Abstract
Woodhouseite is a new sulfate-phosphate member of the beudantite group. It is found in small quantities in quartz veins that adjoin and penetrate the commercial andalusite deposits1 located on the west slope of White Mountain in the Northern Inyo Range, Mono County, California. The andalusite deposits occur in pre-Cambrian meta-quartzite,2 and have been formed by intrusion of late Jurassic granitic rocks that are offshoots of the Inyo Batholith.
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