 | near Franklin, Washington |
 |
GEOLOGY
Cretaceous-age quartz monzonite - Fractures and joints within quartz monzonite host uranium mineralization at shallow depth. Uranium-bearing host rock was first discovered in this area by prospectors with Geiger counters during the mid-20th century. Several Washington occurrences have supplied the collector market with thousands of fine autunite specimens, some of which are considered to be the best ever recovered (Ream, 1991). The premier occurrence was the Daybreak mine (or Dahl lease) near Mount Spokane east of Elk, Spokane County. World-class autunite specimens were produced during active uranium mining for a short time in the mid-1950s.
MINERALS
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| Ca(UO2)2(PO4)2-10H2O - Typically dark green compact groups of fanlike crystals to 3 cm |
| Ca(UO2)2(PO4)2-6-8H2O - Yellow-green pseudomorphs caused by dehydration of autunite. Many exisitng autunite specimens exhibit meta-autunite rims due to partial dehydration. |
* photographed
AUTUNITE with META-AUTUNITE |
Ream, Lanny R. (1991), "Two Autunite Localities in Northeastern Washington," Rocks & Minerals Vol. 66, No.4, pages 294-297
