
Mineral
Rutilated Quartz
Quartz (SiO2) with Rutile inclusions (TiO2)
Hardness: 7 (Mohs scale) for quartz, 6-6.5 for rutile. Color: Clear, smoky, or milky quartz with golden, reddish-brown, or black needle-like rutile inclusions. Luster: Vitreous (glassy). Crystal Structure: Trigonal (quartz), Tetragonal (rutile).…
- Hardness
- 7 (Mohs scale) for quartz, 6-6
- Luster
- Vitreous (glassy)
Identified More mineral →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 7 (Mohs scale) for quartz, 6-6.5 for rutile. Color: Clear, smoky, or milky quartz with golden, reddish-brown, or black needle-like rutile inclusions. Luster: Vitreous (glassy). Crystal Structure: Trigonal (quartz), Tetragonal (rutile). Cleavage: None (quartz), good prismatic cleavage (rutile, though typically not visible in inclusions). Specific Gravity: Approximately 2.65 (quartz), 4.2-4.3 (rutile).
Formation & geological history
Rutilated quartz forms when titanium dioxide (rutile) needles grow within a quartz crystal during its formation. This typically occurs in hydrothermal veins and pegmatites, where superheated mineral-rich water solutions cool and allow the crystallization of quartz, with rutile needles forming concurrently or being encapsulated as the quartz grows. The geological age can vary widely, from hundreds of millions to tens of millions of years, depending on the specific geological event and location.
Uses & applications
Rutilated quartz is highly valued in the jewelry industry for its unique aesthetic appeal. It is commonly used in rings, pendants, earrings, and beads like those shown in the image. It is also collected as a mineral specimen. In some cultures, it is believed to have metaphysical properties, such as amplifying energy and promoting spiritual growth.
Geological facts
The inclusions in rutilated quartz are often referred to as 'angel hair' or 'Venus hair' due to their delicate, thread-like appearance. The color of the rutile needles can vary from golden yellow (most common) to reddish-brown, copper, and even black, depending on the presence of iron or other trace elements within the rutile. Some specimens can exhibit fine, dense rutile hairs, while others may have thicker, sparser needles.
Field identification & locations
Rutilated quartz can be identified in the field by its characteristic clear to translucent quartz host with visible, often golden, needle-like or hair-like inclusions within. The hardness test (scratching glass) can help confirm it is quartz. It is commonly found in Brazil (especially Minas Gerais), Australia, Madagascar, Russia, Pakistan, India, Sri Lanka, and the USA (e.g., North Carolina, Arkansas). When collecting, look for strong clarity in the quartz and well-formed, aesthetically pleasing rutile inclusions. Avoid specimens with significant fractures or poor clarity.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral
Epidote
Epidote - Ca2(Al2,Fe3+)3(SiO4)3(OH)
mineral