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How to identify Hematite

Hematite

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To correctly identify Hematite (Hematite), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.

Step-by-step identification

  1. 1

    Color

    Overall color and any zoning or banding

    Variable: steel-gray, silver-gray, black, reddish-brown, or red. The color can be metallic, dull, or earthy.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Metallic (specular hematite), submetallic, dull, or earthy.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Can be massive, granular, botryoidal (kidney ore), reniform, mammillary, micaceous (specular hematite), columnar, or oolitic.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically forms in the trigonal system. Crystals are often tabular, rhombohedral, or platy. Massive, botryoidal, and micaceous forms are common.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. Hematite exhibits no true cleavage, but it can show a parting parallel to the basal pinacoid {0001} and rhombohedral faces {1011}.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in igneous, metamorphic, and sedimentary rocks. Common in Banded Iron Formations (BIFs), hydrothermal veins, contact metamorphic deposits, and as an alteration product in weathered rocks and soils.

Key Facts

Hardness
5.5-6.5 on the Mohs scale
Specific Gravity
4.9-5.3
Crystal System
Trigonal
Color
Steel-gray, black, reddish-brown, or red
Luster
Metallic, submetallic, dull, or earthy
Transparency
Opaque
Fracture
Uneven to subconchoidal
Cleavage
None (parting sometimes observed)
Composition
Iron oxide (Fe2O3)

Physical characteristics

  • Crystal Habit: Massive, botryoidal, reniform, mammillary, micaceous (specular hematite), columnar, tabular, rhombohedral, oolitic.
  • Cleavage Type: None. Parting on {0001} and {1011} is sometimes observed due to twinning or exsolution lamellae.
  • Fracture Type: Uneven to subconchoidal.
  • Tenacity: Brittle.
  • Luster Type: Metallic, submetallic, dull, or earthy.

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