Pg. 272; 1896, USGS 17th Ann. Rpt., pt. 2, p. 289. Bunker andesite. Holocrystalline, fine-grained, massive andesite, carrying hornblende, augite, and biotite. Age is Tertiary (Eocene).
Forms greater part of Rosita Hills. Occurs in Bunker Hill, Sugar Loaf, etc., Silver Cliffs-Rosita region, central southern CO.
Source: US geologic names lexicon (USGS Bull. 896, p. 294).
Not known how much of Bunker is intrusive or extrusive. Massive nature, lack of flow structure, and coarse grain suggest intrusive origin. Basal contact at some eastern localities is flat suggesting Bunker was a lava flow or sill at those localities. Western contacts are intrusive. Bunker flows are unconformable on the Rosita Formation. Is mineralogically a trachyandesite. Has a syenodiorite-porphyry facies. Makes up stocks, flows, dikes, sills. Age not stated. Geologic map. Oligocene age.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Is part of the late cycle (27 to 26 m.y. b.p., or Miocene) of volcanic rocks at the Rosita center, Custer Co., CO in the Las Vegas-Raton basin.
Source: GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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