Pitticite
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.
History
Activities related to discovery and approval of the group members
Structural context
Pitticite
Crystal System amorphous
a
b
c
alpha
beta
gamma
volume
Based on 1 measurements
Chemical context
Stoichiometric formulas
Pitticite
mindat.org
- March 13, 2023(Fe, AsO4, H2O) (?)Minor, non-essential S, Si, Ca, P and Al may be present.
IMA
- March 13, 2023[Fe,AsO4,SO4,H2O] (?)
mineralogy.rocks
- Aug. 30, 2022(Fe,SO4,AsO4,H2O)
Elements recorded on EPMA
1
Al
1
As
1
Co
1
Cu
1
Fe
1
H
1
K
1
Ni
1
O
1
Zn
Physical properties
ColorColor entities, recognized using a custom trained NER model
- yellowish
- pale yellowish
- reddish-brown
- reddish brown
- brownish red
- brownish black
Color noteOriginal color note from the source
Yellowish, reddish-brown, brownish red to brownish black, grey, nearly white; pale yellowish to reddish brown in transmitted light.
StreakStreak entities, recognized using a custom trained NER model
Streak noteOriginal streak note from the source
Yellow to white
Lustre
Vitreous
Greasy
Dull
Fracture
Irregular/Uneven
Splintery
Conchoidal
Transparency
Transparent
Opaque
Tenacity
very brittle
Hardness
2—3
Measured density
2.2—2.5