
sedimentary
Moqui Marble (Ironstone Concretion)
Goethite/Hematite Concretion (Fe2O3 / FeO(OH))
AI-generated identification · may be incorrectHardness: 5-5.5 (outer shell), 3-4 (inner core). Color: Dark brown, rusty orange, or tan. Luster: Dull/Earthy to sub-metallic. Crystal structure: Amorphous or microcrystalline shell around a sandstone center.
- Hardness
- 5-5
- Color
- Dark brown, rusty orange, or tan
- Luster
- Dull/Earthy to sub-metallic
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Physical properties
Hardness: 5-5.5 (outer shell), 3-4 (inner core). Color: Dark brown, rusty orange, or tan. Luster: Dull/Earthy to sub-metallic. Crystal structure: Amorphous or microcrystalline shell around a sandstone center.
Formation & geological history
Formed during the Jurassic period (approx. 190 million years ago) via groundwater precipitation. Iron minerals dissolved in water precipitated around a nucleus within porous sandstone, eventually forming a hardened shell.
Uses & applications
Primarily collected as geological curiosities, used in metaphysical practices ('shaman stones'), and studied by NASA as terrestrial analogs to 'blueberries' found on Mars.
Geological facts
They are named after the Hopi Tribe (formerly 'Moqui'). On Mars, the Opportunity rover found near-identical structures composed of hematite, suggesting that liquid water once existed on the Red Planet.
Field identification & locations
Identified by their round/ellipsoidal shape, heavy weight for their size, and distinct dark iron-rich crust. Found primarily in the Navajo Sandstone of Utah and Arizona. Collectors should look for weathered outcrops.
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