Limestone, nylon mono netting and lines.Sourcing
Calcium fluoride is a mineral composed of calcium fluoride (CaF2), the principal fluorine-bearing mineral. It occurs as cubic, isometric crystals and cleavable masses. When pure, it is colorless and transparent, or translucent with a glassy luster. Impurities cause color in the stone, and several varieties exhibit fluorescence. Usually found either in pure veins or associated with lead, silver, or zinc ores, it is common in limestone and dolomites. Calcium fluoride is a vital component in several industrial applications, including steel production. It is also used to make hydrogen fluoride (AHF) which, in turn, is used in the production of refrigerants and to make aluminium tri-fluoride (AlF3), critical in aluminium smelting; uranium fluoride (UF6), used in nuclear power stations; and lithium hexafluorophosphate (LiPF6), used to make the electrolyte for lithium batteries. Other applications further downstream are: Fluorite comes in a wide range of colors and has subsequently been dubbed "the most colorful mineral in the world". The most common colors are purple, blue, green, yellow, or colorless. Less common are pink, red, white, brown, black, and nearly every shade in between. Color zoning or banding is commonly present. The color of the fluorite is determined by factors including impurities, exposure to radiation, and the size of the color centers.
Manganese is a chemical element, designated by the chemical symbol Mn. It is found as a free element in nature (often in combination with iron) and could be found in many minerals. Manganese is the fourth most used metal in terms of tonnage, being ranked behind iron, aluminium and copper.
Quartz is the most abundant and widely distributed mineral found at Earth's surface. It is present and plentiful in all parts of the world . Eshal industries supplyi ng and exporting a wide range of quartz.
We are engaged in mining FELDSPAR from our own mines which is generally a clean white mineral that sources sodium, alumina and silica along with some potassium and calcium.We are manufacturing it in different sizes using our updated machineries and production lines. Our company is offering it at affordable prices.
Talc, Hydrous magnesium silicate Mg3Si4O10(OH)2 is a hydrous magnesium silicate mineral with a chemical composition of Mg3Si4O10(OH)2. Although the composition of talc usually stays close to this generalised formula, some substitution occurs. Talc, a mineral made up mainly of the elements magnesium, silicon, and oxygen. As a powder, it absorbs moisture well and helps cut down on friction, making it useful for keeping skin dry and helping to prevent rashes. Ground talc makes talcum powder. The massive variety (soapstone) is used for sinks, table tops, etc. Soapstone found a use in Babylonian days when signature cylinder seals were often carved from it. The Egyptians also used it as a base for some of their blue faience figurines, which were then fired to fuse the glaze. California Indians also used it as sculpture material. Eshal
Cryptocrystalline Magnesite MgCO3 with extremely low silica and iron content, white colour, and very low level of heavy metals. RMA is a raw magnesite milled product with 90% MgO content on ignited basis, which is used in the production of ceramics (tiles etc.). Magnesium Carbonate: isolation, rubber, ink, glass, ceramics, paint, pharmacy and cosmetics industry. Magnesium Chloride: Magnesium metal production, textile, paper, ceramics and cement. Magnesium sulphate: Pharmaceutics, artificial fertilizer industry.
We are suppliers and exporters of the best quality GYPSUM ROCKS. Our highly consistent GYPSUM ROCKS are chemically tested to assure quality and efficiency as well as it is available in various sizes in bulk. We also have a wide range of updated machineries and equipment to meet our customers different requirements. GRINDED GYPSUM is also supplied and exported by our company and available in 300 mesh size.
Barite is a mineral composed of barium sulphate (BaSO4). It receives its name from the Greek word "baryte" which means "heavy." This name is in response to barite's high specific gravity of 4.5, which is exceptional for a non-metallic mineral. Baryte is generally white or colorless, and is the main source of barium. The baryte group consists of baryte, Celestine, anglesite, and anhydrite. The high specific gravity of barite makes it suitable for a wide range of industrial, medical, and manufacturing uses. Barite also serves as the principal ore of barium.
Chromite is a mineral that is an iron chromium oxide. It has a chemical formula of FeCr2O4. It is an oxide mineral belonging to the spinel group. The element magnesium can substitute for iron in variable amounts as it forms a solid solution with magnesiochromite (MgCr2O4). Chromite today is mined particularly to make stainless steel through the production of ferrochrome (FeCr), which is an iron-chromium alloy. Chromite grains are commonly found in large mafic igneous intrusions such as the Bushveld in South Africa and Travancore in India. Chromite is iron-black in color with a metallic luster, a dark brown streak and hardness on the Mohs scale of 5.5.
Bauxite ore is the world's main source of aluminum.Bauxite is a rock formed from a reddish clay material called laterite soil and is most commonly found in tropical or subtropical regions. Bauxite is primarily comprised of aluminum oxide compounds (alumina), silica, iron oxides and titanium dioxide. Whether for the refractory industry or metallurgy we offer raw bauxite in various qualities and preparations.Aluminium ore bauxite can be found in a variety of applications. As calcined bauxite, this raw material is a central raw material in the refractory industry thanks to its highly refractory properties. This versatile mineral is also in demand in steel production as slag conditioner, in the production of refractory aluminium oxide cement, in road construction, in mineral wool production and as welding powder.
We are highly engaged in supplying and exporting of highly demanded IRON ORE. We can facilitate large order quantities of IRON ORE lumps and powder. Our IRON ORE products are available in different sizes and weights. The sizes we offer are 0-50 mm and 325 Mesh. are
Kaolinite is a clay mineral, part of the group of industrial minerals with the chemical composition Al2Si2O5(OH)4. It is a layered silicate mineral, with one tetrahedral sheet of silica linked through oxygen atoms to one octahedral sheet of alumina octahedra. White, sometimes red, blue or brown tints from impurities
We are suppliers and exporters of Industrial salt. Salt sets the dye in fabric and is used to produce glass, polyester, plastics and leather as well as in the chemical industry. Salt assists in cleaning gas and oil wells and is an essential component in the manufacture of paper, tires, brass, bleach and case-hardened steel. Salt is part of the caustic soda and chloralkali processes. Industrial salts are often purchased in bulk and in various levels of purity depending on the application.
Crushed Stone Gabbro, Granite, Blue Metal aggregates & Boulders
Bentonite, soda feldspar, gypsum, gypsum crystal, kaolin, talc, limestone, nepheline syenite.
Gypsum is an evaporite mineral most commonly found in layered sedimentary deposits in association with halite, anhydrite, sulfur, calcite, and dolomite. Gypsum (CaSO4.2H2O) is very similar to Anhydrite (CaSO4). The chemical difference is that gypsum contains two waters and anhydrite is without water. Gypsum is the most common sulfate mineral Uses of Gypsum Gypsum uses include: manufacture of wallboard, cement, plaster of Paris, soil conditioning, a hardening retarder in Portland cement. Varieties of gypsum known as satin spar and alabaster are used for a variety of ornamental purposes; however, their low hardness limits their durability.
Feldspar, any of a group of aluminosilicate minerals that contain calcium, sodium, or potassium. Feldspard make up more than half of Earth crust, and professional literature about them constitutes a large percentage of the literature of mineralogy. Of the more than 3,000 known mineral species, less than 0.1 percent make up the bulk of Earth crust and mantle. These and an additional score of minerals serve as the basis for naming most of the rocks exposed on Earth surface. Description and Identifying Characteristics Feldsparis derived from the German word feld,which means field, and spar, which means crystal. This name reflects the minerals abundance, as most crystalline material found in the field is feldspar. Potassium feldspard are the feldspar minerals in which the silicate tetrahedral and aluminum tetrahedra are bound with potassium ions, rather than sodium or calcium ions as in the plagioclase feldspar subgroup. The potassium feldspar group is composed of three mineral polymorphs, each having the same chemical composition, but slightly different crystal structures. Technically these are distinct minerals, but their physical properties are so similar that they are usually only identified as potassium feldspar in the field. Using other minerals in the rock to determine the host rocks identity is often the most useful guide to their probable identity. felsic plutonic igneous rocks and metamorphic rocks Microcline
Feldspar, any of a group of aluminosilicate minerals that contain calcium, sodium, or potassium. Feldspard make up more than half of Earth's crust, and professional literature about them constitutes a large percentage of the literature of mineralogy. Of the more than 3,000 known mineral species, less than 0.1 percent make up the bulk of Earth's crust and mantle. These and an additional score of minerals serve as the basis for naming most of the rocks exposed on Earth's surface. Description and Identifying Characteristics Feldspar is derived from the German word feld,which means field, and spar, which means crystal. This name reflects the minerals abundance, as most crystalline material found in the field is feldspar. Potassium feldspard are the feldspar minerals in which the silicate tetrahedral and aluminum tetrahedra are bound with potassium ions, rather than sodium or calcium ions as in the plagioclase feldspar subgroup. The potassium feldspar group is composed of three mineral polymorphs, each having the same chemical composition, but slightly different crystal structures. Technically these are distinct minerals, but their physical properties are so similar that they are usually only identified as potassium feldspar in the field. Using other minerals in the rock to determine the host rocks identity is often the most useful guide to their probable identity. felsic plutonic igneous rocks and metamorphic rocks Microcline
Nepheline is an important feldspathoid mineral. It is white, grey or yellow in colour with a vitreous lustre and a poor cleavage. The name Nepheline comes from the Greek word nephele, which means cloud, because it becomes strongly clouded when put in strong acid. Nepheline only forms in silica-poor rocks. It is almost never associated with quartz. It may be found in some contact metamorphosed rocks otherwise it occurs in alkaline complexes in igneous rocks. Nepheline is mostly found in the rock Nepheline Syenite in nature.
