|
Post by arappaho on Dec 14, 2010 10:30:18 GMT -5
Too cold to work today so I'm cleaning out some pics and thought I'd post these before deleting. One thing that makes sourcing the rhyolite that artifacts are made of in this area so difficult is the vast array of types, textures and colors found at each outcropping of the rock. There can be dozens of different looking materials per acre of outcrop, and even a variety in the same rock. Rhyolite was often lain down layer upon layer. For example in this piece; I struck this rock on the left side and the force traveled along the plane of that dark rough textured material until it hit the lighter finer grained layer on the right. You can see how the force dipped when it hit the different material. The lighter "creamy" looking stuff would be much better material for making tools with. It would knap better. Here are a few more pics. I put the piece with the "wave" back in place on the lower one and then spritzed some water on it in the last pic to bring out some of the color. There are hundreds of varieties of this stuff, which is what makes hunting it SO interesting and exciting, I'm sure you all will agree. ;D Thanks for looking, Joe
|
|
|
Post by rockshine on Dec 14, 2010 11:21:35 GMT -5
Thanks for the mini-tutorial, Arappaho. Explanations such as yours are much more informative than seeing a poorly reproduced photo in a mineral id book which may give a lot of scientific/technical data but does nothing to help the amateur rocker actually id a less than perfect specimen in the field. When I encounter collectors on Chunky Gal Mountain who are new to the site, the most common comment is, "But this doesn't look like the picture of Ruby in the book."
|
|
|
Post by arappaho on Dec 14, 2010 16:13:29 GMT -5
Thanks, rockshine. And you are right, the pics in the books sometimes do little to help develop an eye for in the field. Joe
|
|