Arkose is a sedimentary rock characterized by a high content of feldspar, typically exceeding 25 percent of its clastic components. It often forms from the rapid weathering and erosion of granitic terrain, leading to poorly sorted, angular grains in a matrix of quartz and clay. It is easily identified by its coarse, grainy texture and often pinkish or reddish coloration due to the high feldspar content.
Is this arkose?
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 arkose with a known reference. Arkose sits at Mohs 6-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Arkose leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Arkose typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: pink, gray, tan, reddish.
- 5Look at form & habitTypical habit: clastic.
Often confused with
Arkose vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside arkose
Minerals reported to co-occur with arkose. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 6-7
- Density
- 2.6-2.7 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Clastic
- Cleavage
- None
- Rarity
- Common
- Uses
- Construction, Ornamental
- Host rock
- Sedimentary Basin
- Typical price
- $1-20 per specimen
Where rockhounds find arkose
Classic worldwide localities
- Scotland
- USA (Colorado)
- France
- Germany
Field-hunting tip
Look in sedimentary basin country — that is the host setting where arkose typically forms. If you start seeing quartz, feldspar, mica in float, you are in the right ground. Field specimens usually show a clastic habit, so train your eye for that shape before scanning the outcrop.





