CORUNDUM: A VISUAL |
EXPERIENCE |
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Corundum is a special mineral, not
only because of its economic importance (in gem form it is ruby or sapphire;
and emery abrasive is a sub-gem form), but also because of its diversity of colors,
forms, associations, and source localities which makes it uniquely
attractive to collectors. The specimens illustrated
here are selected from our research/display collection to reflect this
diversity. (Click on thumbnail for larger photo.)
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In its pure form, corundum is a
transparent, colorless form of aluminum oxide, Al2O3.
It crystallizes in the hexagonal subsystem of the trigonal system.
Hexagonal prisms (such as the Kenyan sapphire on the left) and pyramidal
modifications (Burma, left and
Sri Lanka, right) are characteristic forms. |
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Perhaps the most attractive are the bipyramids such as the
classic Sri Lankan "geuda" crystal on the left. On the right
are two Brazilian hex prisms and a pyramidal cluster from
the original Kashmir alluvials - note white kaolin residue still
attached. |
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Hexagonal prismatic crystals occur in a
variety of proportions: "elongated", "prismatic" (I know,
redundant), "tabular", and "wafer", for example. Those to the right also show
some of the color variety. They are (left to right) from
"Zoutspansburg",
South Africa; Karnataka, India; Madagascar; Dat Taw Mine, Mogok
Stone Tract, Burma; and Tanzania. |
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Some of the finest wafer
crystals come from the United States; and one of the finest of these
(left) is this 6.62 carat flawless gem from the
Vortex Mine, Yogo Gulch, Montana.
The tabular ruby on the right is from the Dat Taw Mine, Mogok Stone Tract,
Burma. |
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Lateral faces of corundum
crystals are often "smooth" (Madagascar, left), "striated" (Burma, right),
or "layered" (India, second photo below). Extreme layering can produce
lovely, rose-like clusters (Russia, below far left). Terminal faces
can be "smooth" (Mozambique, left center), but are often "layered" (Burma, center,
and
India right center), or distinctively "triangulated" (Pakistan or Afghanistan,
far right). |
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Twins are common from some
localities, and produce specimens that the "crystal killers" (faceters)
hate but collectors love. The Vietnamese (far left) is a good
example of "contact twinning". Following are another contact twin from
Afghanistan (illustrated in
Lapis Magazine, ex coll.
Andreas Weerth), "interpenetrant" twins from
India
and Transvaal, and a neat, floppy-eared "puppy dog" twin
from Viet Nam. |
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Below: two clusters from
Viet Nam
("The Rocket Ship" and a pyramidal cluster), one
from
Sri Lanka ("The
Goldfish"), and two from Tanzania
(Longido
and Morogoro
respectiely). |
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Bottom Row: Ilmen
Mountains, Russia, Nepal (Chumar Mine), Spider Mountain (Mogok,
Burma), and two other Mogok specimens. |
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Polycrystalline or even massive
corundum can be interesting, as these three specimens from the vicinity of
Franklin, North Carolina portray. All of these (collected before 1850)
may have come from Corundum Hill, just outside
Franklin, which was mined for
emery (they ground this stuff up)! |
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Many corundums are found in river
gravels. Perhaps the most famous of these are the
Montana alluvial deposits (top left photo).
Left Photo: The
seven sapphires illustrated on the far left from
Rock
Creek (Gem Mountain) and and the four on the right from
Dry Cottonwood Creek were gifts of Marc Bielenberg to
Louis Zara. The hot pink in the upper center was
given to me by Ben Duffey. Bottom
left photo indicates the variety of colorful sapphires
that can be recovered from the Umba Valley, Tanzania
alluvial deposits - these select specimens show little or
no abrasion |
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On the top right above are two waterworn specimens
from the Mano River which runs along the borders of
Guinea, Liberia, and
Sierra Leone in
West Africa. Below
them is a ruby cobble found in the gold dredge tailings of
Alder Gulch, near
Virginia City, Montana. |
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Corundum occurs
in nature with (or after) a variety of other minerals. Calcite
is the most common. Note how the snow white color contrasts
with the brilliant red of the Viet Namese ruby (far left). The
second photo shows a 2-1/4" long gem ruby from
Afghanistan in a contact
between grey and white calcite. On the right is very rare
"Ruby Cave", Burma specimen, which apparently formed in nepheline calcite. |
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Left to right: nepheline provides the matrix for a historic
Sri Lankan specimen, rubies
in syenite from Viet Nam, and a remarkable large fist cluster of gem rubies in zoisite from the classic
Longido, Tanzania locality. |
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These three American specimens are
unusual. First is "Barney, the Dinosaur" (rubies in smaragdite) from
Chunky Gal Mountain, North Carolina. Second is a nodule of blue/white
corundum altering to margarite mica from Franklin, North Carolina.
Third is a Yogo Gulch, Montana sapphire in lamprophyre(?) matrix - note the
rock
is not green! |
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Here are some true rarities
- in fact, in our experience they are unique! The first is
ruby with fossils - crystallized in a mud pocket with opalized snail
shells; from the John Saul Mine in
Kenya (given by John Saul to Cal Graeber). The second is a detail of an unusually aesthetic association of ruby with diopside,
from Tanzania somewhere. The third shows a trio of pink
elongated doubly terminated prisms , allegedly from
Morogoro, Tanzania. |
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Some corundum localities are well
known for the gems they produce - and among these, Burma and
Kashmir set the
standard against which all gem rubies and sapphires are measured.
However, as a mineral collector, I find others just as attractive (and often
more affordable)! To illustrate the geographical variation, we conclude this photoessay
with some armchair travel. See GALLERY
pages for more photos and information. |
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Karnataka (Mysore) Province,
India has several holes in the ground that have produced remarkable,
large ruby crystals, ranging from brownish to purplish red. The
ones pictured to the right weigh up to 20 pounds. |
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Other Karnataka localities produced
"watermelon ruby" encapsulated in blue zoisite rind
(often misidentified as corundum or kyanite -far left), doubly terminated rubies
in gneiss (near left) and huge blocks of massive ruby/sapphire
corundum suitable for carvings such as this 45-lb. "Ganesha" (right).
(Carving is property of Anil Dholakia.) |
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Nepal is not a large producer
of corundums, but look at these! The cluster on the left (2 views), from
the Chumar Mine, Ganesh Himal, is one F. John Barlow described in a personal letter: "This, without question,
is the finest ruby crystal group ... and I
don't believe (it) will ever be topped." The details on the
right show unique "shark fin" projection, green fuchsite
mica, and unique "chain" of crystals seen on several of the "original"
ruby specimens
(ca. 1981) from the Chumar Mine. The pale blue sapphire in matrix is from recent artisanal operations in
the northeastern Taplejung region. |
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European localities are not
known as major gem sources, but occasionally they produce important
mineral specimens. The tabular ruby on the left, from the
Sivec Mine near
Prilep, Macedonia, weighs over four pounds, and is apparently the largest ever found at
the site. Center photo is one of my favorite crystals from the
Ilmen
Mountains, Russia. On the right is a superb cluster of terminated
rubies in gneiss from the Klegaassen Pegmatites near
Arendal, Norway. |
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Burma
(Myanmar) is arguably the source of not only the finest gems but also
the most interesting and varied mineral specimens. Top: mass of bipyramids from
Spider Mountain, Mong Hsu
cluster, extremely cavernous complex crystal from
Dattaw Mine.
Bottom: Pastel striated crystal from Ka Baing, rare brown gemmy
crystal from Mogok, pair of large gem rubies from
Kuat Sar
Taung (Mogok). |
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So, I hope you have enjoyed this
look at specimens from our collection of this most remarkable mineral. In all, there are over 2,300
catalogued specimens and lots,
including many of types or from localities not illustrated here. Please e-mail me
at collector@corunduminium.com
if you are interested in anything related you
do not see
here. I shall try to reply to each query as soon as possible, either personally or by posting the info on the
"What's New" page of this website. This is a one horse show; so please be
patient.
Will Heierman
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(Author's Note: As I am a mineral collector
not trained as a geologist or mineralogist, there may be technical
errors or more precise ways of saying things that should be brought to
my attention. If you see one, please e-mail me at webmaster@corunduminium.com.) |
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