Rock Identifier
Hematite Nodules (Moqui Marbles) (Ferric Oxide (Fe2O3)) — mineral
mineral

Hematite Nodules (Moqui Marbles)

Ferric Oxide (Fe2O3)

Hardness: 5-6.5 (Mohs scale); Color: Dark brown, black, to metallic grey; Luster: Metallic to earthy; Crystal Structure: Trigonal (often found in botryoidal or concretionary forms); Specific Gravity: 5.26

Hardness
5-6
Color
Dark brown, black, to metallic grey
Luster
Metallic to earthy
Identified More mineral

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 5-6.5 (Mohs scale); Color: Dark brown, black, to metallic grey; Luster: Metallic to earthy; Crystal Structure: Trigonal (often found in botryoidal or concretionary forms); Specific Gravity: 5.26

Formation & geological history

Formed by the precipitation of iron oxide from mineral-rich groundwater flowing through porous sandstone. These nodules often grow around a nucleus like a shell or sand grain over millions of years.

Uses & applications

Primary ore for iron production. Also used as jewelry, in pigments (red ochre), as a polishing agent (jeweler's rouge), and in alternative healing practices.

Geological facts

Hematite is famous for its 'blood-red' streak when rubbed against an unglazed porcelain plate. On Mars, spherical hematite concretions are nicknamed 'blueberries' and provided evidence of past water.

Field identification & locations

Identify by its high density (feels heavy for its size) and its reddish-brown streak. Commonly found in desert environments like the Southwestern United States, particularly in the Navajo Sandstone.