Conchoidal - Fractures developed in brittle materials characterized by smoothly curving surfaces, (e.g. quartz).
Habit:
Crystalline - Fine - Occurs as well-formed fine sized crystals.
Habit:
Massive - Granular - Common texture observed in granite and other igneous rock.
Hardness:
6-6.5 - Orthoclase-Pyrite
Luminescence:
Fluorescent, Short UV=orange yellow, Long UV=orange.
Luster:
Vitreous - Greasy
Streak:
gray
Optical Properties of Chondrodite
Gladstone-Dale:
CI meas= -0.021 (Excellent) - where the CI = (1-KPDmeas/KC) CI calc= 0.084 (Poor) - where the CI = (1-KPDcalc/KC)
KPDcalc= 0.1798,KPDmeas= 0.2003,KC= 0.1962 Ncalc = 1.61 - 1.69
Optical Data:
Biaxial (+), a=1.592-1.643, b=1.602-1.655, g=1.619-1.675, bire=0.0270-0.0320, 2V(Calc)=76-78, 2V(Meas)=64-90. Dispersion weak to moderate, r > v.
Pleochroism (x):
yellowish brown, deep chrome yellow, reddish brown, or brownish yellow.
Pleochroism (y):
pale yellowish brown, yellow, pale reddish brown, or yellowish green.
Calculated Properties of Chondrodite
Electron Density:
Bulk Density (Electron Density)=3.09 gm/cc note: Specific Gravity of Chondrodite =3.15 gm/cc.
Fermion Index:
Fermion Index = 0.03 Boson Index = 0.97
Photoelectric:
PEChondrodite = 6.55 barns/electron U=PEChondrodite x rElectron Density= 20.25 barns/cc.
Radioactivity:
GRapi = 0 (Gamma Ray American Petroleum Institute Units) Chondrodite is Not Radioactive
Chondrodite Classification
Dana Class:
52.03.02b.02(52)Nesosilicate Insular SiO4 Groups and O, OH, F, and H2O