Rutile is most recognized by collectors as slender, needle-like inclusions within clear Quartz, often called 'rutilated quartz'. It forms distinctive tetragonal crystals that can appear in reticulated or 'sagenite' clusters and is a major ore of titanium.
Is this rutile?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch rutile with a known reference. Rutile sits at Mohs 6-6.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale brown, yellowish brown; gray, greenish black with high Nb–Ta.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine to submetallic.
- 4Match the color rangeCompare against the expected color range: reddish-brown, red, black, yellowish, blood red, bluish, brownish yellow, brown red, violet.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: acicular, massive, prismatic.
Often confused with
Rutile vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Rutile leaves pale brown, yellowish brown; gray, greenish black with high nb–ta, Brookite leaves white to grayish white or yellowish white; luster reads adamantine to submetallic on Rutile and metallic adamantine to submetallic on Brookite.

How to tell apart: Streak differs, so Rutile leaves pale brown, yellowish brown; gray, greenish black with high nb–ta, Anatase leaves white to pale yellow.

How to tell apart: Streak differs, so Rutile leaves pale brown, yellowish brown; gray, greenish black with high nb–ta, Tourmaline leaves white; luster reads adamantine to submetallic on Rutile and vitreous on Tourmaline.
Often found alongside rutile
Minerals reported to co-occur with rutile. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- TiO₂
- Mohs hardness
- 6-6.5
- Density
- 4.23 g/cm³
- Streak
- Pale brown, yellowish brown; gray, greenish black with high Nb–Ta
- Luster
- Adamantine to submetallic
- Transparency
- Opaque, transparent in thin fragments
- Crystal system
- Tetragonal
- Crystal habit
- Acicular, massive, prismatic
- Cleavage
- {110}, good; {100}, moderate; {111}, in traces
- Rarity
- Common
- Uses
- Industrial, Collector, Gemstone, Lapidary
- Host rock
- A common high-temperature, high-pressure accessory mineral in igneous rocks, anorthosite, and granite pegmatite; in hydrothermally-altered rocks; in gneiss, schist, contact metamorphosed limestone; in clays, shales
Where rockhounds find rutile
41 mapped spotsClassic worldwide localities
- Magnet Cove, Hot Spring Co., Arkansas, USA
- Graves Mountain, Washington, Lincoln Co., Georgia, USA
- Stony Point, Alexander Co., North Carolina, USA
- Parkesburg, Chester Co., Pennsylvania, USA
- Cavradi, Tavetsch, Graübunden, and Lodrino, Tessin, Switzerland
- Pfitschtal, Trentino-Alto Adige, Italy
U.S. states with rutile
Each link opens a state-specific list of mapped rockhounding spots that produce rutile.
Field-hunting tip
Where it forms: A common high-temperature, high-pressure accessory mineral in igneous rocks, anorthosite, and granite pegmatite; in hydrothermally-altered rocks; in gneiss, schist, contact metamorphosed limestone; in clays, shales. If you start seeing anatase, brookite, hematite in float, you are in the right ground. Typical habit: acicular, massive, prismatic. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in North Carolina, Virginia, Utah. Start trip planning there.







