Halite is a mineral with a crystalline structure.
Halite typically forms cubic or sometimes octahedral crystal shapes.
Halite's transparency is transparent/translucent.
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Halite is table salt. The cubic crystal "galena" is lead sulfide.
Halite has a cubic crystal structure, which makes it naturally form into perfect cubes. When broken repeatedly along its natural cleavage planes, halite will continue to fragment into smaller cubes due to its internal molecular arrangement. This phenomenon is a result of the crystal structure of halite and its tendency to break along specific planes.
Galena and halite have different chemical compositions. Galena is lead sulfide (PbS), while halite is sodium chloride (NaCl). Both minerals have distinct crystalline structures: galena has a cubic crystal structure, while halite has a cubic crystal structure as well.
Halite, or sodium chloride, has a face-centered cubic crystal structure. This means that each sodium ion is surrounded by 6 chloride ions in a cubic arrangement, and each chloride ion is surrounded by 6 sodium ions. The ions are closely packed in a repeating pattern in all three dimensions.
Halite crystals belong to the isometric crystal system. This means that the crystal structure exhibits cubic symmetry, with all edges of the crystal being of equal length and intersecting at 90-degree angles.
Halite is a cleavage because it splits evenly, but fracture would mean it breaks irregularly.
The tendency of halite to break apart in specific directions when struck is called "cleavage." Halite has perfect cubic cleavage, which means it can split along its crystal planes to produce smooth, flat surfaces. This property is a result of the arrangement of its ionic bonds within the crystal structure.
Absolutely. For example, Galena and Halite.
This crystal is face-centered cubic.