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We were traversing a stretch of the Calaveras Complex, a sequence of Permian-Late Triassic rocks that formed in a subduction zone, where the oceanic crust of the Pacific Ocean basin was forced beneath the western edge of the North American Continent. The rocks were churned up into a mess of slate and chert called a melange. The melange includes huge blocks of limestone (marble, actually), greenstone, and other metamorphic rocks that can be several miles across. It is one of the marble blocks that provided the huge slab that served as the base for the grinding stones.
Marble, like limestone, is composed of calcium carbonate (the mineral calcite), which many people associate with cavern development. Indeed, our previous stop that day was a tour of a beautiful little cave only two miles away. The region is pretty well honeycombed with dozens of caves that just beg for exploration (contact the local speleological society if you are interested in learning more about it). Pictures of our tour of the cave will be coming soon.
The Other California is my continuing series of the lesser known corners of my beautiful state, and the unique geology that can be found there. I don't know the entire state as well as I wish, and would welcome a guest blog on one of your favorite hidden places!
The Other California is my continuing series of the lesser known corners of my beautiful state, and the unique geology that can be found there. I don't know the entire state as well as I wish, and would welcome a guest blog on one of your favorite hidden places!
2 comments:
Marble is not the most durable choice for a grinding stone, but I'd have to guess that the Miwoks who used these didn't suffer much acid indigestion and maybe not so much tooth wear as others who used more durable (quartz & feldspar based) mortar & pestles.
I have to agree with Ron about the native health issues. Glad you got to explore a cave while there.
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