Soapstone

Soapstone has become ubiquitously used as a carving medium by beginners and experienced journeymen and journeywomen sculptors, owing to its ease of working and its brilliant finish. It can be rapidly worked in detail with hand or power tools and can be brightly polished in beautiful hues. In its natural condition, it is earthy and mundane; one wonders why some sculptor first started to work this stone.

Geology

The geologic term for soapstone is talc or steatite; the two terms are synonymous. Talc is the name that you will find in a book of minerals; however, steatite will commonly be listed in the description. ReportedIy, the term steatite was used commonly during World War 1I to describe massive and machinable talc that could be turned into strategic products such as insulators and metal molds. There are many grades of soapstone, ranging from hard to soft and dense to flaky. Soapstone has a minimum of 20 percent of talc, but can contain several subordinate minerals.

Talc is phyllosilicate, from the same class of minerals as the micas. Technically, it is Mg3Si401O(OH)2, hydrous magnesium silicate, with a specific gravity ranging from 2.58 to 2.83. Talc is the indicator mineral for a hardness of 1 on the Mohs Hardness Scale. This mineral has a greasy feel, and is a very poor conductor of electricity and heat, the reason it is used 8S an insulator. Minerals that commonly are found in association with soapstone are cWorite. serpentine, magnesite, antigorite, pyrite and enstatite. Another mineral that is similar and can ouly be distinguished from talc by chemical or x-ray analysis is pyrophyllite, hydrous aluminum silicate.

Talc can be formed in two ways. It is the product of alteration of other rocks and minerals; it has been metamorphosed. It can be regionally altered dolomitic limestone or altered igneous rocks. Therefore, talc is commonly found in two different environments–massive deposits or veins. The alteration from the original rock, such as olivine, to talc is made in a water-rich environment at moderate temperatures of about 1300 degrees F. Commonly, the vehicle for the intrusion of water are shear zones along faults. While the formation of talc is not a direct result of the movement, the travel of water along the zone of weakness completes the process. The largest of bodies of soapstone come from regional metamorphism (burial) of large deposits of dolomitic limestone, a calcium magnesium carbonate. Some of the larger bodies in the world are located in Ontario Province, New York, North Carolina, Georgia, California, Austria, Madras and Italy. The smaller bodies tend to be narrow veins related to shear zones or igneous intrusions, and are commouly found in Washington, Virginia, and California.

Colors vary considerably: buff, brown, gold, red, orange, black, green, blue, and black with white marbling. Frequently, the outside of the rock may be red and this iron-oxide weathered zone will give way to another color on the interior of the stone. In the Pacific Northwest, the most common colors tend to be buff, brown and green.

Quarrying

Soapstone is obtained in several ways, depending on the size and accessibility of the deposit. One method with which many of those in the Northwest Stone Sculptors Association are familiar is hunting for cobbles and boulders on the slopes of a landslide deposit near Lake Wenatchee. (This deposit in now formally claimed by a commercial mining company. so it is no longer open to us.) The soapstone chunks are scattered about the landscape. and shovel and crowbar are necessary tools to liberate them. Sometimes small pieces can be found that are the right size to just toss in the back of the truck, whereas other larger behemoths must be cut in-place with a bow or chain saw to gain a manageable piece. Some of the larger boulders have soapstone on the outside, but then transition to another harder rock type on the interior.

In vein deposits, a backhoe is commonly used to loosen soapstone chunks, following the line of the vein. In the massive deposits or in very wide layers, the materials can be worked with a dozer and a backhoe together. It is common for the quarry operators to use the natural joints and weak planes in the formation to loosen the rock. Each piece is then trimmed into sizes ranging from 5 to 1,000 pounds, using chain, band and bow saws.

The waste materials from larger quarrying operations can be used for such things as cooking stones or foot warmers. and as additives in paint and cosmetics.

The Asbestos Quandary

Is there asbestos in the soapstone that we chip and pulverize right in front of our faces? The answer is yes and no. Asbestiform laths are obvious in some of the soapstone that we see; however. the asbestos particles do not have to be visible to the naked eye or even maguifying glass to be harmful. It has been reported that roughly 40 to 50 percent of the soapstone contains some asbestos. The only way to know for sure is to have the stone tested by a laboratory. Soapstone from the Lake Wenatchee area in Marblemount also tested clean this year. However, one stone does not a quarry make; different parts of a quarry can contain different accessory minerals. To be on the safe side; if you are not going to test each piece of stone that you work, treat the stone as if it does contain asbestos and wear appropriate breathing protection.

Tools and Flaws

Soapstone can be worked with both hand and power tools. The watch words should probably be “Don’t break the tea cup with a sledge hammer”. Tools used on soapstone should be appropriately suited and sized to this very soft rock. The use of a large hanuner or chisel can cause the unwanted splitting of the rock along an unnoticed plane of weakness. It is preferable to be on the safe side by using smaller hand tools. Because soapstone can usually be removed readily with rasps and rifflers, they should be used in the vicinity of a linear flaw.

Rasps, rifflers and then sandpapers are the orderly progression for the smoothing and polishing process. Water should be liberally used during the sanding to aid. in the polishing and to keep the pores of the wet/dry sandpaper unclogged.

It is common for there to be harder spots in the stone and even small pieces of iron pyrite. That will put a dent in your rasp! On the other hand, there are reports of small voids in soapstone, perhaps from the weathering of sulfides.

An interesting development was reported in a 1992 edition of Sculpture Nortlmest by Patty McPhee regarding the firing of finished soapstone pieces in a kiln. She reported that the fIring of pieces to cone 4 (about 1,600 degrees Fahrenheit) turned them very hard and darkened them. The firing increased the hardness from 1 to about 4 or 5. This could be a welcomed development to soapstone sculptors, but is still experimental. On the other hand, it has been reported by others that the fIring of soapstone has caused the destruction of a finished piece.

Appreciations

Thanks to sculptor Rich Baker of Ellensburg, Washington and to quarry operators John and Steve Pugh of Steatite of Southern Oregon, Inc. in Grant’s Pass, Oregon for sharing their knowledge and expertise of soapstone.