Topaz is a pretty stone. 

Topaz is a very hard stone. 

Some people find these stones in Brazil. They also find them in Russia. Miners dig deep holes to get them.
Orange topaz is a special stone. It is the birthstone for November. It is also the stone for Utah. 
Topaz is a very hard mineral. 

Many places in the world have topaz. Brazil and Russia are two popular places to find it. Miners often use open pits to get the stones. 
Topaz is a semiprecious stone. This means it is a lovely gem used for jewelry. Orange topaz is the birthstone for November. It is also the state gem of Utah. 
Topaz is a beautiful mineral used as a gemstone in jewelry. 
Many colors of topaz exist in the world. In its natural state, topaz is often colorless or clear. Sometimes it looks golden-brown or yellow-orange. These colors happen because of tiny impurities in the stone. People can change the color of topaz using heat or radiation. This can turn the stone deep blue, pink, or purple. 
People have known about topaz for a very long time. The name likely comes from a Greek word for an island in the Red Sea. Ancient people believed topaz could protect travelers from danger. In the Middle Ages, some thought it could help with fevers. People in India believed wearing it over the heart gave intelligence. The name we use today was first applied to this mineral in 1737. 
Topaz can be found in many different places. Brazil and Russia are two of the most popular sources. 
It is easy to tell topaz apart from other stones. Topaz is much heavier than a similar stone called citrine. It also feels very smooth and slippery when you touch it. You can even test it by putting it in a special liquid. Quartz will float in the liquid, but topaz will sink.
Topaz is a silicate mineral composed of aluminum, silicon, oxygen, and fluorine. Its chemical formula is AlSiO(F, OH). 
The internal structure of topaz determines how it looks and behaves. It belongs to the orthorhombic crystal system and the dipyramidial crystal class. The crystal structure alternates between sheets of fluorine and oxygen. Aluminum atoms occupy octahedral sites within this structure. Silicon atoms sit in tetrahedral sites.
Topaz comes in many different colors and varieties. In its natural state, it is often colorless or has a grayish cast. Trace element impurities can turn it pale blue or golden-brown. Some varieties, like pink or red topaz, occur when chromium replaces aluminum in the structure. 
The history of the word "topaz" is quite ancient. It likely comes from the Greek word *topázios*. This was the name for a mysterious island in the Red Sea. Ancient people mined a yellow stone there, which we now believe was chrysolite. The name we use for the modern mineral was first applied in 1737. 
Topaz is found in many locations across the globe. It is often associated with felsic igneous rocks like granite and rhyolite. Brazil and Russia are two of the most popular sources for the mineral. 
Scientists and industries use topaz for more than just jewelry. Because it is very hard, lower-quality topaz is used as an abrasive material. It is also used to create refractory materials. These are substances that can withstand very high temperatures. Topaz can even act as a flux in steel production. However, using it as a refractory material has environmental concerns. The process of calcining topaz can produce fluorine as a byproduct. This means the mineral has both beautiful uses and industrial roles.
It is possible to create synthetic topaz in a laboratory. One method involves the thermal hydrolysis of SiO2 and AlF3. When these are heated to between 750°C and 850°C, topaz forms. Another method uses amorphous Al2O3, Na2SiF6, and water. This mixture is heated to 500°C under 4,000 bars of pressure for nine days. 
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