View northwest into Cottonwood basin from the slopes adjacent to the previously mined pits.
View northwest into Cottonwood basin from the slopes adjacent to the previously mined pits. The white areas in the basin are exposures of lake sediments from a 14 to 16 million year old lake which filled the basin, and which occurred beside the rhyolite volcanic center that is associated with the previously mined mineralization at Hog Ranch. The Hog Ranch property extends into this area and encompasses prospects which occur in the lake sediments such as the Cameco and Airport zones, which may be associated with rhyolite dykes that intrude the lake sediments.
You can view the Previous HR Photo Gallery item: Flat topography in the Cottonwood Basin Lake sediments at the Airport zone.
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