Earth Record
Mineralogy and formation
Moqui marbles (also Moki marbles) are iron oxide concretions found in the Navajo Sandstone of southern Utah. The concretions formed when iron-bearing groundwater flowed through the porous sandstone approximately 2-5 million years ago, precipitating concentric shells of iron oxide (primarily hematite and goethite) around nucleation points in the sand. The result is rounded to disc-shaped nodules with a hard iron oxide shell enclosing sandstone.
They range from marble-size to several inches in diameter. Similar iron oxide concretions were discovered on Mars by the Opportunity rover (nicknamed "blueberries"), and the comparison has made Moqui marbles scientifically significant as terrestrial analogues for Martian geological processes. The name comes from the Moqui (Hopi) people.
Hematite Component: Trigonal (R-3C); Goethite Component: Orthorhombic (Pbnm) structure
Chemical FormulaOuter shell: primarily Fe2O3 (hematite) and FeO(OH) (goethite); interior: loose quartz sand (SiO2) cemented by iron oxidesCrystal SystemHematite Component: Trigonal (R-3C); Goethite Component: Orthorhombic (Pbnm)Mohs Hardness5Specific Gravity3.5-5.3 (shell material); lower overall due to porous sandy interiorLusterMetallic to submetallic on shell surface; earite to dull on weathered surfacesColorBrownIMA StatusrockType LocalityNavajo Sandstone, south-central and southeastern Utah, USAIMA NumberNo IMA number (rock, not approved mineral species) USA (Utah)
Telling it apart
Moqui marbles are iron oxide concretions, typically hematite and goethite shells around a sandstone core, found in the Navajo Sandstone of southern Utah. Sellers sometimes confuse them with clay balls, slag, or manufactured iron spheres. The field check is weight and surface texture: genuine moqui marbles have a rough iron oxide rind that is heavier than sandstone but lighter than solid iron, with specific gravity variable depending on core density.
They are not hollow like some geodes and not uniformly metallic like manufactured balls. Hardness of the iron shell runs about 5 to 6. If the sphere is perfectly smooth, perfectly round, and uniformly heavy, it may be manufactured. Real moqui marbles show surface irregularities, natural weathering textures, and sometimes exposed sandy cores where the shell has broken. Because these concretions form naturally in sedimentary environments over millions of years, authenticity depends on geological origin, not mineral species.
Spotting the real thing
Moqui marbles: iron oxide concretions with a hard hematite shell enclosing a softer sandy interior. The shell is magnetic (attracted to a magnet). Specific gravity of shell material 3.
5-5. 3. If the concretion is not magnetic at all, it may be a non-iron concretion.
Natural Moqui marbles from Utah show a range of smooth to textured surfaces.
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