Rock Identifier
Hematite Nodules (Moqui Marbles or similar) (Iron oxide (Fe2O3)) — mineral
mineral

Hematite Nodules (Moqui Marbles or similar)

Iron oxide (Fe2O3)

Hardness: 5.5-6.5; Color: Steel-gray to reddish brown; Luster: Metallic to sub-metallic; Crystal Structure: Trigonal/Hexagonal; Specific Gravity: 5.26; Streak: Cherry-red

Hardness
5
Color
Steel-gray to reddish brown
Luster
Metallic to sub-metallic
Identified More mineral
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Physical properties

Hardness: 5.5-6.5; Color: Steel-gray to reddish brown; Luster: Metallic to sub-metallic; Crystal Structure: Trigonal/Hexagonal; Specific Gravity: 5.26; Streak: Cherry-red

Formation & geological history

Formed by precipitation from iron-rich groundwater passing through permeable sandstone. Iron minerals aggregate around a nucleus, often during the Jurassic or Cretaceous periods.

Uses & applications

Major ore of iron; used in jewelry (as hematine), polishing compounds (jeweller's rouge), and grounding stones in metaphysical practices.

Geological facts

Hematite was found on Mars by the Opportunity rover, indicating that water was once present on the Red Planet since the mineral usually forms in aqueous environments.

Field identification & locations

Identified by its high density for its size and its distinctive reddish-brown streak when rubbed on unglazed porcelain. Commonly found in desert regions of Utah (USA).