Willemite

Object/Artifact

-

Crater Rock Museum

Name/Title

Willemite

Entry/Object ID

2014.1.99

Description

Chemical Composition: Zn2SiO4 Crystal System: Hexagonal System Description: Common Name: Willemite,Calcite,Fluorite Chemistry: Zn2 Si O4 Class: Ortho-Silicates Location: Purple Passion Mine- Wickenburg, AZ. Description: A triangular chunk of Willemite strewn with Calcite crystals and a good size patch of Fluorite. PHYSICAL CHARACTERISTICS: • Color is usually colorless or white but can be tinted yellow, blue, red, brown and often green. • Luster is vitreous to resinous. • Transparency crystals are transparent to translucent. • Crystal System: trigonal; bar 3 • Crystal Habits include typically short prismatic crystals although some prismatic crystals can be rather long with sometimes very steep rhombohedral terminations. Also as granular, lamellar and fibrous masses. • Cleavage in good in one direction (basal) • Fracture is conchoidal to uneven. • Hardness is 5.5 • Specific Gravity is approximately 3.9 - 4.2 (above average for non-metallic minerals). • Streak is white. • Other Characteristics: strongly fluorescent green and sometimes phosphorescent. • Associated Minerals are zincite, franklinite, rhodonite, calcite, greenockite and other rare minerals. • Notable Occurrences include of course Franklin as well as Paterson and Sterling Hill, New Jersey and Mammoth Mine, Tiger, Arizona, USA; Morsnet, Belgium; St. Hilaire, Quebec; Tsumeb, Namibia and Greenland. • Best Field Indicators are fluorescence, associations, luster, cleavage and crystal habit. Fracture: Conchoidal Hardness: 6 Orthoclase Luster: Vitreous Occurrence: Willemite is a somewhat rare zinc mineral, but it was found in such great abundance at Franklin New Jersey that it instantly became an important ore of zinc. The deposit at Franklin, New Jersey is truly unique. Not only is willemite found there but other rare minerals are also found there, and some in amazingly large quantities. Minerals such as zincite, franklinite (named after the locality), rhodonite, greenockite, fluorescentcalcite , various zeolites and many other rare and interesting minerals are found at this amazing locality. The unique mineral assemblage is believed to have come into existance from the metamorphism of formerly oceanic floor, metallic mineral deposits that were oxidized into secondary minerals before metamorphism. In the case of willemite the secondary minerals were probably smithsonite and hemimorphite . At other localities for willemite it is more scarce and forms as a secondary mineral from primary zinc deposits. Dispite being discovered at Franklin first, it was a site in Belgium, where the mineral formed small brown crystals, that gave it its name, willemite. It seems that the minerologists at Franklin described the mineral but never named it. In the meantime the minerologists at Belgium named the mineral after William I of Belgium. Willemite is one of the few silicate minerals that have a trigonal symmetry. This symmetry is far more common among carbonates than among silicates. Willemite shares the same symmetry with the emerald green silicate dioptase and the closely related silicate phenakite. Although massive willemite is much more common, some crystals do show the rhombohedral terminations atop hexagonal prisms that is characteristic of it symmetry. Willemite's great desirability is not so much its use as a zinc ore, its rarity, its associations or even its crystal habits as it is its wonderful fluorescence. Nearly all willemite specimens fluoresce a bright green under ultra-violet light. This fluorescence combined with the red fluorescence of the calcite at Franklin, makes specimens from there even more special. Some willemite specimens will even show phosphorescence. Phosphorescence is the ability of a mineral to glow after the initial light is removed. The mineral has essentially stored the energy of the initial activating light and re-emits light on a delayed basis. Willemite is one of the best examples of a fluorescent mineral and is a must have for any collector interested in this phenomenon. Rock Type: Sedimentary Specific Gravity: 3.9-4.2 Streak: White

Collection

RAGM Mineral Collection

Acquisition

Accession

2014.1

Source or Donor

Crater Rock Museum (unknown donors)

Acquisition Method

Gift

Dimensions

Width

6-1/2 in

Depth

4-3/4 in

Length

10 in

Location

Location

Shelf

CS-D-5

Room

Curation Storage

Building

Crater Rock Museum

Category

Storage

Moved By

Curator

Date

March 7, 2024