Hematite specimen

Crystal & mineral guide

Hematite

Fe₂O₃

OreOxideHeritage

Primary iron ore mineral — also cut as metallic gray beads and cabochons.

Identify Hematite with RockScan

About Hematite

Hematite is the world's main iron ore. Specular hematite shows bright metallic plates; massive material is cut into heavy metallic jewelry. Diagnostic cherry-red streak separates it from similar dark minerals. Dense feel is immediate in hand.

Hematite belongs in a crystal identifier workflow because photo cues — color zoning, crystal habit, and surface luster — combine with measurable traits like Mohs 5–6 and specific gravity 4.9–5.3. Use RockScan’s camera to get a first-pass ID, then confirm with the checklist below.

Hematite properties

Mohs hardness5–6
Crystal systemTrigonal
LusterMetallic to dull earthy
ColorSteel-gray to black; red streak
CompositionIron(III) oxide
FormationSedimentary BIFs, hydrothermal, and metamorphic deposits
OccurrenceWorldwide; Brazil, Australia, USA, UK (specular)
Specific gravity4.9–5.3
CleavageNone (parting possible)

How to identify Hematite

  1. Cherry-red streak on unglazed porcelain
  2. High SG — notably heavy
  3. Metallic gray polish vs red earthy varieties

Collector notes

  • Name from Greek 'haima' — blood, for the red streak
  • Banded iron formations record early Earth oxygen rise

Value context: Ore grades by Fe content; jewelry values bright metallic polish and weight.

Hematite FAQ

How do you identify Hematite?

Hematite (Fe₂O₃) is typically recognized by steel-gray to black; red streak color, metallic to dull earthy luster, Mohs hardness 5–6, and trigonal crystal system. RockScan can suggest Hematite from a photo and surface these checks on the result card.

What is Hematite made of?

Hematite composition: Iron(III) oxide. It forms via sedimentary bifs, hydrothermal, and metamorphic deposits and is found in Worldwide; Brazil, Australia, USA, UK (specular).

Is Hematite valuable?

Ore grades by Fe content; jewelry values bright metallic polish and weight.