Marble Stone is a rock resulting from metamorphism of sedimentary carbonate rocks, most commonly limestone or dolomite rock. Metamorphism causes variable recrystallization of the original carbonate mineral grains.

The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals. Primary sedimentary textures and structures of the original carbonate rock (protolith) have typically been modified or destroyed.

*Colour may vary from that shown


KCMS 1002
KCMS 1002
KCMS 1102
KCMS 1102
KCMS 1104
KCMS 1104
KCMS 1106
KCMS 1106

Quartz is the second-most-abundant mineral in the Earth's continental crust, after feldspar.

There are many different varieties of quartz, several of which are semi-precious gemstones. Especially in Europe and the Middle East, varieties of quartz have been since antiquity the most commonly used minerals in the making of jewelry and hardstone carvings.

*Colour may vary from that shown
KCQS 103
KCQS 103
KCQS 104
KCQS 104
KCQS 107
KCQS 107
KCQS 111
KCQS 111

Handmade sink
Handmade sink
NS 01
NS 01
NS 02
NS 02
NS 03
NS 03
KC 2017
KC 2017
KC 2100
KC 2100
KC 2105
KC 2105
KC 2132
KC 2132
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