It is a mineral that formed as a consequence of the chemical reaction of ash and lava, which originated from the eruption of volcanoes millions of years ago, with lakes or sea waters.
It is a precious and limited mineral owing to its hydrous magnesium silicate high action proper, its porosity, crystal morphology, and physicochemical properties.
In classifications of clay which are classified according to their aluminum hydrosilicate crystal construction, those which are equidimensional elongated in one direction are classified as kaonite group.
It comprised of clay minerals with tiny crystals, which originated from chemical decomposition of volcanic ash, tuff, lava that abound with aluminum and magnesium.
Psychochemical Features
Form
Shape
Color
Granular and powdery
Angled
Green / White
Psychochemical Analysis
SiO₂
70.77%
Al₂O₃
13.62%
CaO
5.08%
K₂O
3.83%
Fe₂O₃
3.78%
MgO
3.12%
Na₂O
0.49%
TiO₂
0.92%
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