An occurrence in the Camp Verde area. The occurrence is within a wash just west and north of the famous Camp Verde salt mine. Infrequent rains bring crystals down the wash near Salt Mine Road but the best pseudomorphs are to be found further north in the wash where they weather from soils along the banks and walls of the wash. Three types of pseudomorphs are known and include aragonite, calcite and gypsum pseudomorphs after glauberite. The aragonite and calcite pseudos are far more common in Copper Canyon while the white gypsum pseudos are much more common at the former mine site. The aragonite pseudos are often composed of spiky aragonite crystals faithfully replacing original glauberite crystals---these fluoresce a cream color under shortwave UV light. The calcite pseudos are a cream to yellowish color and can be found as exceedingly sharp crystals in the bed of the wash and weathering out at various places along the sides of the wash.
4 entries listed. 4 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. 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.
Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd. ed.: 232.
Slaughter, Dana S.; Collecting at Camp Verde, Arizona (unpublished paper).
Mineral and Locality Search Options