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Ruby

Ruby - the name directed at red, gem-quality corundum - is among the best gemstones for jewellery settings. Rubies might be any shade of red, from pinkish to purplish or brownish red, with respect to the chromium and iron content from the stone. Frequent twinning from the crystals makes the fabric prone to fracture, yet ruby is a difficult mineral, second and then diamond in hardness. Crystal prisms are hexagonal with tapering or flat ends. Since the crystals grow they form new layers, and with respect to the geological conditions and minerals present, colour variations, called zoning, occur.
These are simply worldwide in igneous and metamorphic rocks, or as waterworn pebbles in alluvial deposits. The best stones originate from Burma; those from Thailand, the primary source, are brownish red; Afghanistan, Pakistan and Vietnam produce bright red stones; those from India, New york (USA), Russia, Australia, and Norway are dark, often even opaque.
In 1902, a Frenchman, Auguste Verneuil, produced a synthetic ruby crystal by exposing powdered aluminium oxide and colouring material towards the flame of the blowtorch.
Properties
Chemical Composition: 
Aluminium Oxide - Al2O3 (trace elements Chromium, Iron, Titanium, etc. are responsible for the different colored varieties
Classification / Type: 
-
Colors / Varieties: 
Red / Reddish-pink
  • 6-Ray Star Ruby
  • Trapiche Ruby
Crystal System / Forms: 
Trigonal System
Hardness: 
9
Specific Gravity: 
3.98 - 4.00
Cleavage / Fracture: 
None may show parting / Conchoidal fracture. (Parting or false cleavage occurs along directions of weakness which are parallel to the basal plane or the rhombohedral faces of the crystal and are observed externally as grooves or striations on the surface.
Optic Character: 
Anisotropic, D.R., Uniaxial negative
Lustre: 
Vitreous
Refractive Index / Birefringence: 
1.762 - 1.770 / 0.008; Range: 1.754 - 1.778
Pleochroism: 
Strong in deep colored varieties
Dispersion: 
0.018
Magnification: 
  • Crystals of calcite, dolomite, apatite, etc.
  • Silk - three directional needles of rutile intersecting at 60° / 120°; Needles of boehmite intersecting at almost 90°; Needles of ilmenite etc.
  • Parallel polysynthetic twin lamellae.
  • Color zoning and angular growth zoning.
  • Fingerprints and fluid inclusions.
  • Zircon halo inclusions etc.
U.V. Fluorescence: 
Varies according to the color
Spectrum: 
Strong absorption of the yellow, green and violet wavelengths. A broad band centered at around 550nm, a series of fine lines in the red, two of which appears as a single line which is actually 'doublet' at 694.2nm and 692.8nm (two lines closely spaced) which in appropriate lighting are fluorescent. Other lines are at 468nm, 475nm and 476.5nm. The presence of Iron in some rubies suppresses the fluorescence and imparts a duller color to the stone.
Cause of Color: 
Chromium, Iron (may / may not be present).
Treatment (Enhancement): 
Specific Tests & Remarks: 
-
Synthesis: 
Simulants (with key separation tests): 
Natural / Synthetic Spinel (optic character, R.I., inclusions), Tourmaline (R.I., S.G., pleochroism, inclusions), Red Garnets (optic character, spectrum), Glass (optic character, inclusions, U.V. fluorescence), Glass (optic character, inclusions, U.V. fluorescence), Doublets (inclusions, U.V. fluorescence), Synthetic Cubic Zirconia (optic character, R.I., S.G.), etc.
Geological Occurrence: 
In igneous and metamorphic rocks (marble, dolomite, etc.
Sources: 
Myanmar (known as Burmese Ruby), Thailand, Sri Lanka, Africa (Kenya, Tanzania, Madagascar), India (Orissa, Kangyam - Kaur, Karnataka, Andhra Pradesh, Madhya Pradesh), Vietnam.
Cuts & Uses: 
Facetted cuts (usually mixed cuts), cabochons, beads, carvings, etc.
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