An amorphous Fe3+ hydrous arsenate sulphate of questionable validity. Chemical composition appears to be variable.
"Microprobe analyses of 7 pitticites from various localities indicate that it is a gel-like mineral of widely varying composition with no apparent stoichiometry. Previously reported minor amounts of Si, Ca, P and Al are constituents of pitticites but are non-essential. Pitticite is retained as a generic name for amorphous, gel-like, ferric iron arsenate minerals of varying chemical composition" (Dunn, 1982).
A secondary mineral formed at near-surface conditions from the oxidation of arsenopyrite, realgar, or orpiment; also forms as a recent deposit from mine and spring waters.