Earth Science Museum
University of Waterloo
200 University Ave. W.
Waterloo, Ontario, Canada, N2L 3G1
Phone: (519) 888-4567 ext. 32469
Back to Rocks and Minerals Articles
The mineral talc is a hydrous magnesium silicate. A massive talcose rock is known as steatite, and an impure massive variety is called soapstone.
The name talc is believed to be derived from the Arabic word talc or tolk meaning mica, since talc forms mica-like flames. The present name was given by Georgius Agricola in 1564. Kerite is a common name also used for talc.
Talc. Grimsthorpe, Ontario. University of Waterloo Earth Sciences Museum Collection.
There are many uses of talc, especially as an industrial mineral because of its resistance to heat, acid and electricity. Because of these resistances it can be used as counter tops, electrical switchboards, ceramics, and insecticides. It is most commonly known as the main ingredient in talcum powder. It is also an important filler in paints and rubber. Talc is used commercially because it can retain fragrance, lustre, purity, softness and whiteness. Some of the major markets for talc are ceramics, pain paper and plastics. Ground talc is used in roofing and cosmetics.
Talc can be blue, pale green, gray, pink, white, yellowish or brownish white to almost silver. Its lustre is dull to pearly or greasy. What determines these characteristics are its natural or artificial impurities. Talc only has a hardness of one on the Moh’s scale of hardness. This translates into a very soft material, which results from its layered nature. Naturally, this substance is hydrophobic (dislikes water), and tends not to absorb water, therefore giving some of its favourable water-resistant characteristics.
Both of these minerals are nearly identical, each being very soft. Talc is one on Moh’s scale of hardness, and pyrophyllite is one to two. Both can be easily crushed and cut, because they are so soft. Also both have perfect cleavage in one direction, allowing these minerals to break into thin sheets. Each feels greasy to the touch, this is why talc is used for a lubricant, and both are formed in metamorphic environments.
Talc. Madoc, Ontario. University of Waterloo Earth Sciences Museum Collection.
Some replacements for talc when manufacturing ceramics are clays and pyrophyllite. Kaolin and mica can be substituted instead of talc in rubber paint and plastics production. For paper production, kaolin can be used in place of talc. There is an abundance of talc with sufficient amounts for many decades to come, but some of these alternatives may be cost-effective depending on the cost of talc. China is the world’s top producer of Talc, followed by the U.S. and Japan.
Talc was first discovered on a farm in Madoc in the 1880s. It was 1896 that the Henderson Talc Mine came into production. In 1911 the Conley Mine opened in the adjacent property, where there contained a northeast extension of the Henderson ore body. The mines went through various owners until 1937, when the Henderson and Conley mines were merged into one under the name Canadian Talc Limited. Again in 1951 Canada Talc was bought by Canada Talc Industries Limited. More than 800,000 tons of high-grade talc has been mined from this deposit to date.
... To be continued
Earth Science Museum
University of Waterloo
200 University Ave. W.
Waterloo, Ontario, Canada, N2L 3G1
Phone: (519) 888-4567 ext. 32469
The University of Waterloo acknowledges that much of our work takes place on the traditional territory of the Neutral, Anishinaabeg and Haudenosaunee peoples. Our main campus is situated on the Haldimand Tract, the land granted to the Six Nations that includes six miles on each side of the Grand River. Our active work toward reconciliation takes place across our campuses through research, learning, teaching, and community building, and is co-ordinated within our Office of Indigenous Relations.