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Willemite
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| Formula: |
Zn2SiO4 |
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Hexagonal |
Space
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R3 |
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Overview
Willemite is an abundant component of the Zn-Mn-Fe orebodies at both
Franklin and Sterling Hill, and was mined in great quantities for its
zinc content.
Willemite fluoresces a brilliant
yellow-green under short-wave ultraviolet light, and this property
was exploited by New Jersey Zinc Company workers monitoring ore
concentrates, and involved in spot-assaying or surveying of underground
workings.
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Willemite.
Massive, gemmy green specimen. Franklin, NJ. Width 8 cm.
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Willemite is a silicate of zinc with the same structure as phenakite,
a rare beryllium mineral.
Zinc and silicon tetrahedra share corners to form hollow 'tubes'
parallel to [0001]. The mineral crystallizes in the hexagonal system
with rhombohedral symmetry.
Most crystals are elongate on [0001]; some microscopic crystals
exceptionally so, forming fine hair-like growths.
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Willemite
crystal structure. Coordination polyhedra (and a few atoms) shown. Left, views
normal to c-axis. Right, viewed down c-axis. Zinc filled tetrahedra are
green; silicon filled tetrahedra are blue.
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Willemite.
Typical forms present on microcrystals. Crystals are almost always elongate on [0001]. See
figure 118 in Palache (1935).
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Willemite is found in grains, massive, and in crystals.
Crude, opaque crystals many centimeters in length have been found. Smaller crystals
formed in open late-stage vugs are often exquisitely formed, are well described in
Palache
(1935), and make superb SEM study material. |

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Crystal drawings of willemite from Palache
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SEM view of a
willemite crystal. Franklin, NJ. Width 0.1 mm.
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Willemite crystals
in vug. Franklin, NJ. Width 0.6 mm.
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Willemite is most commonly green, but it has an extremely
diverse color range: white, yellow, red, orange, brown, black and blue varieties are known
from the area.
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Willemite. Small green and yellow gemmy
samples. Franklin, NJ. Width 5 cm.
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Red willemite.
Granular ore sample, with minor franklinite (black). Sterling Hill, NJ. Width 10 cm.
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Some of this color variety is due to the presence of microscopic
inclusions; nearly all Franklin-Sterling willemite makes fascinating
material for study under the microscope.
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Willemite.
Close-up view of a polished slab of massive, gemmy green willemite. Franklin, NJ. Width 4
cm.
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Be sure to also visit the fluorescence pages for willemite.
For further information on willemite, consult Dunn
(1995).
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'Radiating' willemite.
Classic sample of white willemite in radial aggregates of thin
needles. Franklin, NJ. Width 12
cm. Fluorescing (green) view under shortwave UV light.
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