mineral halit


Halite (pengucapan: / ˈ h æ l aɪ t / atau / ˈ h eɪ l aɪ t /), umumnya dikenal sebagai garam batu, adalah suatu jenis garam, bentuk mineral (alami) dari natrium klorida (Na Cl). Halit membentuk kristal isomerik.


Halite (/ ˈ h æ l aɪ t, ˈ h eɪ l aɪ t /), commonly known as rock salt, is a type of salt, the mineral (natural) form of sodium chloride (Na Cl). Halite forms isometric crystals.

Halite Mineral Data

NaCl Environment: Marine or continental evaporite deposits. IMA Status: Valid Species (Pre-IMA) Prehistoric Locality: World wide in sedimentary basins. Link to MinDat Location Data. Name Origin: From the Greek halos, meaning "salt" and lithos meaning "rock." Name Pronunciation: Halite Synonym: ICSD 18189 Murate of Sota PDF 5-628 Rock Salt

Halite Mineral | Uses and Properties

Halite is mainly a sedimentary mineral that usually forms in arid climates where ocean water evaporates. However, many inland lakes such as the Great Salt Lake of North America and the Dead Sea between Jordan and Israel are also locations where halite is …

Halite Mineral | Properties, Formation, Uses and Deposits

Halite, also known as rock salt or sodium chloride (NaCl), is a naturally occurring mineral that holds significant importance in various aspects of human life. This crystalline mineral is composed of equal parts sodium and chlorine ions and is renowned for its distinctive cubic crystal structure.

Halite salt: The mineral Halite information and pictures

The Mineral halite Halite, the natural form of salt, is a very common and well-known mineral. It is found in solid masses, and as a dissolved solution in the oceans and in salt lake s. The inland lakes that are rich in salt exist in arid regions, and may also be below sea level without an outlet.

Halite | Salt, Rock Salt, Evaporite | Britannica

Halite, naturally occurring sodium chloride (NaCl), common or rock salt. Halite occurs on all continents in beds that range from a few metres to more than 300 m (1,000 feet) in thickness. Termed evaporite deposits because they formed by the evaporation of saline water in partially enclosed basins,

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