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A study of MADAGASCAR CORUNDUM |
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AL2O3 |
Sapphire found in a metamorphic marble.
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· Crystallographic properties of corundum: |
Trigonal.c = 1,3630 pp 0 86°4' ; pa1 = 122°26' |
Macle according to p (1011), often polysynthetic, |
accompanied by plans of separation, similar plans are also |
observed according to a1 (0001) unequal break to conchoïdal. |
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Hardness 9. Density 3,95 to 4,1 Refractive index: 1.76 - 1.77 |
Uniaxial and optically négative.ng = 1,7675; Np = 1,7593 |
The faces a1 frequently show the phenomenon of asterism, |
generally due to reflexions within separation p. |
Strong polychromatism , with following maximum ng. |
· Chemical properties: corundum is composed of pure |
alumina; its colouring is due to metallic oxide traces or inclusions. |
The story |
The color of sapphire, due to iron and titanium oxide, gives its |
best effect under daylight. Electric light makes it often dark. |
The color of the ruby, due to chromium oxide, on the contrary shows |
its most luminous red under electric lighting. |
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In Madagascar, corundum shows two different aspects: |
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1 stony and opaque crystals. |
2 crystals of smaller size often transparent and usable as gem. |
In Madagascar, stony corundum comes from mica schists metamorphosed by granite, as well as |
endomorphosed granitic veinules and more or less deprived of quartz which injects those. Silimanite is |
an usual satellite of corundum in this type of deposit. One also finds some one in eruptive rocks, |
syenites. |
Gems are generally found in alluvium, but occur either from basaltic slags, or from metamorphic |
marble or endomorpheous feldspatic rocks. |
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One distinguishes two principal types of corundum in Madagascar: |
Type I : isoceloedric, more or less acute accompanied or not by a small face a1 (0001) and more rarely |
by facets p (1011). Represented by figures 1 to 11, but which often become complicated in |
consequence of the irregularity of the development of some of their faces and by stacking with |
parallel axes of a great number of individuals. |
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10 |
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11 |
12 |
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13
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Scalenoedron |
Stacking with parallel axes, |
Crystal supporting on one of its bases |
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gutters at contours of the face. |
a small rhombohedron p in parallel |
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position. |
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Type 2: Characterized by the association of the prism d 1 (1120) at a broad base, with which can |
associate the isosceles ones, among which e 3 is most frequent, as well as the rhombohedron p. |
The base of Malagasy corundum crystals very frequently shows scratches or triangular figures in |
relief, limited by p. |
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Macle of blue corundum. |
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Translucent violet - pink sapphire |
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Ruby in amphibolite. |
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The crystals engaged in rocks, rich in mica, have rough faces encrusted of biotite or muscovite, minerals |
which also exist at the state of inclusions, associated with magnetite and pyrite. |
Because of its hardness, its inalterability and its density, corundum constitutes a standard mineral of |
alluvia. |
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Polychrome Sapphire |
Blue Sapphire ( origin: |
Blue Sapphire ( origin: Ilakaka 1999 ) |
( origin: Iankaroka 1990 ) |
Andranondambo 1992 ) |
Found in the sandstones of Isalo in |
This sapphire comes from a granit, |
The stone comes from |
alluvium, the shape is rounded. |
its shape is intact. |
a metamorphic marble. |
The origin of the stone is a marble. |
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· The structure of crystals. |
It is R.J.Haüy who put forth the first assumption, confirmed 200 years later, on the structure of the |
crystallized material. He lets drop accidentally a calcite crystal which broke into small rhomboedrons. He |
supposed whereas the crystals were consisted of stacking small rhomboedrons elementary (that he called |
the "integral molecule"), he could reconstitute all known shapes of calcite. In a crystal lattice, three atoms |
or groups of atoms (nodes), which is not on the same line, determine a plan called reticular plan. But there |
is a great number of these plans: it is enough to choose nodes not strictly nearby. As the network is infinite, |
there is even an infinity of possible plans. The dimension of the faces does not play any role. During its |
growth, a face can develop more quickly than another. The angle that the faces make between them |
remains constant, since it depends on the network. This structure of the crystalline material explains the
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law of the constancy of the dihedral angles. |
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Triangular figure on a |
Scratches on a rare |
Stacking in macle |
Triangles on a translucent |
colorless corundum. |
colorless corundum. |
of a ruby. |
corundum. |
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The alluvial ruby deposit of Ambatovaravarana in the highlands, |
is located in the center on the picture, under the hill. © Image J. Darbellay |
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Your guide to GGGems |
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© All of the pictures on this website have been shot by gggems.com |
Alain Darbellay |
Text written by Alain Darbellay. |
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