Cavradi gorge, Curnera Valley, Tujetsch (Tavetsch), Vorderrhein Valley, Grischun (Grisons; Graubünden), Switzerland
Fe2O3
Crystal System: trigonal
Colour: steel-grey, black or bright rust-red
Lustre: metallic, sub-metallic, dull, earthy
Habitus: tabular, rhombohedral, prismatic or rarely scalenohedral
Hardness: 5 - 6
Fracture: irregular/uneven or sub-conchoidal
Cleavage: none
Density: 5.255 g/cm3
Origin and geological occurrence: hematite is abundant on weathered iron-bearing rocks. It is an accessory mineral in felsic igneous rocks and in high-temperature hydrothermal veins. Also found as a product of contact metamorphism. A huge quantity of hematite has been found in the so called BIFs (Banded iron Formations): metamorphosed sedimentary marine rock.
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