‡Ref.: Kellogg, L.O. (1906), Sketch of the geology and ore deposits of the Cochise mining district, Cochise County, Arizona, Economic Geology: 1: 651-659.
Cooper, J.R. & L.C. Huff (1951), Geological investigations and geochemical prospecting experiment at Johnson, Arizona, Economic Geology: 46: 731-756.
Cooper, J.R. & L.T. Silver (1964), Geology and ore deposits of the Dragoon quadrangle, Cochise County, Arizona, USGS PP 416.
Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd. ed.: 110, 133, 214, 318, 342, 392, 424.
The Texas Canyon is a prominent geological feature along Interstate highway 10. The canyon is marked by spectacular rock features, including 'balancing rocks', the result of weathering of the quartz monzonite intrusive of the Texas Canyon stock (pluton). The periphery of the pluton is host to the tungsten deposits of the Cochise District. The former Johnson Camp and its copper deposits and mines are also within sight of the pluton. Unfortunately, the state of Arizona had to post signs that defacing the rocks is a crime - it seems to have worked - they're strange and beautiful.
Mineralization is largely attributable to the intrusion of the pluton and metamorphic alteration of the surrounding rocks.
NOTE: Coordinates are for the Texas Canyon proper, at the center of the mineralized area.
|
|
Map Reference: 32°0'16"N , 110°8'19"W
This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.
|
10 entries listed. 10 valid minerals.
The above list contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database!
