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A gemstone that occurs in a wide range of natural and treated colors.

topaz crystals of various colors

Colored Topaz Crystals: A collection of topaz crystals of various natural colors - sherry, imperial, pink, and purple. Most topaz crystals are colorless. Most topaz in commercial jewelry has been heated, irradiated or coated to improve its color. Specimens and photos by Arkenstone / www.iRocks.com

What is Topaz?

Topaz is a rare silicate mineral with a chemical composition of Al2SiO4(F,OH)2. It usually forms in fractures and cavities of igneous rocks such as pegmatite and rhyolite, late in their cooling history. It is also found as water-worn pebbles in stream sediments derived from those igneous rocks.

Topaz is a well-known gemstone sold in a wide variety of attractive colors. Some of these colors are natural, while others are produced by treating pale or colorless topaz with heat, radiation, or metallic coatings.

Contents:   Physical Properties | Gemstones | Gem Treatments | Geologic Occurrence

Physical Properties of Topaz

Chemical Classification Silicate.
Color Natural colors include: colorless, yellow, orange, red, pink, blue, green. Occurs in a wide range of treated colors, most often blue.
Streak Colorless - harder than the streak plate.
Luster Vitreous.
Diaphaneity Translucent to transparent.
Cleavage Perfect basal cleavage.
Mohs Hardness 8
Specific Gravity 3.4 to 3.6
Diagnostic Properties Hardness, prismatic crystals, sometimes striated, cleavage, specific gravity.
Chemical Composition Al2SiO4(F,OH)2
Crystal System Orthorhombic.
Uses Gemstone, Mohs hardness index mineral.

Physical Properties of Topaz

One of the best-known physical properties of topaz is its hardness. It has a hardness of 8 on the Mohs hardness scale. It also serves as the Mohs hardness scale index mineral for a hardness of 8. Every student who takes an introductory geology course learns about the hardness of topaz. Diamond, corundum and chrysoberyl are the only commonly-known minerals that are harder.

Most topaz is colorless or milky. Yellowish and brownish colors are also common. Natural pink, orange, red, purple and blue topaz are rare and valuable if they are of gem quality.

When allowed to grow unrestricted, topaz forms orthorhombic crystals, often with striations that parallel the long axis of the crystal. It also has a distinct basal cleavage that breaks perpendicular to the long axis of the crystal. This cleavage makes topaz a more fragile gemstone than its hardness of 8 would imply. Hardness is the resistance to being scratched, but the ability to resist breakage is a property known as tenacity.

Topaz has a specific gravity that ranges between 3.4 and 3.6. This is quite high for a mineral composed of aluminum, silicon and gaseous elements.

Blue Topaz: Faceted ovals of two colors of blue topaz that are popular today. On the left is a "Swiss Blue" topaz weighing 2.02 carats. On the right is a "London Blue" weighing 2.26 carats. Both stones were colorless topaz mined in Brazil, then irradiated and heated to produce the blue colors. Topaz with treated blue color is the most common color of topaz in commercial jewelry today.

topaz treatment methods

Topaz Treatment Methods: Colorless topaz, also known as white topaz, (top left) can be irradiated and heated to produce gems with a blue color (top right). Irradiation alone can produce a pale pink color (bottom right). Coating with certain metallic oxides can produce a vivid pink color (bottom left). Most topaz in commercial jewelry today is colorless material that has been heated, irradiated or coated to improve its color.

Use of Topaz as a Gemstone

The name "topaz" and many language variants have been used for yellowish gemstones for at least two thousand years. At that time all yellowish gems were called topaz in many parts of the world. People who traded in gems did not realize that these yellowish stones were of many different kinds.

Then, about two hundred years ago, people who traded in gems began to realize that these yellowish gems might be topaz, quartz, beryl, olivine, sapphire or one of many other minerals. They also learned that topaz occurred in a wide range of colors other than yellow. Today, gemologists know the full range of colors for natural topaz.

If you visited a jewelry store fifty years ago and asked to see topaz, you would likely be shown gems that were in the color range of yellow, orange and brown. Starting in the 1970s and 1980s the most common color that you would be shown began to be blue. This blue color was usually produced by treatments that converted colorless topaz into a more marketable gemstone.

mystic topaz

"Mystic" Topaz: Some topaz is heated and then coated with a metallic oxide to change its color or to produce an iridescent effect. These treatments are sold under the trade name of "mystic topaz." These materials are simply clear topaz with a coating that might not be very durable.

Topaz Treatments

Today most topaz offered in mall and department store jewelry stores at low to moderate price levels has been treated in a laboratory. Colorless topaz is heated, irradiated and coated with thin layers of metallic oxides to alter its color.

Natural blue topaz is extremely rare and usually is pale blue. Almost all of the blue topaz offered in stores is colorless topaz that has been irradiated and then heated to produce a blue color. "Swiss blue" and "London blue" are trade names for two of the most common varieties of treated blue topaz seen in today's market.

Natural pink to purple topaz is also extremely rare. These colors are often produced in a laboratory. The starting point is a stone cut from colorless topaz. It is first heated and then coated it with a layer of metallic oxide to produce the pink color. If coated stones are worn in jewelry, over time the coating often wears thin or wears through at points on the stone where abrasion occurs.

Some topaz is coated with a metallic oxide that gives the stone a multicolored iridescent luster. These stones, known as "mystic topaz" appear to change color if the observer moves the stone under a light. or changes the angle of observation. These coatings are also thin and can be worn through during wear.

Topaz Mountain Rhyolite

Topaz Mountain Rhyolite: Outcrop of stratified tuff of the Topaz Mountain Rhyolite, filling a paleovalley. These valley fills were once thought to be deposited by water, but now many of them are believed to have been deposited by ground surges of hot ash. The Topaz Mountain Rhyolite has many vuggy areas, which often contain champaign-colored topaz crystals. Located in western Utah. USGS image.

Geologic Occurrence of Topaz

Topaz has a chemical composition of Al2SiO4(F,OH)2. The fluorine in its composition is a limiting factor on its formation. Fluorine gas in concentrations high enough to form minerals only occurs in a few geologic environments.

Most topaz forms the veins and cavities of igneous rocks such as pegmatite and rhyolite. It forms during the late stages of magma cooling while hydrothermal activity delivers fluorine. Topaz occurs in pockets within pegmatites, in fractures that carried hydrothermal fluids, and in gas cavities within rhyolite.

Precipitating in cavities, topaz sometimes develops nicely-formed crystals. These crystals can have excellent clarity and be used as a gem material. Especially attractive crystals of topaz are popular with mineral collectors. They have the value of a mineral specimen and the value of a gem material.

Topaz is also found as water-worn pebbles in stream sediments derived from the weathering of pegmatites and rhyolites. These are often produced by placer mining.

Topaz is found in many locations worldwide where rocks like pegmatite and rhyolite are formed. It is only a minor mineral at these locations and it is considered to be a rare mineral on the basis of its general abundance.

Brazil is the leading source of gem quality topaz today. Sri Lanka is another important producer. Topaz is also produced in Nigeria, Australia, Pakistan, Russia, India, Zimbabwe, Madagascar, and Namibia. In the United States, Utah named topaz as its state gemstone.

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