
mineral
Hematite Concretion
Iron(III) oxide (Fe2O3)
Hardness: 5.5-6.5 Mohs; Color: reddish-brown to grey; Luster: metallic to earthy; Crystal Structure: Trigonal (often found in botryoidal or concretionary forms); Specific Gravity: 5.26.
- Hardness
- 5
- Color
- reddish-brown to grey
- Luster
- metallic to earthy
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Physical properties
Hardness: 5.5-6.5 Mohs; Color: reddish-brown to grey; Luster: metallic to earthy; Crystal Structure: Trigonal (often found in botryoidal or concretionary forms); Specific Gravity: 5.26.
Formation & geological history
Formed through the precipitation of iron-rich fluids passing through porous sedimentary rock (like sandstone). These concretions grow over thousands to millions of years around a central nucleus.
Uses & applications
Primarily used as an ore of iron. Also used in pigments, jewelry (beads), and as a popular specimen for educational or metaphysical collections.
Geological facts
These are often nicknamed Moqui Marbles, Martian Blueberries, or Shaman Stones. Similar hematite nodules were discovered on Mars by the Opportunity rover, suggesting liquid water was once present.
Field identification & locations
Identify by their high weight relative to size (high density), reddish-brown streak, and often perfectly spherical or pebble-like shapes. Found in arid sedimentary basins like the Navajo Sandstone in Utah.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock