|
Celadonite |
Chemical Formula |
K(Mg,Fe2+)(Fe3+,Al)[Si4O10](OH)2 |
Species |
Silicates |
Crystal System |
Monoclinic |
Mohs Scale |
2 |
Specific Gravity |
3 |
Color |
Blue-green, olive green, apple green |
Luster |
Dull |
Refractive Index |
n = 1.606 - 1.625 n = 1.630 - 1.662 n = 1.579 - 1.661 |
Diaphaneity |
Translucent |
Cleavage |
Perfectperfect on |
Crystal Habit:Minute micaceous scales or earthy aggregates |
Geological Setting:Replaces ferromagnesian minerals in altered intermediate to mafic igneous rocks, zeolite grade metamorphic rocks, amygdaloidal fillings in basalts and andesites. |
Celadonite is a mica group mineral, a phyllosilicate of potassium, iron in both oxidation states, aluminium and hydroxide with formula: K(Mg,Fe
2+)(Fe
3+,Al)[Si
4O
10](OH)
2.
It crystallizes in the monoclinic system and usually forms massive aggregates of prismatic crystallites or in dull clay masses. It is soft with a Mohs hardness of 2 and a specific gravity of 3. Typically occurs as dull gray-green to bluish green masses. It forms vesicle fillings and linings in altered basaltic lavas.
It was first described in 1847 on Mt. Baldo, near Verona, Italy. The name is from the French celadon, for sea-green.