
Huachuca Mountains -
GeologyRoger Weller, geology instructor
wellerr@cochise.edu last edited: 5/8/08
The eastern third of the Huachuca
Mountains is predominantly Precambrian granite, which lies in unconformable
contact with late Precambrian sediments, Bolsa Quartzite, and Abrigo Limestone
near the central part of the range. The western third of the range is a thick
section of Cretaceous sediments, including a fairly complete section of Bisbee
Group rocks, with several large Laramide dikes and sills present. A fairly
large granite stock, presumably of Triassic or Jurassic age, is exposed in the
southern part of the range close to the Mexico border.
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