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  RJH_7817.JPG - These rocks are the inland contemporaries of the Temblor Formation at sharktooth hill.   The big pink layer is a large rhyolite tuff from what must have been a nearby caldera.  
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 These rocks are the inland contemporaries of the Temblor Formation at sharktooth hill. The big pink layer is a large rhyolite tuff from what must have been a nearby caldera.
Camera: NIKON D700 | Date: 2/18/11 1:53 PM | Resolution: 4256 x 2832 | ISO: 200 | Exp. Time: 1/250s | Aperture: 8.0 | Focal Length: 48.0mm (~48.0mm)
Total images: 192 | Last update: 2/26/11 6:32 PM | Help