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Showing posts with the label spodumene

Gemstone Windows and Dark Patches: What to Look for in a Cut Gem

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AI-generated educational illustration. Conceptual only; not a photograph of an actual specimen or location. A coloured gem may have a pale, see-through centre or areas that look almost black. Both affect its appearance, but they do not have the same cause. What is a window? A window is an area where light passes through the gem instead of being returned towards the viewer. You may see the background through it, especially near the centre. Cutting angles and the material's refractive index—how it bends light—help determine whether this happens. There is no single ideal depth for every gemstone. Why dark patches need a closer look Darkness can have several causes. The material may absorb a lot of light. Some facets may reflect dark surroundings or the observer. Extinction is another cause, involving light that is not returned to the viewer after internal reflection. For that reason, calling every black patch “extinction” can be misleading. A simple viewing routine Look at the gem fac...

What is Spodumene? its chemistry and varieties and mining

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 Spodumene  spodumene pronunciation Spodumene, a member of the pyroxene group, is lithium aluminium silicate LiAlSi 2 O 6 and forms highly characteristic flattened and striated prismatic transparent crystals of the monoclinic system with good cleavages in two directions intersecting nearly at right angles and a notably brittle tendency. The hardness is 6.5–7 and the SG 3.18. The RI for the alpha, beta and gamma rays is 1.648–1.663, 1.655–1.669 and 1.662–1.679 respectively with biaxial positive DR 0.014–0.027. Crystals are strongly pleochroic with lilac, green or yellow in one direction and colourless in the other. The varieties include a yellow to pale green spodumene with no varietal name, the lilac-pink kunzite and a very rare chrome-green hiddenite. Kunzite shows no useful absorption in the visible but the chrome-green hiddenite shows a characteristic chromium spectrum with the customary strong doublet in...