Choosing what type of rock is the trick. This is California; we have a great many geological environments, and many rock types could be described as "typical". We live next to the Sierra Nevada batholith, so a big chunk of granitic rock could be used. But that's kind of plain. We are in the Great Valley, so we could go with a big piece of sandstone or siltstone from the Great Valley Sequence, but such rocks are not very durable, and the rocks we choose may very well be in place fifty years from now.
We decided to seek out two rocks that are found very close to our campus, in the Sierra Nevada foothills. The first is serpentine, the metamorphic product of bringing the Earth's mantle peridotite up through the crust under high pressure to the surface. It is relatively rare in most places, but is common throughout much of California. It is unique enough that it was declared our state rock in the 1960s, joining our state mineral gold, and our state gemstone benitoite.
The problem was finding an appropriate piece of the right size. There are lots of outcrops along the highway 49, but few active quarries. Serpentine was an important source of chromite, magnesite and mercury, but those ores are mostly imported these days. They were usually mined during wartime (WWI and WWII especially). Serpentine was an important source of asbestos, which was a wonderful fireproofing material, but later it was also found to be a cause of lung cancer and mesothelioma. Asbestos became a scary material (all those lawyer commercials on late night TV may have clued you in to this), and serpentine is no longer mined for that purpose. We finally located a nearby quarry that was still active, grinding the material for road beds.
The other problem with serpentine is that on the journey from the depths of the mantle to the Earth's surface, the rock is internally sheared and fractured. It is not always durable enough. So we were invited to search the quarry for a good piece, one that could survive a bit of rough handling. Looking at the steep quarry face, and all the talus that has fallen from the edge, a possible candidate emerged. Look at the photo above (note Mrs. Geotripper up on the side of the quarry for scale): are there any chunks of rocks that have fallen and survived the impact? Yup, I saw it too, looking a bit like a turtle shell.
Here it is up close (below). Not just a big chunk, but one that is covered with the beautiful polished green surfaces that resemble jade. Just the perfect rock for school kids to touch when they are walking into the entrance of the museum. We discussed price with the quarry operators.
"How much per pound?"
"Oh, we sell by the ton. Say $30 per ton."
"We'll take two!"
First mission accomplished!
Then we were off to the Carson Hill Mine Quarry to seek our next objective, a much rarer prize: A big piece of mariposite. Mariposite is a mineral that is practically unique to our region (Mariposa is the Spanish word for "butterfly"; it is the name of the southernmost town in the Mother Lode). It is a chromium bearing mica that is somewhat related to fuschite, but the color is a very bright apple-green. It is often closely related to the gold-bearing quartz veins of the Mother Lode, and I have seen some beautiful samples that contain visible gold. It's a bit harder to find large samples, but the Carson Hill Mine, a Gold Rush era gold mine turned stone quarry, said they had some candidates we might like.
Photo by Mrs. Geotripper |
We pulled into the corner where they warehouse the big chunks of mariposite, and we started climbing over the boulder pile looking for the perfect sample. There was more in this one pile than I've ever seen anywhere else! How to choose?
We looked and looked and settled on several possibilities. Talking price? It's $0.20 a pound. You must choose wisely....
Our second mission was accomplished. Two multi-ton boulders collected! Of course, I couldn't resist collecting a slightly smaller piece of serpentine for the department...
Photo by Mrs. Geotripper |
That is a great quarry to visit, if you look up the side of the pit on the far side you can see the old mine shafts. It helps to have one of the workers point them out.
ReplyDeleteDoug N
Nice rocks.
ReplyDeleteOh, Gary, I'm so disappointed. You were collecting serpentinite, not serpentine. The differentiation between the rock and the mineral struck me the first time I ever saw a piece of serpentinite in thin section under a microscope.
ReplyDeleteSorry, meant Garry, not Gary. Slip of the keyboard. BTW, Mrs. Geotripper is an excellent photographer.
ReplyDeleteOh, I was just following the lead of the experts, i.e., the California State Legislature, which declared the mineral serpentine the state ROCK, and who never even mentioned rock serpentinite. :)
ReplyDeleteThose are some BIG rocks!! i think sometimes people look so hard for the small stuff, they lose sight of how good the bigger stuff can look :)
ReplyDelete