How to identify Botryoidal Hematite
Hematite (Fe2O3) with botryoidal habit
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Open the appTo correctly identify Botryoidal Hematite (Hematite (Fe2O3) with botryoidal habit), 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
Color
Overall color and any zoning or banding
Steel-gray to black, sometimes with an iridescent tarnish. Internally, it can be reddish-brown.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Metallic to submetallic, sometimes dull in massive forms.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Characteristically rounded, globular, or mammillary aggregates, resembling bunches of grapes or kidneys.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Botryoidal, mammillary, reniform (kidney-shaped). Individual crystals are typically microscopic within the aggregates.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None observed in botryoidal forms due to its aggregate nature; however, hematite itself has no true cleavage but exhibits parting on {0001} and {1011}.
- 6
Geological Environment
The rock formation and setting where it occurs
Hydrothermal veins, sedimentary deposits (e.g., banded iron formations), contact metamorphic zones, and as a secondary mineral in oxidized zones of ore deposits. Often found in cavities or open spaces where precipitation can occur freely.
Key Facts
- Hardness
- 5.5 - 6.5 on Mohs scale
- Specific Gravity
- 5.26 g/cm³ (pure hematite)
- Crystal System
- Trigonal
- Color
- Steel-gray, black, reddish-brown (in thin splinters or powder)
- Luster
- Metallic to submetallic, dull to earthy in some varieties
- Transparency
- Opaque
- Fracture
- Uneven to subconchoidal
- Cleavage
- None (parting on {0001} and {1011} is observed in some crystalline forms, but not typically in botryoidal aggregates)
- Composition
- Iron(III) oxide (Fe2O3)
Physical characteristics
- Crystal Habit: Botryoidal, mammillary, reniform, massive, micaceous (specularite), oolitic, columnar, stalactitic, tabular crystals.
- Cleavage Type: None (parting is present in some crystalline forms)
- Fracture Type: Uneven to subconchoidal
- Tenacity: Brittle
- Luster Type: Metallic to submetallic, dull to earthy
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