Talc

Talc is composed of magnesium, silicon, oxygen, and hydrogen, and is the softest of all minerals, having the lowest possible rating on the Mohs scale of mineral hardness. It occurs in two main forms: steatite, a massive talcose rock, and soapstone, which is an impure form of steatite that also contains many other minerals such as mica and dolomite.

Talc is a hydrous magnesium silicate with a structure highly similar to pyrophyllite, which is also a hydrous aluminium silicate. Both minerals are phyllosilicates – a type of silicate exhibiting a crystalline structure in the form of parallel sheets and are commonly mined from the same mineral deposits. Given their almost identical physical properties, they can often be substituted for one another.

Asbestos mineral deposits can also occur alongside talc deposits and as a result they can be co-mined, however this is problematic for producers of talc-based consumer goods as small quantities of asbestos can be carcinogenic. There are growing concerns amongst consumers and industry of the contamination of talc with asbestos, highlighting the importance of properly testing talc products intended for human consumption.

Volumes of talc production and known reserves are not reported consistently across producing countries as many estimates do not disaggregate talc and pyrophyllite production figures. It is difficult to estimate the total known global reserves of talc, India and China were the largest producers in 2024.

Talc has a diverse set of applications across a variety of industries, such as in the manufacture of paints or as a filler material in many paper and plastic products. Its whiteness combined with the ability to prevent caking and absorb oils lend talc to many uses in the cosmetics industry, such as antiperspirants, powdered and liquid makeup, and baby powders. However, ESG issues and shifting consumer preferences have driven down profitability in the talc supply chain in recent years.