
mineral
Red Jasper
Silicon Dioxide (SiO2) mixture
Hardness: 6.5-7 Mohs; Color: Brick red to brownish red due to iron inclusions; Luster: Vitreous to dull; Crystal structure: Trigonal (Microcrystalline); Cleavage: None; Opaque.
- Hardness
- 6
- Color
- Brick red to brownish red due to iron inclusions
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brick red to brownish red due to iron inclusions; Luster: Vitreous to dull; Crystal structure: Trigonal (Microcrystalline); Cleavage: None; Opaque.
Formation & geological history
Formed primarily in sedimentary environments via the deposition of silica from volcanic ash or water, often colored by iron oxides during hydrothermal processes or metamorphosed within iron-rich deposits.
Uses & applications
Used extensively in jewelry as beads and cabochons, for decorative carvings, as an ornamental stone in construction, and held in high regard by rock collectors for its unique banding and patterns.
Geological facts
Red jasper has been used since antiquity; it was known as the 'mother of all stones' in some cultures and was used by ancient Egyptians and Minoans for amulets, seals, and talismans.
Field identification & locations
Identify by its brick-red color, extreme hardness (it will scratch glass), and smooth, waxy surface when river-worn. Common in stream beds and coastal regions where silica-rich rocks have eroded.
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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