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Generation realestate 1Forms identified dillon from G1 crystals are the prisms montana {011}, {101}, and {210}; the pinacoids {010} and {001}; and the pyramids {111}, {211}, and {112}. Formation of clear prismatic crystals with two termination types (referred realestate to as type dillon and montana and realestate 1 and type 2) characterize this group. dillon Specimens showing only this generation are rare because G2 and/or G3 montana frequently cap or completely realestate and dillon overgrow them. All specimens have montana flat lustrous realestate prism faces dominating the long axis; dillon in some cases, this habit gives the bases of some of the crystals a slight amber tint because they montana are overgrown by colored G2 material.
Davis, W. E., and R. E. realestate Hunt. 1956. Geology and oil production on the northern portion of the Cedar Creek Anticline, dillon Dawson County, Montana. In First Annual Williston Basin montana Symposium, North Dakota-Saskatchewan Geological Survey, realestate 121-29.Gill, J. R., and W. dillon A. Cobban. montana 1966. The Red Bird section of the Pierre Shale in Wyoming. U.S. Geological Survey professional paper 393-A.
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