland," vol. ii.,p. 194, by Mr. A. Thorns, that Dr. Heddle was confident, in his own mind, from their optical properties, that these were Diamonds. The point is of great interest, as beyond this there seems no record of this mineral occurring in the British Islands. At Carratraca, in Spain, Diamond is reported to have been found in a stream with Serpentine.
In North America Diamonds have frequently been found since 1850, when the first one was discovered in the alluvial workings for gold in California. Since this time they have been found at intervals both in the recent alluvium and also in the ancient detritus covered by lava flows. The Californian localities include, in Amador Co., Volcano, where an association with Garnet and Chalcedony is seen ; Fiddletown, with Gold and lead- and copper-ores ; in Butte Co., the Cherokee ravine with Zircon, Chromite, etc.; in El Dorado Co., at Forest Hill. In