Aventurine Feldspar Identification Guide
How to identify aventurine feldspar (sunstone) by its metallic copper-red schiller and feldspar cleavage, versus quartz aventurine and goldstone.
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What Aventurine Feldspar Looks Like
Aventurine feldspar is the mineralogical name for sunstone — a feldspar (oligoclase, or sometimes labradorite/orthoclase) containing tiny platy inclusions of hematite or copper that produce a warm, metallic aventurescence/schiller. The body color is often orange, reddish-brown, golden, or near-colorless, and tilting the stone reveals glittering coppery-red or golden flashes from the aligned platelets. Luster is vitreous; it is transparent to translucent, frequently with visible flat cleavage surfaces.
Step-by-Step Field ID Checklist
- Look for metallic spangles — tilt under bright light; aligned coppery/golden flashes (schiller) appear, often concentrated along certain planes.
- Find feldspar cleavage — look for two flat, reflective cleavage directions meeting at nearly 90 degrees; these flat planes distinguish feldspar from quartz.
- Note the warm body color — orange to reddish or golden in classic sunstone.
- Test hardness — about 6–6.5; a steel knife may just scratch it, and it will scratch glass weakly.
- Check transparency — typically more transparent than quartz aventurine.
Key Diagnostic Tests
- Hardness: 6–6.5 (feldspar), softer than quartz aventurine (7) — a useful separator.
- Cleavage: Two good cleavages at ~90 degrees — diagnostic of feldspar and absent in quartz.
- Aventurescence/schiller: Directional metallic flashes from oriented hematite or native copper platelets.
- Luster: Vitreous, pearly on cleavage planes.
- Streak: White.
- Density: ~2.62–2.65.
- Acid: No reaction.
Common Look-Alikes and How to Tell Them Apart
- Quartz aventurine: Quartz aventurine is harder (7), has no cleavage (conchoidal fracture only), and is usually green with green mica sparkle, whereas aventurine feldspar is softer, shows flat cleavage planes, and has warm coppery-red schiller.
- Goldstone (man-made glass): Uniform dense copper glitter, gas bubbles, no cleavage, softer (~5.5), and an unnaturally even sparkle. Aventurine feldspar has natural directional schiller and feldspar cleavage.
- Other feldspars (moonstone, labradorite): Moonstone shows a floating blue/white adularescence rather than metallic spangles; labradorite shows broad blue-green color flashes (labradorescence). Oregon sunstone (a labradorite) is a specific copper-bearing aventurine feldspar.
- Citrine/orange quartz: Transparent orange but lacks schiller spangles and has no cleavage.
Where Aventurine Feldspar Is Found
Classic aventurine feldspar (sunstone) comes from southern Norway (the original locality), India, Russia, Canada, and Tanzania. The famous Oregon Sunstone (USA) is a copper-bearing labradorite found in basalt flows in eastern Oregon and is renowned for its coppery schiller and color range. Aventurine feldspar typically occurs in igneous rocks such as basalt, syenite, and pegmatite.
Frequently asked questions
Is aventurine feldspar the same as sunstone?
Yes. Aventurine feldspar is the mineralogical term for sunstone — a feldspar containing platy hematite or copper inclusions that produce a warm metallic aventurescence or schiller.
How do I tell aventurine feldspar from quartz aventurine?
Aventurine feldspar is softer (6–6.5), shows two flat cleavage planes meeting near 90 degrees, and has warm coppery-red schiller. Quartz aventurine is harder (7), has no cleavage, and is usually green with green mica sparkle.
How can you tell aventurine feldspar from goldstone?
Goldstone is man-made glass with uniform dense copper glitter and gas bubbles, no cleavage, and is soft. Aventurine feldspar is a natural mineral with directional schiller and flat feldspar cleavage planes.
What causes the sparkle in aventurine feldspar?
Tiny aligned platelets of hematite or native copper within the feldspar reflect light, creating the metallic glittering effect known as aventurescence or schiller.
Aventurine Feldspar identified by the community
Recent Aventurine Feldspar specimens identified with Rock Identifier.