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Mineral

Halite

Also Known As Rock Salt
Halide Minerals

Halite, commonly known as rock salt, is the mineral form of sodium chloride, NaCl, and forms isometric crystals. It is typically colorless or white, but depending on inclusions and impurities it can also be light or dark blue, purple, pink, red, orange, yellow or gray. Most halite occurs in sedimentary rock formed by the evaporation of seawater or salty lake water, and such evaporite beds can be hundreds of metres thick. It also forms salt domes, which are common along the Gulf coasts of Texas and Louisiana and are often associated with petroleum deposits. Salt is used extensively in cooking as a flavor enhancer and in food preservation, and rock salt is spread on roads and sidewalks to melt ice. The name comes from the Ancient Greek word for salt.

Facts
Formation Class
Evaporite (commonly occurs with other evaporite deposit minerals such as sulfates, halides and borates) 1
Chemical Formula
NaCl 1
Hardness (Mohs)
2.5 1
Commonly cited range is 2.0 to 2.5 on the Mohs scale; 2.5 is used here.
Colour
Colourless or White 3
Colour
Grey or Black 3
Colour
Red or Pink 3
Colour
Orange or Yellow 3
Colour
Green 3
Colour
Blue or Purple 3
Lustre
Vitreous 3
Rarity
Common 3
Classification
Strunz Class
Halides 1
Crystal System
Cubic (Isometric) 1
Use
Food / De-icing 2
Wikipedia 'Halite' states this use (or use-bearing statement); earth5 pass.
Connections

Associated With

Evaporite, Materials

Halite named as one of the most common marine evaporite minerals.

Source Evaporite (Wikipedia)

Caused By

Source EBSCO Research Starters: Sedimentary mineral deposits
Additional Source Halite (Wikipedia)Occurrence
Additional Source EBSCO Research Starters: Sedimentary rock classificationEvaporites

Classified As

Crystallizes In System

In Discipline

Source Halite (Wikipedia)
Sources
1. Halite (Wikipedia)
Wikimedia Foundation
  • Article text
    Halite ( HAL-yte, HAY-lyte), commonly known as rock salt, is a type of salt, the mineral (natural) form of sodium chloride (NaCl).
  • Infobox: mohs
    2.0-2.5
  • Lead section
    Halite ( HAL-yte, HAY-lyte), commonly known as rock salt, is a type of salt, the mineral (natural) form of sodium chloride (NaCl).
  • Lead section
    The mineral is typically colorless or white, but may also be light blue, dark blue, purple, pink, red, orange, yellow or gray depending on inclusion of other materials, impurities, and structural or isotopic abnormalities in the crystals.
  • Caused By: Sedimentation, Occurrence
    Halite dominantly occurs within sedimentary rocks where it has formed from the evaporation of seawater or salty lake water.
View the Source
2. Wikidata: Halite
Wikidata Q5314
3. minerals.net: Halite
minerals.net
  • Color field
    Colorless, white, red, yellow, orange, pink, blue, violet, green, and gray. May also be multicolored with a solid and clear color such as blue and white.
  • Luster field
    Vitreous
  • About
    Halite, the natural form of salt, is a very common and well-known mineral.
View the Source
Evaporite (Wikipedia)
Wikimedia FoundationAssociated With: Evaporite, Marine evaporite minerals section
Quote, Associated With: Evaporite, Marine evaporite minerals section
The most common marine evaporites are calcite, gypsum and anhydrite, halite, sylvite, carnallite, langbeinite, polyhalite, and kainite.
View the Source
EBSCO Research Starters: Sedimentary rock classification
EBSCO Research StartersCaused By: Sedimentation, Evaporites
Quote, Caused By: Sedimentation, Evaporites
The main groups of sedimentary rocks include evaporites, which form from the evaporation of seawater or freshwater, resulting in minerals like gypsum and halite.
View the Source
EBSCO Research Starters: Sedimentary mineral deposits
EBSCO Research StartersCaused By: Sedimentation, Evaporite deposits
Quote, Caused By: Sedimentation, Evaporite deposits
Large deposits of anhydrite (calcium sulfate), gypsum (hydrated calcium sulfate), and halite (sodium chloride, also known as table salt) have formed in small seas in areas with arid climates.
View the Source
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