
mineral
Hematite
Hematite (Fe2O3)
Hardness: 5.5 to 6.5 on Mohs scale. Color: Dark reddish-brown to steel-gray or black. Luster: Metallic to submetallic or earthy. Crystal Structure: Trigonal. Cleavage: None, exhibits uneven to conchoidal fracture. Specific Gravity: 5.26.
- Hardness
- 5
- Color
- Dark reddish-brown to steel-gray or black
- Luster
- Metallic to submetallic or earthy
Identified More mineral →
Explore Hematite in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 5.5 to 6.5 on Mohs scale. Color: Dark reddish-brown to steel-gray or black. Luster: Metallic to submetallic or earthy. Crystal Structure: Trigonal. Cleavage: None, exhibits uneven to conchoidal fracture. Specific Gravity: 5.26.
Formation & geological history
Forms in a diverse range of environments, primarily aqueous sedimentary settings, hydrothermal veins, and as an accessory mineral in igneous and metamorphic rocks. Can form over a vast geological timescale through precipitation from iron-rich waters.
Uses & applications
Primary ore of iron used in steel production, also utilized as a pigment, in heavy media separation, jewelry, and ornamental carvings.
Geological facts
Hematite is the most important ore of iron worldwide and is responsible for the characteristic red color of soils on Mars.
Field identification & locations
Easily identified by its characteristic reddish-brown streak on an unglazed porcelain streak plate, despite its dark metallic appearance. Commonly found worldwide, especially in banded iron formations.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Soil with Mineral Detritus and Quartz Fragments
Regolith / Silicate Mineral Aggregate
sedimentary
Limonite / Goethite (Iron Ore Mineral nodule)
FeO(OH)·nH2O / FeO(OH)
mineral
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral