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BLUE & PURPLE HALITE CRYSTAL<<<<"LARGE & THICK SPECTACULAR HALITE CRYSTAL"
Weight approx: 56.4 grams or 282.0 carats
Dimensions Length & Width: 73.3 mm X 56.4 mm X 20.0 mm (thick)
Dimensions Length & Width: 2.9" X 2.2" X 0.8" (thick)
Origin: 10th Ore Zone, Intrepid Potash East Mine, Carlsbad, Eddy County, New Mexico, USA.
Color: royal blue & luxuriant purple"A beautiful & attractive large & thick specimen"
Clarity: transparent to translucent (predominantly translucent)
NOTE: This Halite Crystal specimen is rare, due to its stupendous royal blue color.
Makes a perfect & prized addition to your collection.
Utilize for metaphysical purposes,healing.
Truly a magnificent specimen.
Photos don't do justice.
$495.00
Includes draw string pouch for safe storage & FAST FREE SHIPPINGShipping Via: USPS with tracking number & insurance.
WE'RE OVERSTOCKED. DRASTICALLY REDUCING PRICES.$149.limited time Due to the color contrast between different computer monitors, the photos may notreflectthe exact color of the item. Ladies & Gentlemen, if you're happy with your order, please leave us positive response. If you're not 100% satisfied,contact us & we will do everything possible to make your experience perfect. We sincerely appreciate your INFORMATION:
Halite belongs to the group of "Halides" which are essentially compounds in which metallic elements combine with halogens (which are bromine, chlorine, fluorine & iodine). Halite is found in sedimentaryrock that is formed,by the evaporation of water. So, it's considered an evaporite mineral due to the fact that it'sformed by precipitation.In addition, also found in bedded sedimentary deposits.
Cleavage: perfect cubic
Crystal System: cubic
Fracture: uneven to conchoidal
Habit: cubic crystals
Hardness: 2.5
Specific Gravity: 2.1-2.2
Possesses a "salty" taste.
Soluble in cold water.
Feels "greasy" to the touch.
Luster: vitreous.
Clarity: transparent to translucent.
It turns a flame yellow in color.
Minute impurities will produce fluorescence colors of green, orange or red.
Halite lowers the freezing point of
