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GEOLOGY ARTICLE

Asbestos: what's in a name
by MIKE BALDWIN

07.29.06 -- Any of more than a dozen fibrous minerals can be classified as asbestos. Controversy still brews over which fibers constitute true asbestos. Two distinct families of the mineral exists. The asbestos mineral which is most often found lying beneath American communities contains chrysotile, the least toxic. All other asbestos minerals are in a family known as amphibole asbestos. Tremolite falls into the amphibole asbestos family.

OSHA (Occupational Safety and Health Administration) was the first agency to regulate asbestos. OSHA's rules, which rigidly define the mineral by fiber length and width, only covers chrysolite and five amphiboles, including tremolite. It's not that these six minerals are the only ones which contain potential asbestos hazards; rather, these six minerals are the only ones which were being widely mined and used commercially when OSHA wrote their asbestos regulations.

Over the years an EPA (Environmental Protection Agency) definition of asbestos has expanded to include fibers of a different size or makeup which may be just as toxic as the OSHA-defined fibers. For instance, asbestos contamination of the vermiculite mine near Libby, Montana, (where an epidemic of lung cancers and other respiratory diseases claimed the lives of 200 and sickened 1,200 others) was initially attributed to tremolite asbestos.

Further examination of the Libby mine found that only 6 percent of the material contained tremolite. 80 percent of the contaminating material contained winchite and the remainder contained richerite. Richerite and winchite are both chemically similar to asbestos, but are not classified as asbestos by OSHA standards. However, the health community does classify them as asbestos, because both have been found to trigger asbestos diseases. 1

ASBESTOS is a commercial term used for fibrous silicate minerals.  The fibers of asbestos are chemically inert as well as heat resistant and flexible.  Asbestos then can be different minerals, but most commonly it is CHRYSOTILE (a variety of serpentine).  Other asbestos minerals are tremolite, crocidolite and amosite. 2 

TREMOLITE mineral occurs as long, bladed crystals which are often twinned. It also forms as columnar, fibrous, or plumose aggregates, often radiating, and in massive granular habits. It is colorless, white, gray, green, pink or brown. The streak is white. Tremolite is transparent to translucent; it has a vitrous luster. It forms a series with actinolite. Tremolite forms in contact metamorphosed dolomites and serpentinites. 3

SERPENTINITE is a green, metamorphic rock consisting predominantly of serpentine minerals. Major constituents are chrysotile and antigorite. Medium constituents may include olivine, pyroxene, garnets, amphibole, chromite and magnetite. Calcite is almost always present. Colors vary from light gray green to green black. Bluish, brown and reddish tones sometimes occur. In the stone business serpentinite is usually just called serpentine like the mineral. Many serpentinites contain ores which are worth mining or are very closely associated with deposits (ie. iron, chromium, magnesite, talc and asbestos). 4

©2006 Information for this article was compiled by MAGS member, Mike Baldwin. Photograph of Fibrous Asbestos courtesy of Glendale Community College, Susan Celestian. Used by permission. Information used for educational purposes under the provisions of the "Fair Use Act of 1976".

References:
01 Janet Raloff; What's in a aname? Asbestos definitions can depend upon whom you consult; Science News; Vol. 170., No. 2; Science Service; Washington, DC; pg. 27; July 8 2006.
02 Asbestos; Glendale Community College Earth Science Image Archive; www.gc.maricopa.edu/. ../asbestos.htm. Accessed 29 July 2006.
03 Chris Pellant; Tremolite; Minerals; Eyewitness Handbooks; Rocks and Minerals; DK Publishing, Inc.; New York, NY; pg 155; 1992.
04 Walter Schumann; Serpentinite; Handbook of Rocks, Minerals and Gemstones; Harper Collins Publishers; New York, NY; pg 322; 1993.

 

   


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