Illite is a non-expanding,
clay-sized, micaceous mineral. Illite is a
phyllosilicate or layered silicate. Structurally illite is quite similar to
muscovite or
sericite with slightly more
silicon,
magnesium,
iron, and water and slightly less tetrahedral
aluminium and interlayer
potassium. The chemical formula is given as (K,H3O)(Al,Mg,Fe)2(Si,Al)4O10[(OH)2,(H2O)], but there is considerable ion substitution. It occurs as aggregates of small
monoclinic grey to white crystals. Due to the small size, positive identification usually requires
x-ray diffraction analysis. Illite occurs as an alteration product of muscovite and
feldspar in
weathering and
hydrothermal environments. It is common is sediments, soils, and argillaceous
sedimentary rocks as well as in some low grade
metamorphic rocks.
Glauconite in sediments can be differentiated by x-ray analysis.
See more at Wikipedia.org...

General Information:

Chemical Formula:
(K,H3O)(Al,Mg,Fe)2(Si,Al)4O10[(OH)2,(H2O)]

IMA Status:
Not IMA Approved
Physical Properties:

Cleavage:
[???] Perfect

Color:
white.

Density:
2.6 - 2.9, Average = 2.75

Diaphaniety:
Translucent

Hardness:
1-2 - Between Talc and Gypsum

Luster:
Earthy (Dull)

Streak:
white
More details...