Blende may refer to: Sphalerite (Zinc blende, ZnS).
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the specific gravity of the sphalerite mineral is aproximatelyy 4.0
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The largest deposits of sphalerite is found in the US.
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Sphalerite is primarily used as an ore of zinc, which is an important metal for industrial applications. It is also used as a gemstone when it forms as transparent crystals with a high luster. Additionally, sphalerite is used in the manufacturing of certain types of batteries.
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Sphalerite is the main ore of zinc, a mineral dietary supplement, and rustproofing material.
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In some games, sphalerite can be used to make weapons, but they are not very powerful.
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Sphalerite is not a sedimentary rock. It is a mineral that typically occurs in hydrothermal veins in igneous and metamorphic rocks. Sphalerite is a zinc sulfide mineral commonly found in ore deposits.
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Sphalerite is typically brown, yellow, green, or black in color. It can also exhibit a range of shades within these colors due to impurities in its composition.
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The density of sphalerite is approximately 4.1-4.3 g/cm^3.
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Diamond has perfect cleavage in four directions, fluorite has perfect cleavage in four directions, sodalite has perfect cleavage in three directions, and sphalerite has perfect cleavage in six directions.
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Oxygen in the air reacts with heated sphalerite to form zinc oxide and sulfur dioxide.
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No, sphalerite is not a good conductor of electricity. It is classified as a semiconductor, meaning it has some conductivity but not as high as good conductors like metals.
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Sphalerite forms when zinc-bearing fluids interact with sulfur-bearing minerals in hydrothermal veins or sedimentary environments. These fluids precipitate the zinc and sulfur as sphalerite crystals, which can occur in a variety of colors depending on impurities present. Temperature and pressure conditions during formation influence the crystal structure and appearance of sphalerite.
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Seth C Schaefer has written:
'Electrochemical determination of the Gibbs energy of formation of sphalerite (ZnS)' -- subject(s): Sphalerite
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Zincblende is an alternative name for sphalerite, a mineral containing cubic crystals.
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Zinc is primarily obtained from the mineral sphalerite, which is a type of zinc sulfide. It can also be extracted from other minerals such as smithsonite, hemimorphite, and willemite.
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According to my Dana Minerals and how to Identify Them, "... in the rare perfectly pure specimen Sphalerite is clear and nearly colorless and has an adamantine luster."
Otherwise, its colour seems to be highly variable, " ~ ranging from black, though brown and yellow, to red. "
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Sphalerite is typically opaque, meaning that it does not allow light to pass through. This mineral usually appears as a dark-colored material with a metallic luster, rather than being transparent.
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Sphelter is a term commonly used to refer to zinc. It is a natural element that is primarily obtained from the ore sphalerite, which is a major source of zinc. The process of refining sphalerite helps in extracting zinc for various industrial applications.
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It is also found as an element (in trace amounts) in plants and animals.
Humans require Zinc as part of a balanced diet, this is obtained from foods such as: oysters, beans, spinach, nuts, oats, red meat and milk.
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Quartz, tin, copper, silver, aluminum, sulfur, sphalerite . . . probably more.
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It is found in veins in rocks (where it was deposited hydro-thermally) as the mineral sphalerite.
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The primary ore of zinc is sphalerite (zinc sulfide). Other zinc ores include smithsonite (zinc carbonate), hemimorphite (zinc silicate), and willemite (zinc silicate).
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J. M. Stuve has written:
'Low-temperature heat capacities of sphalerite and wurtzite' -- subject(s): Sphalerite, Wurtzite
'Thermodynamic properties of NiBr and NiSo from 10 to 1,200 K' -- subject(s): Nickel, Thermal properties
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Zinc is the metal that can be extracted from sphalerite ore. Sphalerite is the most important ore of zinc and typically contains around 67% zinc when pure. The extraction process involves crushing and heating the ore to remove impurities and recover the zinc metal.
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nickel (pentlandite), copper (chalcopyrite), zinc (sphalerite), lead (galena) aluminum (bauxite)
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Sphalerite is found worldwide, with significant deposits in countries such as the United States, Mexico, Peru, Canada, Australia, and Spain. It is often associated with regions rich in lead and zinc minerals.
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bauxite, gelena, casserterite, chal copyrite, sphalerite, wolframite..
(alyssamc6)
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Willemite is usually formed as an alteration of previously existing Sphalerite ore bodies and is often associated with Limestone.
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F. John Norman has written:
'Iron content of sphalerite from the Manitouwadge area, Ontario'
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Sphalerite is a mineral that is sometimes used as a gemstone in jewelry. It is valued for its range of colors and high dispersion, which gives it a sparkle when cut and polished. However, its relatively low hardness and cleavage make it less durable compared to popular gemstones like diamond or sapphire.
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Galena not a rock its a Economic mineral of lead. Formula of Galena is PbS. Galena and Sphalerite(ZnS) Found togather at Hydrothemal deposits.
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Scientists collect Germanium from certain types of mineral specimens. These include Sphalerite and other ores from silver, copper, and lead.
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Zinc can be found in a number of minerals. The primary one mined is (ZnFe)S, or sphalerite. Use the links to do more reading.
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Clark D. Michlowski has written:
'A preliminary study of the sulfuric acid leaching of a Timmins area sphalerite concentrate'
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(Zn,Fe)S ; (Zn,Fe,Mg,Mn,Cd,In,Ga)S
Source: http://www.minerals.net/mineral/sulfides/sphaleri/sphaleri.htm
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Rubellite, Almandine, Carnelian, Ruby Jack(Red variety of Sphalerite), Red Beryl, PYROPE, CROCOITE, RED AVENTURINE, RED JASPER, RHODONITE
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The chemical name for zinc blend is zinc sulfide. It is a naturally occurring mineral form of zinc and sulfur.
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Zinc is a mineral in its natural state as sphalerite (ZnS), which is a compound of Zinc and Sulphur. It is normally found along with other igneous type minerals such as copper, lead and iron.
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Sphalerite is a mineral that can exhibit a greasy luster when uncut. It is a zinc sulfide mineral that can vary in color and is commonly found in ore deposits.
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Germanium can be found in small quantities in coal deposits worldwide. It is also found in some zinc ores, such as sphalerite. Germany, Russia, and the United States are some of the main producers of germanium.
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Sphalerite is typically mined through open-pit or underground mining methods. In open-pit mining, the overlying rock and soil are removed to access the ore, while in underground mining, tunnels or shafts are dug to reach the deposits. The sphalerite-containing ore is then extracted and processed to isolate the valuable mineral.
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Greasy luster describes a shiny appearance similar to the sheen on a greasy surface. It is commonly seen in minerals like graphite and sphalerite due to their smooth, oily texture that reflects light in a certain way.
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Zinc is primarily found combined with other elements in minerals such as sphalerite, smithsonite, and hemimorphite. It is rarely found in its pure form in nature.
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This type of luster is known as subadamantine. It is characterized by a shiny, reflective appearance similar to broken glass, often seen in minerals like diamond, zircon, and sphalerite.
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Barite
Calcite
Carnotite
Dolomite
Feldspar
Galena
Geodes
Gold
Gypsum
Hematite
Limonite
Marcasite
Metatorbernite
Mica
Pyrite
Quartz
Silver
Sphalerite
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Some examples of sulfide minerals include galena (lead sulfide), pyrite (iron sulfide), chalcopyrite (copper iron sulfide), and sphalerite (zinc sulfide).
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