This material is believed to be montebrasite. Material in the core forms rough, nearly equi-dimentional masses 12 inches (30 cm) or less in diameter with rough crystal faces. Other masses are much larger. One unusually large pod, 20 feet in maximum exposed dimension appears to be an aggregate of crystals 3 inches to more than 4 feet in diameter. Chemical analyses by London and Burt (1982) supersede former field identifications of earlier publications.