
Mineral
Pink Thulite
Thulite (Ca2Al3(SiO4)3(OH)) - Pink Zoisite
AI-generated identification · may be incorrectHardness: 6-6.5 on Mohs scale; Color: Pink, rose-red, or reddish-brown; Luster: Vitreous to pearly; Crystal Structure: Orthorhombic; Cleavage: Perfect in one direction; Specific Gravity: 3.10-3.38
- Hardness
- 6-6
- Color
- Pink, rose-red, or reddish-brown
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Pink, rose-red, or reddish-brown; Luster: Vitreous to pearly; Crystal Structure: Orthorhombic; Cleavage: Perfect in one direction; Specific Gravity: 3.10-3.38
Formation & geological history
Formed through regional metamorphism or hydrothermal alteration of basic igneous rocks or calcium-rich sedimentary rocks. It is often found in quartz veins and manganese-bearing rocks.
Uses & applications
Used primarily as a decorative stone, in jewelry (cabochons and beads), and as a carving material for ornamental objects. It is a popular collector's mineral.
Geological facts
First discovered in Sauland, Norway, in 1820 and named after the mythical island of Thule. It gets its distinctive pink color from trace amounts of manganese (Mn) replacing calcium in the crystal structure.
Field identification & locations
Identify by its unique 'bubblegum pink' color mottled with white calcite or quartz. Most commonly found in Norway, but also in Namibia, Australia, and parts of the United States like North Carolina and Washington.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary