Quartzitelumps-H White

Quartzitelumps-H White


Quartz is the most abundant and most common mineral on the Earth. It is found in almost every geological environment and also it is at least a component of almost every rock type. It has a hexagonal crystal structure and is made of trigonal crystallized silica. It is most varied in terms of varieties, colors and forms.

The most important distinction between the types of quartz is that one is of macrocrystalline, which is individual crystal visible to the unaided eye, and the other is microcrystalline or cryptodrystalline varieties, aggregates of crysstals visible only under high magnification. Chalcedony is the generic term for cryptocrystalline quartz. The transparent variety tends to be macrocrystalline and the cryptocrystalline varieties are either translucent or mostly opaque.

We produce Quartz in forms of :
1. Granular Particles
2. Powder (150-25 microns)
3 lumps form 1 inches to 15 inches

Packing :
Standard Packing available in 50 kg. HDPE bags & 1 or 1.25 mt Jumbo bags with liner inside, or as per customer requirements.



Physical Properties of Quartz

Color Clear (in pure form)
Crystal habit 6-sided prism ending in 6-sided pyramid (typical)
Crystal system Trigonal
Cleavage None
Fracture Conchoidal
Mohs scale hardness 7 – lower in impure varieties
Luster Vitreous
Refractive index 1.544-1.553 – Dr +0.009 (B-G interval)
Streak White
Specific gravity 2.65 constant; variable in impure varieties
Melting point 1650 (±75) 0C
Boiling point 22300C
Solubility H2O insoluble


Chemical Properties

SiO2 99.80% (± 00.20%) 98.30% (± 00.20%) 96.50% (± 00.30%)
Al2O2 00.03% (± 00.05%) 00.50% (± 00.10%) 00.80% (± 00.10%)
Fe2O2 00.05% (max) 00.085% (max) 00.20% (max)
K2O 25 ppm (max) 00.001% (max) 00.20% (± 00.05%)
Na2O 40 ppm (max) 00.001% (max) 00.09% (max)
TiO2 Nil Traces Traces
LoI @ 10000 C 0.05% 0.10% 0.10%


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