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Metro Mining Company

Metro Mining Company
Kushaiguda, Secunderabad, Telangana

gstGST : 36AASFM2200J1ZA Verified Add Review
Call 08068051321 Ext. 713

Our Products

  1. Ores And Minerals 3 Products available

  2. Stone Block

    2 Products available

  3. Clay

    2 Products available

  4. Quartz Stone

    2 Products available

  5. Wedding Cards

    1 Products available

  6. Cobbles And Kerbs

    1 Products available

  7. Soil Conditioners

    1 Products available

  8. Feldspar Minerals

    1 Products available

  9. Industrial Chemicals

    1 Products available

  10. Pesticides & Insecticides

    1 Products available
  11. Others Products 1 Products available

Ores And Minerals

Our Complete range of products are Bentonite, Laterite Ore and Feldspar.

bentonite

Bentonite
  • Min. Order (MOQ) 28 Metric Ton
Bentonite is an absorbent aluminium phyllosilicate clay consisting mostly of montmorillonite. It was named by Wilbur C. Knight in 1898 after the Cretaceous Benton Shale near Rock River, Wyoming.[1][2] The different types of bentonite are each named after the respective dominant element, such as potassium (K), sodium (Na), calcium (Ca), and aluminium (Al). Experts debate a number of nomenclatorial problems with the classification of bentonite clays. Bentonite usually forms from weathering of volcanic ash, most often in the presence of water. However, the term bentonite, as well as a similar clay called tonstein, has been used to describe clay beds of uncertain origin. For industrial purposes, two main classes of bentonite exist: sodium and calcium bentonite. In stratigraphy and tephrochronology, completely devitrified (weathered volcanic glass) ash-fall beds are commonly referred to as K-bentonites when the dominant clay species is illite. Other common clay species that are sometimes dominant are montmorillonite and kaolinite. Kaolinite-dominated clays are commonly referred to as tonsteins and are typically associated with coal.

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Laterite Ore

Laterite Ore
Nearly two third of the area of Goa is covered by a mantle of laterite ranging in thickness from a couple of meters to over 25 mts.Maximum thickness of laterite is observed along the coast in the west and minimum along the Ghat section in the East.The laterites in Goa are generally formed from Quartz-chlorite-Amphibole Schist, Pink ferruginous phyllite, Schitose metabasalt & Metagreywacke.The laterite in Goa are used in construction activity as laterite boulders and laterite stones (Locally called as chira).The laterite stones are used in construction activity because of their peculiar nature of being soft while cutting and becomes hard after use.

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feldspar

Feldspar
  • Min. Order (MOQ) 28 Metric Ton
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. The term feldspar encompasses a whole range of materials. Most of the products we use on a daily basis are made with feldspar: glass for drinking, glass for protection, fiberglass for insulation, the floor tiles and shower basins in our bathrooms, and the tableware from which we eat. Feldspar is part of our daily life. Feldspar minerals are essential components in igneous, metamorphic and sedimentary rocks, to such an extent that the classification of a number of rocks is based upon feldspar content. The mineralogical composition of most feldspars can be expressed in terms of the ternary system Orthoclase (KAlSi3O8), Albite (NaAlSi3O8) and Anorthite (CaAl2Si2O8). Chemically, the feldspars are silicates of aluminium, containing sodium, potassium, iron, calcium, or barium or combinations of these elements.

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