hemimorphite

There are also two minerals, zincite and hemimorphite, which have been historically called calamine.

Historically, smithsonite was identified with hemimorphite before it was realised that they were two distinct minerals.

Other crystals found in Mammoth Mine include hemimorphite, willemite, and quartz.

It occurs in association with hemimorphite, smithsonite, chrysocolla, coronadite and various iron oxides.

The Wenshan Zinc Mine is known for producing world class, deep blue hemimorphite specimens.

Associated minerals include: rosasite, smithsonite, hemimorphite, hydrozincite, malachite and azurite.

It occurs in association with brochantite, anglesite, caledonite, leadhillite, cerussite, malachite and hemimorphite.

It occurs associated with smithsonite, hemimorphite, willemite, cerussite, aurichalcite, calcite and limonite.

The silicate was the more rare of the two, and was named hemimorphite because of the hemimorph development of its crystals.

It occurs in association with chalcocite, bornite, willemite, smithsonite, hydrozincite, hemimorphite, adamite, olivenite and gebhardite.

Stotts discovered galena and hemimorphite deposits west of the town and began to develop the lead mining industry that later fueled Stotts City's booming growth.

It has been found in association with cerussite, descloizite, hemimorphite, hopeite, hydrozincite, "limonite", parahopeite, pyromorphite, scholzite, smithsonite, and vanadinite.

Sphalerite ZnS (primary) alters to secondary hemimorphite ZnSiO(OH).

Zinc silicate ZnSiO(O H) HO or hemimorphite.

It occurs with cerussite, anglesite, smithsonite, hemimorphite, vanadinite, pyromorphite, mimetite, descloizite, plattnerite and various iron and manganese oxides.

Metallurgists wishing to produce brass thus used calamine (actually a mixture of the virtually indistinguishable zinc ores smithsonite and hemimorphite) as the zinc component of brass.

It occurs in the oxidized zone of ore deposits and is associated with dioptase, wulfenite, hemihedrite, phoenicochroite, duftite, mimetite, shattuckite, chrysocolla, hemimorphite, willemite and fluorite.

The regions on the Belgian-German border are well known for their deposits of hemimorphite of metasomatic origin, especially Vieille Montagne in Belgium and Aachen in Germany.

Associated minerals include the lead minerals anglesite and galena, the zinc minerals sphalerite, hemimorphite, and smithsonite, and gangue minerals quartz, calcite, goethite, and dolomite.

Ashburtonite is associated with beudantite, brochantite, calerdonite, cerussite, diaboleite, duftite, malachite, platterite, adamite, antlerite, bayldonite, bindheimite, carminite, chenevixite, chlorargyrite, chrysocolla, cinnabar, hemimorphite, hydrozincite, jarosite, lavendulan, linarite, mimatite, olivenite, paratacamite, and rosasite.

The 117 species now known from the deposit include adamite (in an array of colors and habits), legrandite, kottigite/parasymplesite, and paradamite, as well as specimens of scorodite, hemimorphite, plattnerite, aurichalcite, rosasite, fluorite, calcite, wulfenite and other species.

It occurs in weathered hydrothermal base-metal deposits as hay-like bundles of dark prismatic crystals with a length of a few millimeters; the bundles grow on, or sometimes within various minerals, including cerussite, smithsonite, hemimorphite, leadhillite, hydrozincite, rosasite, aurichalcite, murdochite, limonite, pyromorphite, wulfenite, calcite and quartz.