Cubic -- hexoctahedral
Environment
Sedimentary salt beds, volcanic fumaroles.
Crystal description
Like halite, but the cubes are much more frequently modified by octahedron faces, which may even be dominant. Like halite, massive and cleavable.
Physical properties
Same as halite in color and luster, but not blue or purple.
Hardness
2;
specific gravity
2.0;
fracture
uneven;
cleavage
cubic. Brittle; transparent; water-soluble.
Composition
Potassium chloride (52.4% K, 47.6% Cl). Some Na may be present.
Tests
More bitter taste than halite. When sodium is not abundant the violet potassium flame is readily seen, but it may be masked by the sodium. More soluble than halite, it can be leached away from sea salt piles by rain.
Distinguishing characteristics
Distinguished from halite by the taste and the flame test. The crystals commonly show octahedral faces (rare in halite). In the mined occurrences, sylvite is frequently colored red by hematite inclusions, though there seems no genetic reason for it.
Occurrence
Sylvite forms layers like halite. Since it is more soluble than that mineral, sylvite beds will usually lie above the halite in the sedimentary deposit series; it is one of the closing minerals to come out of an evaporating salt lake. It is much rarer than halite. Good specimens come from Stassfurt, Germany, and from New Mexico.
Remarks
Both sylvite and halite are said to be very diathermanous, which means being transparent to heat waves; heat acts like light waves penetrating a transparent substance, passing easily through it without being absorbed and without warming the mineral itself. It is of economic importance as a major source of potash for fertilizer.