
Mineral
Rutilated Quartz
Quartz (SiO2) with Rutile (TiO2) inclusions
Hardness: 7 on Mohs scale. Color: Clear to smoky gray, often with golden, silver, or greenish rutile inclusions, giving it a fibrous or hair-like appearance. Luster: Vitreous (glassy) when polished. Crystal Structure: Hexagonal (trigonal) system.…
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous (glassy) when polished
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Physical properties
Hardness: 7 on Mohs scale. Color: Clear to smoky gray, often with golden, silver, or greenish rutile inclusions, giving it a fibrous or hair-like appearance. Luster: Vitreous (glassy) when polished. Crystal Structure: Hexagonal (trigonal) system. Often found as prismatic crystals with striations parallel to the C-axis. No clear cleavage, exhibits conchoidal fracture. Specific Gravity: 2.65.
Formation & geological history
Formation Process: Rutilated quartz forms when rutile (titanium dioxide) inclusions are trapped within quartz crystals during their growth. This typically occurs in hydrothermal veins and pegmatites where silica-rich fluids cool and crystallize, often at elevated temperatures and pressures. The rutile needles are formed prior to or simultaneously with the quartz, becoming encapsulated within the growing quartz structure. Geological Age: Varies widely depending on the geological setting, ranging from hundreds of millions to several billion years old.
Uses & applications
Uses: Primarily used in jewelry for its unique visual appeal, especially in cabochons, beads, and faceted stones. Also highly sought after by mineral collectors. Less commonly used in industrial applications, as clear quartz without inclusions is generally preferred for optical or electronic uses.
Geological facts
Rutilated quartz is highly valued by collectors and in metaphysical circles for its unique appearance, which is literally 'rutile hair' within the quartz. The included rutile can form various patterns, from randomly dispersed needles to star-like bursts or parallel bundles. The Schiller effect or chatoyancy can be observed when the rutile needles are aligned. It's sometimes referred to as 'Venus hair' or 'Angel hair' in spiritual contexts.
Field identification & locations
How to Identify in the Field: The most distinctive feature is the presence of metallic (often golden, sometimes silvery or reddish) needle-like inclusions within a transparent to translucent quartz host. These inclusions are rutile. The quartz host itself will exhibit typical quartz properties. Common Locations: Brazil (especially Minas Gerais), Madagascar, Australia, Kazakhstan, Norway, Pakistan, and the United States (e.g., North Carolina). Tips for Collectors: Look for clear quartz with well-formed, visible rutile needles. The density and color of the rutile can vary, influencing the stone's value. Larger, well-defined inclusions are generally more desirable.
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