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Haliteâs most distinctive characteristic is its salty taste. For practical and sanitary reasons, you probably should not test the taste of a mineral sample by directly licking the sample. Instead, moisten your finger, rub the sample and then taste the residue left on your finger.
In the language of close-packing, the larger chloride ions are arranged in a cubic array whereas the smaller sodium ions fill all the cubic gaps (octahedral voids) between them. This same basic structure is found in many other compounds and is commonly known as the halite or rock-salt crystal structure.