[1][2] It can be seen in the Panamint Range and Funeral Mountains adjoining Death Valley, within Death Valley National Park; and in the Spring Mountains in Clark County.
[1][3] It has members of quartzite, shale, sandstone, and dolomite.
[1] It preserves scattered olenellid trilobite and archaeocyathid fossils in upper part of formation, dating back to the Ediacaran period of the Neoproterozoic Era and Lower Cambrian Period of the Paleozoic Era.
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