
sedimentary
Sandstone Concretion
Moqui Marble (Iron-oxide concretion)
AI-generated identification · may be incorrectHardness: 5-5.5 (outer shell) to lower centered core; Color: Ochre, rusty brown, tan; Luster: Dull or earthy; Crystal structure: Amorphous or microcrystalline; Cleavage: None; Shape: Spherical to sub-spherical.
- Hardness
- 5-5
- Color
- Ochre, rusty brown, tan
- Luster
- Dull or earthy
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Physical properties
Hardness: 5-5.5 (outer shell) to lower centered core; Color: Ochre, rusty brown, tan; Luster: Dull or earthy; Crystal structure: Amorphous or microcrystalline; Cleavage: None; Shape: Spherical to sub-spherical.
Formation & geological history
Formed by the precipitation of mineral cement (usually hematite or goethite) within the spaces between sand grains. This process typically occurs in groundwater aquifers within sedimentary basins, often millions of years old.
Uses & applications
Used primarily as decorative curiosities, educational specimens in geology, and occasionally in metaphysical practices. Historically, native tribes used them as game stones.
Geological facts
In the American Southwest, these are often called 'Moqui Marbles' after the Hopi tribe. Similar spherical hematite concretions were discovered on Mars by the Opportunity rover, famously nicknamed 'blueberries'.
Field identification & locations
Identify by its distinct spherical shape and sandy texture. They are frequently found weathering out of sandstone formations, particularly the Navajo Sandstone in Utah and Arizona.
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