Granite is formed from magma which has found its way through the earth’s crust and solidified. It is generally accepted that most granites were formed during the Carboniferous and Permian geological ages some 250-360 million years ago.

In many cases the granite was not exposed until millions of years later when the overlaying softer soils and rocks had been eroded away.

The colour and appearance of granite can vary enormously, as shown by our range. If the molten magma was close to the surface cooling would have been rapid thus resulting in a fine texture, e.g. SPI, however if the deposits were deeper set, the rate of cooling would be considerably slower, therefore enabling larger crystals to form, e.g. Baltic Brown.

By using the word “granite” we refer to compact polishable igneous rocks that are suitable for building and decorative purposes, consisting of minerals such as silica, feldspar, engine, mica, basalt, diorites etc.

Granite is quarried extensively throughout the world and its resilience, strength and high aesthetic value as well as its ability to be polished into various textures makes granite unique as a quality building material.