Talc and Soapstone

Talc, a hydrous magnesium silicate, is an extremely soft mineral—your

fingernail scratches it easily. It has a greasy or a pearly luster, and

its color is white, light green, or gray. When rubbed across a streak

plate, it leaves a white streak.

Talc cleaves perfectly in one direction, and the cleavage fragments are

thin, flat, and sheet-like. Its fracture is uneven. This mineral has a

soaplike or greasy feel, and it is sectile—a knife will cut through it.

Talc is not particularly heavy—it has a specific gravity of 2.7 to 2.8.

This mineral seldom occurs with a crystal shape. More commonly it is

massive and is granular or layered.

Talc is not always found as a single, pure mineral. In nature, it

commonly occurs mixed with one or more other minerals, such as

tremolite, anthophyllite, chlorite, and magnetite. This combination of

talc with other minerals forms a soft, greasy or soapy-feeling

metamorphic rock called soapstone. The talc in this rock may be

difficult to identify without special laboratory tests.

In Texas, talc and soapstone are found in Precambrian metamorphic rocks.

In west Texas, talc occurs in an area about 20 miles long (just north of

U. S. Highway 80 in the vicinity of Allamoore, Eagle Flat siding, and

Talc Rock siding) in Hudspeth County. Some of this talc is mined from

open pits and used by the ceramic industry to make wall tile. Some of it

is finely ground, mixed with insect poison, and used as insect powders

and dusts.

[Illustration: Talc schist from the Allamoore area of Hudspeth County,

Texas.]

Deposits of soapstone, containing talc, occur in the Llano uplift area

of central Texas with schist, gneiss, and serpentine rocks in

northeastern Gillespie, northwestern Blanco, and southern Llano

counties. Smaller deposits occur in northeastern Mason County and in

northwestern and southeastern Llano County.

The Llano uplift area soapstones are light green to light buff. It is

thought that some of them were once igneous rocks that contained

magnesium minerals. Fluids, along with great heat and pressures below

the earth’s surface, changed these igneous rocks into soapstone.

Some of this Llano uplift area soapstone is mined from open pits near

Willow City in Gillespie County. It is used mostly in making insect

powders and roofing granules. In addition, some of the central Texas

soapstones have been used for hearths and for fireplace linings.

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