Science Fair Project Encyclopedia
Magnesite
| Magnesite | |
|---|---|
| Image needed | |
| General | |
| Category | Mineral |
| Chemical formula | magnesium carbonate:MgCO3 |
| Identification | |
| Color | White |
| Crystal habit | usually massive, rarely as rhombohedrons or hexagonal prisms |
| Crystal system | trigonal; bar 3 2/m |
| Cleavage | [1011] Perfect, [1011] Perfect, [1011] Perfect |
| Fracture | Brittle - Conchoidal |
| Mohs Scale hardness | 3.5 - 5 |
| Luster | Vitreous |
| Refractive index | Uniaxial (-) nω=1.508 - 1.510 nε=1.700 |
| Pleochroism | N/A |
| Streak | white |
| Specific gravity | 3.0 - 3.2 |
| Fusibility | infusible |
| Solubility | Effervesces in hot HCl |
| Other Characteristics | |
Magnesite is magnesium carbonate, MgCO3. Iron (as Fe2+) substitutes for Mg with a complete solution series with siderite, FeCO3. Calcium, manganese, cobalt, and nickel may also occur in small amounts. Dolomite, (Mg,Ca)CO3, is almost indistinguishable from magnesite.
Magnesite occurrs as veins in and an alteration product of serpentine and other magnesium rich rock types in both contact and regional metamorphic terranes. These magnesites often are cryptocrystalline and contain silica as opal or chert.
References and external links
- Dana's Manual of Mineralogy ISBN 0471032883
- Mineral Galleries
- Webmineral.com
- Mindat.org
- Minerals.net
10-26-2009 08:16:03
The contents of this article is licensed from www.wikipedia.org under the GNU Free Documentation License. Click here to see the transparent copy and copyright details
The contents of this article is licensed from www.wikipedia.org under the GNU Free Documentation License. Click here to see the transparent copy and copyright details