Hemimorphite is a silicate mineral with zinc as the main component. It contains 53.7% zinc and sometimes contains a small amount of aluminum and iron. It is an important mineral of metallic zinc, and only a few colorless and transparent crystals are used as gems. Hemimorphite belongs to the orthorhombic crystal system, and the crystals are thin or shaped or cone-shaped, but single crystals are rare, usually dense granular, stalactite, grape-like, fibrous or bundle-like aggregates or porous and transparent to translucent Is 4.5-5. Its colors are white, gray, blou, light green, yellowish brown and brown, among which the blue energy is related to copper-containing impurity elements, and sometimes it is distributed in strips. Hemipolar ore has completely columnar cleavage in two directions, and the cleavage surface is pearly; it also has strong pyroelectricity and piezoelectricity.
Gem grade hemimorphite crystals are colorless and transparent, while rare yellow, green and light yellow transparent crystals can be processed into faceted gems. The dark blue block is the best, and the fibrous block can be polished into The opal species, and the cluster of bundles and cockscombs are valuable ornamental stones. Gemstones similar to Hemimorphites include prehnite, white lead ore, ens., which can be distinguished from these similar gemstones based on the hardness, specific gravity, refractive index, non-fluorescence and more zinc content of the Hemimorphite minerals: Class-grade heteropolar mine treasures are rare. Blue egg round gemstones weighing 1-3 carats have been found, produced in Mexico. A colorless crystal of Hemimorphite weighing 1.9 carats is in the collection of the Calgary Divo Group in Canada
Hemipolar minerals are produced in the oxidation zone of lead-zinc sulfide deposits. They are secondary minerals formed by weathering of primary zinc minerals. They are often symbiosis with smithsonite, white lead ore, galena, and green copper ore. Its origins are all over the world, mainly Mexico, the United States, Romania, Germany, Austria, Italy and the United Kingdom, ens., and most gem-grade heteropolar mines come from Mexico.
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