Quantcast

Ch. 7: Opal

Ch. 7: Opal Page of 311 Ch. 7: Opal Text size:minus plus Restore normal size   Mail page  Print this page
142
PRECIOUS STONES.
Fluorescence is strongly marked in some specimens. Other effects of heat are seen, one of the most striking being the way it decrepitates if heated suddenly, due, it is supposed, to minute cavities within the mineral, containing in many cases liquids. A change of colour may also occur on heating, the blue and violet shades changing to purple. By itself it is not readily fusible, but when mixed with some other substances it easily fuses to a slag and on this account is largely used as a flux; hence, possibly, the name.
On heating, a difference of electrical potential is induced between the cube faces and angles of the cube; this also occurs when light falls on the crystal.
The specific gravity varies between 3'01 and 3"19.
Crystals show a conchoidal fracture and a very perfectly developed octahedral cleavage. On account of this cleavage, Fluor Spar may be used to practice on to gain skill in the cleavage of Diamonds, and Tennant has used the mineral to make models of well-known Diamonds with a view to ascertaining the probability of the Great Mogul Diamond having been broken up into smaller gems. On account of the ready cleavage and natural brittleness of this mineral it is very easily damaged if knocked or allowed to fall. The powder of Fluor Spar of any colour, if sufficiently fine, is white, hence the mineral gives a white " streak" when drawn over a harder substance. The hardness of Fluor Spar is the standard No. 4 of Mohs' scale.
The crystalline form is cubic, and crystals may have the general habit of the cube or the octahedron, often with the edges and solid angles highly modified by faces of other crystal forms. Crystals occur up to a foot or more across the cube face, and in some places in enormous quantities.
Ch. 7: Opal Page of 311 Ch. 7: Opal
Suggested Illustrations
Other Chapters you may find useful
Other Books on this topic
bullet Tag
This Page