Tiger's Eye, Hawk's Eye, Cat's Eye

 

last modified: Tuesday, 26-May-2009 03:44:48 CEST

Document status: inconsistent, some images missing


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Specific Properties

The most obvious property and the reason for its use as a gemstone is the silky shine that can be seen in polished, and especially in tumbled and cabochon-cut stones. All "eyes" show a wavy pattern of parallel lines that seem to move when the stone is turned. Smaller specimen will show only one or two long lines. This effect is named chatoyance because its look resembles an eye of a cat ("chat" is French for cat). It can also be seen in other minerals, for example in chrysoberyl, which is then named "oriental cat's eye". The chatoyance is a result of the fibrous structure of tiger's eye, hawk's eye, and cat's eye.

Hawk's eye is a partially silicified fibrous blue-gray crocidolite asbestos, so its fibrous structure is due to embedded fibers of crocidolite in quartz. It is usually very dark and almost opaque.

In tiger's eye the crocidolite fibers appear to have been fully replaced by quartz and the hydrous iron oxide goethite, FeOOH, the latter being responsible for the yellow-brown color. Though brighter than hawk's eye, tiger's eye is still almost opaque. The former fibrous structure is preserved in the orientation of the small columnar quartz crystals that grew perpendicular to the walls of the vein. Due to its fibrous structure, tiger's eye has a somewhat splintery fracture, not unlike wood.

Cat's eye is typically more translucent and brighter, and occurs in a variety of colors, green, yellow, brown, and rarely blue. The cause of its chatoyance can be embedded fibers of asbestos, as well as actinolite fibers.

Asbestos is a well known useful but hazardous material and can cause lung cancer, but its dangerous fibers are well embedded in hawk's eye and cat's eye and pose no danger for its owner. They are completely replaced by quartz and iron oxides in tiger's eye.

According to the more common theory, tiger's eye would present a pseudomorph of quartz after crocidolite. Occasionally hawk's eye shows areas of yellow color, corresponding to tiger's eye, and this indicates that hawk's eye represents an intermediate step in the alteration of crocidolite to quartz and iron oxides. This assumption is further supported by the fact that both tiger's eye and hawk's eye occur in the same veins as crocidolite, however in general only at places where these veins appear at the surface. This top layer is said to have been silicified starting from the surface. If one follows a vein into the ground, one will first find tiger's eye, then at most places after a few meters hawk's eye, and finally crocidolite asbestos. So the silicification at most places extends further into the ground than the oxidative alterations, and both processes are considered secondary - they apparently occurred after the crocidolite veins have formed, the silicification only for some period in time, while the oxidation is an ongoing process.

I should mention, however, that recently objections have been raised about this theory. These objections are mainly based on mineralogical, in particular crystallographic observations on tiger's eye and hawk's eye specimen that support a syngenetical (simultaneous) formation of crocidolite fibers and quartz.

 

Occurrence

Tiger's Eye and Hawk's Eye occur in cracks of rock that once have been filled by asbestos fibers. The cracks and clefts are rarely more than a few centimeters wide, but may extend over several meters, resulting in platy specimen.


 

Locations and Specimen

Most tiger's eye and hawk's eye comes from the Asbestos Mountains near Griquatown, South Africa.
Cat's eye is found in India and Sri Lanka.


South Africa


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This is a close-up of the tumbled tiger's eye on the image on top of this page.



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This is the flip side of the specimen from Griquatown in the image on top of this page, showing a little more detail. On the left and right side of the specimen there one can see material of the host rock that formed the walls of the cleft. The asbestos fibers initially grew straight, of course, and were subsequently bent when the walls of the cleft were displaced. Quartz would have been broken, but asbestos is flexible (fire-proof fabric used to be made of it) and the fibers assumed a sigmoidal shape. The fact that there are two sigmoidal zones, a narrow one to the left and a wide one to the right might reflect varying degrees of stiffness of the fibers across the cleft.



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A tumbled blue hawk's eye, probably from South Africa.


 

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