Occurs in irregular cavities that are pseudomorphic molds of an uncertain precursor; in some places enclosed by chromian leadhillite.
Habit:
Typically as isolated crystals & divergent sprays
Quality of samples:
not specified / average specimens
Confirmation
Validity:
Believed Valid
References
References:
Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 329; Dunn, P.J., et al (1989), Pinalite, a new lead tungstate chloride mineral from the Mammoth mine, Pinal Co., AZ, Am.Min.: 74: 934-935.