
mineral
Rutilated Quartz
Quartz with Rutile inclusions (SiO2 with TiO2 inclusions)
Hardness: 7 (Quartz), 6-6.5 (Rutile); Color: Clear to smoky quartz base with golden, reddish, or black rutile needles; Luster: Vitreous; Crystal Structure: Hexagonal (Quartz), Tetragonal (Rutile); Cleavage: None (Quartz), Prismatic (Rutile); Specific Gravity: 2.65 (Quartz)
- Hardness
- 7 (Quartz), 6-6
- Luster
- Vitreous
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Physical properties
Hardness: 7 (Quartz), 6-6.5 (Rutile); Color: Clear to smoky quartz base with golden, reddish, or black rutile needles; Luster: Vitreous; Crystal Structure: Hexagonal (Quartz), Tetragonal (Rutile); Cleavage: None (Quartz), Prismatic (Rutile); Specific Gravity: 2.65 (Quartz)
Formation & geological history
Rutilated quartz forms when titanium dioxide (rutile) needles crystallize within the growing quartz crystal. This typically occurs in hydrothermal veins and pegmatites, often associated with granitic igneous activity. The temperature and pressure conditions during quartz growth influence the inclusion of rutile. Its geological age varies depending on the specific quartz deposit, ranging from millions to billions of years old.
Uses & applications
Primarily used in jewelry for its attractive inclusions, which create unique patterns. It's often cut into cabochons, beads (as seen in the image), and faceted stones. Due to its aesthetic appeal, it's also sought after by mineral collectors.
Geological facts
The 'needles' of rutile within the quartz can vary greatly in thickness, density, and color, making each piece unique. Historically, rutilated quartz was sometimes called 'Venus Hair Stone' or 'Angel Hair' due to the fine, golden inclusions. It is believed by some to have metaphysical properties, such as enhancing energy and clarity.
Field identification & locations
Rutilated quartz is identified by its clear to smoky quartz base containing distinct needle-like inclusions of rutile, which can be golden, reddish-brown, or black. These inclusions are typically thin and straight, but can sometimes be curved or clustered. It can be found in various locations worldwide, including Brazil (a major source), Australia, Kazakhstan, Madagascar, Norway, Pakistan, and the United States (especially Arkansas). In the field, look for quartz crystals with visible internal fibrous or needle-like structures that are distinct from fractures or other mineral growths. Its hardness of 7 helps distinguish it from softer minerals.
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