Siderite | |
Chemical Formula |
FeCO3 |
Species |
Carbonates |
Crystal System |
Trigonal |
Mohs Scale |
3-4 |
Specific Gravity |
3.96 |
Color |
Pale yellow to tannish, grey, brown, green, red, black and sometimes nearly colorless |
Streak |
White |
Luster |
Vitreous, Silky, Pearly |
Refractive Index |
n = 1.875 n = 1.633 |
Diaphaneity |
Translucent |
Cleavage |
PerfectPerfect on . |
Fracture |
Irregular/Uneven, Conchoidal |
Crystal Habit:Tabular crystals, often curved - botryoidal to massive | |
Geological Setting:Most often found in bedded sedimentary deposits with a biological component, with shales, clays and coal beds - suggesting that the siderite is biogenically created under low-oxygen and low-Ph conditions. It is also found in metamorphosed sedimentary rocks as more massively crystalline material, as a primary gangue mineral in hydrothermal deposits, and in pegmatites, including nepheline syenite pegamtites; as bog deposits. |