Lansfordite | |
---|---|
General | |
Category | Carbonates |
Formula (repeating unit) | MgCO3·5H2O |
IMA symbol | Lfd[1] |
Strunz classification | 5/D.01-30 |
Dana classification | 15.1.6.1 |
Crystal system | Monoclinic |
Space group | P21/c (No. 14) |
Unit cell | a=7.3458 Å, b=7.6232 Å, c=12.4737 Å, β=101.722° |
Identification | |
Formula mass | 174.39 |
Colour | Colourless, white after exposure |
Crystal habit | Crystals, stalactites terminated by crystal faces, efflorescences, parallel growths. |
Cleavage | Perfect, Distinct |
Mohs scale hardness | 2.5 |
Luster | Vitreous (if fresh) |
Streak | White |
Diaphaneity | Translucent, opaque after exposure |
Specific gravity | 1.6 |
Density | 1.6 |
Birefringence | 0.042 |
Lansfordite is a mineral of magnesium carbonate (MgCO
3). It represents the pentahydrate of magnesium carbonate, and has the total formula MgCO3·5H2O
.[2] Landsfordite was discovered in 1888 in a coal mine in Lansford, Pennsylvania. It crystallizes in the monoclinic system (space group P21/c[3]) and typically occurs as colorless to white prismatic crystals and stalactitic masses.[4] It is a soft mineral, Mohs hardness of 2.5, with a low specific gravity of 1.7. It is transparent to translucent with refractive indices of 1.46 to 1.51.[5] The mineral will effloresce at room temperature, producing nesquehonite.[6]