Smithsonite
A variety of Calcite Group
What is Smithsonite?
Smithsonite is a tricky mineral to correctly identify because it can present itself in various colors. Centuries ago, it was once the primary source for zinc mining; however, other minerals have now taken its place. This crystal is too soft to be very useful in the gem trade. It was given the name smithsonite after James Smithson, of Smithsonian Museum fame.
Etymology & Origins
Historically, smithsonite was identified with hemimorphite before it was realized that they were two different minerals. The two minerals are very similar in appearance and the term calamine has been used for both, leading to some confusion. The distinct mineral smithsonite was named in 1832 by François Sulpice Beudant in honor of English chemist and mineralogist James Smithson (c.1765–1829), whose bequest established the Smithsonian Institution and who first identified the mineral in 1802.
Uses & Applications
Smithsonite is an important source of zinc in some areas. Zinc is added to vitamin supplements and is used in applications such as pennies, tires, paint, sunscreen, batteries, galvanizing metals, and making alloys. Smithsonite also used as an ornamental stone and gemstone.
Healing Properties
Smithsonite is often used to reduce stress and calm emotions. Many say it is a powerful stone that helps declutter the mind, improve clarity and allow for better resolutions when used during challenging times. It is believed to help with depression, low energy levels, and shyness. Use of this stone can empower a person to find their inner strengths and become confident in their decision making.
Optical Properties
- Refractive Index
- 1.620-1.850
- Birefringence
- 0.228
- Pleochroism
- None
- Optical Character
- Uniaxial negative
- Dispersion
- 0.014-0.031
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Associated Chakras
Key Characteristics
Characteristics of Smithsonite
Smithsonite is a variably colored trigonal mineral which only rarely is found in well formed crystals. The typical habit is as earthy botryoidal masses. It has a Mohs hardness of 4.5 and a specific gravity of 4.4 to 4.5.
Formation of Smithsonite
Smithsonite occurs as a secondary mineral in the weathering or oxidation zone of zinc-bearing ore deposits. It sometimes occurs as replacement bodies in carbonate rocks and as such may constitute zinc ore. It commonly occurs in association with hemimorphite, willemite, hydrozincite, cerussite, malachite, azurite, aurichalcite and anglesite. It forms two limited solid solution series, with substitution of manganese leading to rhodochrosite, and with iron, leading to siderite.
Health & Safety Information
- ⚠️Harm Reason: Smithsonite dust is toxic because it contains heavy metals Zinc.
- ⚠️Heavy Metal: Zinc
- ⚠️How to prevent the risks of Smithsonite?
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Quick Facts
Physical Properties
- Color
- White, grey, yellow, green to apple-green, blue, pink, purple, bluish grey, brown, colourless, faintly tinted
- Hardness (Mohs)
- 4 - 4.5
- Density
- 4.43 g/cm³
- Streak
- White
- Luster
- Pearly, Vitreous
- Crystal System
- Trigonal
Chemical Properties
- Chemical Formula
- ZnCO3
- Elements
- C, O, Zn
Also Known As
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