CO-OP TRIP TO CHINESE CAMP

February 2009

FOR MAGNESITE & COMMON OPAL

Drew and Allen hold up their finds!

Casey inspects a piece of common Opal while Allen whacks away at a big chunk.

Jane Henry keeps a watchful eye while Ron Francis and grandson Cameron move a rather large specimen of Opal along the rails.

If only the Chinese Camp gas station were still open – what a great price!

Red Hills Magnesite
By Jenni Long

On Saturday, February 7th, several MLMS members joined a COOP field trip to the Red Hills of Tuolumne County. Most of us were very unfamiliar with one of the materials we were to collect, Magnesite. We were told it had been mined in these hills near Chinese Camp quite some time ago but the mine was abandoned and now opened for collecting.
So, what exactly could we do with our collected Magnesite? With a hardness of 3.5 - 5 on the Moh's Scale, it could be cut and polished and the harder specimens possibly tumbled. Once cut and polished the Magnesite resembles white turquoise. In fact, "the most common imitation of turquoise encountered today is dyed howlite and Magnesite." Magnesite's black veining makes it the most convincing "stand-in" for turquoise, once dyed the familiar blue color.
Magnesite has uses other than ornamental. It is the primary ore for magnesium and can be found in certain types of cement, paper and rubber. It also has uses in nutritional supplements (magnesium oxide).
How is Magnesite formed? The most widely accepted theory is that carbon dioxide-charged surface waters percolated down through fissures in serpentine. The magnesium silicates of the serpentine were then changed into magnesium carbonate. This makes perfect sense after being on location … there was serpentine everywhere! In fact this particular location is right in the middle of what's known as the "Sierra Nevada metamorphic belt," where one of the largest exposures of serpentine rocks exists.
Back to the Chinese Camp location, according to the Bureau of Land Management, several hundred tons of crude Magnesite ore were mined from the 1860s to the 1940s with most of the production occurring in the 1920s. Rumor has it, large quantities of the Magnesite made it over to China where it was cut, dyed and then sent back to the United States to be sold as imitation turquoise! So, how can you "test" your turquoise to make sure it's not Magnesite in disguise? Magnesite will dissolve in hot hydrochloric acid. But, if you don't happen to have some spare hydrochloric acid lying around, use your tongue! Because of micro-pores on the surface, your tongue will adhere to the porcelaneous material . . . mmm, tastes like chicken!
Sources:
www.onemine.org

wikipedia.org
www.blm.gov
The Peterson Field Guide to Rocks and Minerals