We are an eminent and a renowned exporter and supplier of Feldspar, Silica Sand, China Clay, Lime Stone and other Industrial Minerals. Our minerals are available in attractive shades and textures in hushed tones of multicolor, white, grey, mustard, brown and many more. Our corporate entity is well-acknowledged for its products due to the high durability and reliability factor attached to them.

Limestone often contains variable amounts of silica in the form of chert or flint, as well as varying amounts of clay, silt and sand as disseminations, nodules, or layers within the rock. The primary source of the calcite in limestone is most commonly marine organisms. These organisms secrete shells that settle out of the water column and are deposited on ocean floors as pelagic ooze or alternatively is conglomerated in a coral reef (see lysocline for information on calcite dissolution). Secondary calcite may also be deposited by supersaturated meteoric waters (groundwater that precipitates the material in caves). This produces speleothems such as stalagmites and stalactites. Another form taken by calcite is that of oolites (oolitic limestone) which can be recognized by its granular appearance. Limestone makes up about 10% of the total volume of all sedimentary rocks.

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