Bentonite is absorbent aluminium. It is essentially impure clay consisting mostly of montmorillonite. There are different types of Bentonite, each named after the respective dominant element, such as potassium (K), sodium (Na), calcium (Ca), and aluminium (Al). Bentonite usually forms from weathering of volcanic ash, most often in the presence
of water.

Quartz, second most common of all minerals, is composed of silicon dioxide, or silica, SiO2 and distributed all over the world as a constituent of rocks and in the form of pure deposits.

Talc is the world's softest mineral. Although all talc ores are soft, platy, water repellent and chemically inert, no two talc ores are quite the same. The magazines we read, the polymers in our cars and houses, the paints we use and the tiles we walk on are just some of the products that talc enhances.

Bauxite is an aluminium ore and is the main source of aluminium. This form of rock consists mostly of the minerals gibbsite, boehmite, and diaspore, in a mixture with the two iron oxides
goethite and hematite, the clay mineral kaolinite, and small amounts of anatase.

We cater a composite range of Dolomite mineral in various forms such as, powder form and Calcined form. Our dolomite finds application in various industries like chemicals, steel and iron.

Feldspar is by far the most abundant group of minerals in the earth's crust, forming about 60% of terrestrial rocks. Most deposits offer sodium feldspar as well as potassium feldspar and mixed feldspars. Feldspars are primarily used in industrial applications for their alumina and alkali content.