Kyanite
Al₂SiO₅
(Ca,Na)(Al,Si)₄O₈
Sunstone is a beautiful variety of plagioclase feldspar known for its internal metallic flashes — a phenomenon called ‘aventurescence.’ This sparkling effect looks like tiny golden glitters floating inside the stone. It is often found in warm shades of orange, gold, and red, though rarer green, blue, and watermelon varieties also exist. Sunstone is a geological cousin of moonstone and labradorite — all are feldspar minerals — but displays a completely different and uniquely captivating optical effect.
Sunstone is a variety of oligoclase or labradorite — both plagioclase feldspars — that contains oriented inclusions of metallic minerals that create the distinctive aventurescence effect. The mineral crystallizes in the triclinic system and forms as a primary igneous mineral in certain basalt flows and pegmatites.
The term “sunstone” encompasses several different geological varieties with the same visual effect but different mineralogy and geographic origins:
Oregon Sunstone (Labradorite with copper inclusions): The most geologically unique and commercially important variety. Found in the Rabbit Hills, Plush, and Sunstone Public Collection areas of southeastern Oregon (Lake County and Harney County), these stones are distinctive for several reasons. Unlike all other sunstones, Oregon Sunstone contains microscopic platelets of native copper as its inclusion type. These copper platelets form during the cooling of basaltic lava flows from the High Lava Plains of Oregon. The copper precipitates within the feldspar crystals as the lava cools, aligning parallel to the feldspar’s crystal planes.
Oregon Sunstone often occurs in very pale to intensely colored material — champagne, orange, salmon, red, green, and bicolor combinations. Stones with green color are extremely rare and highly valuable, as the green is caused by copper platelets of a specific orientation and concentration. Some Oregon Sunstones are completely clear and colorless without any aventurescence — these are still technically sunstone but lack the characteristic sparkle.
Scandinavian Sunstone (Oligoclase with hematite/goethite inclusions): Classic sunstone from Norway and southern Sweden contains tiny plate-like inclusions of hematite or goethite (iron oxides). The orange-gold color comes from both the iron oxide inclusions and their interaction with light. Norwegian sunstone from Tvedestrand is the historical type locality.
Indian Sunstone: Commercial material from Rajasthan, India, containing hematite or goethite inclusions. Often orange to brownish-orange.
Tanzania and other African sources: Smaller commercial deposits producing orange to red material with hematite inclusions.
Canada: Some localities in Ontario and British Columbia produce oligoclase with aventurescence.
Aventurescence — from the Italian “avventura” (chance or fortune, referring to its accidental discovery) — is a sparkling, metallic glitter visible inside certain minerals caused by light reflecting off tiny, flat metallic inclusions.
In sunstone, these inclusions are microscopic platelets (often hexagonal or rhomboidal in shape) of copper, hematite, or goethite that grew parallel to the feldspar’s crystal planes during the original igneous crystallization. Their flat, mirror-like surfaces all face in the same general direction within the crystal.
When light enters the stone at certain angles, it strikes these metallic platelets simultaneously and reflects back toward the viewer as a burst of shimmering, sparkling light. The effect is three-dimensional — the sparkles appear to float at different depths within the stone, creating the impression of a galaxy of tiny stars captured in solid form.
Several factors control the character of the aventurescence:
Inclusion size: Larger platelets produce bold, individual, distinctly visible flashes. Smaller platelets produce a finer, more diffuse, red-gold glow (schiller effect). The largest copper platelets in Oregon Sunstone can be visible to the naked eye as distinct bronze glints.
Inclusion density: More inclusions produce more sparkle, but very high density can make the stone appear darker and more opaque.
Inclusion color: Copper inclusions produce golden-yellow to orange flashes; hematite produces reddish-orange to reddish sparkle; goethite produces brownish-yellow tones.
Orientation: When the inclusion platelets are all perfectly parallel, the aventurescence is bold and directional — it appears only when the stone is at a certain angle to the light. When inclusions are slightly varied in orientation, the sparkle is broader and visible over a wider range of angles.
Sunstone shares the physical properties of plagioclase feldspar:
Hardness: 6 to 6.5 on the Mohs scale — adequate for most jewelry applications but requiring care for rings that may receive hard impacts.
Cleavage: Perfect in two directions (characteristic of all feldspars). This cleavage means sunstone can split along these planes if struck hard enough. Protective settings are advisable for valuable pieces.
Luster: Vitreous to pearly — polished sunstone has a bright, glassy surface luster overlaid by the internal aventurescence.
Transparency: Variable. Many Oregon Sunstones are highly transparent — gem-quality clear material with strong aventurescence is quite valuable. Indian and Norwegian material tends toward more translucent character.
Specific gravity: 2.62–2.72, consistent with plagioclase feldspar.
Refractive index: Approximately 1.537–1.547 (varies with composition from oligoclase to labradorite end-members).
Sunstone’s color palette is broader than many gemstone buyers expect:
Colorless to pale champagne: Oregon Sunstone without strong iron or copper coloration. Can still show strong aventurescence from copper platelets.
Yellow-gold to orange: The most common and classic sunstone color, from both Oregon copper inclusions and hematite/goethite elsewhere.
Salmon to peach: Warm, flattering mid-orange tones popular in jewelry.
Deep red-orange: Rich color from high copper density or strong hematite coloration.
Green (Oregon only): The rarest and most valuable Oregon Sunstone color. Green coloration results from a specific size and orientation of copper platelets that absorb certain wavelengths and create green by interference. Truly green Oregon Sunstone can command prices rivaling fine colored gemstones.
Watermelon or bicolor (Oregon): Spectacular stones showing green in the center grading to orange or red toward the edges, similar to watermelon tourmaline.
Schiller effect without visible sparkle: Very fine copper or hematite inclusions produce a warm glow rather than distinct sparkles — still called sunstone but a different visual character.
Sunstone has a rich history across multiple cultures, spanning indigenous traditions, Norse navigation mythology, and modern gem collecting.
Native American traditions in Oregon: The Paiute people of the Oregon High Desert lived near the Rabbit Hills sunstone deposits for centuries. According to Paiute tradition, sunstone was formed from the blood of a great warrior whose spirit entered the stones, giving them their reddish color and internal fire. Paiute people used sunstone in trade networks reaching across the American West and believed the stones carried protective power.
The Viking Sunstone Navigation Legend: One of the most fascinating historical controversies in geology and archaeology centers on the Norse saga references to “sólarsteinn” (sunstone) — a crystal supposedly used by Viking navigators to locate the position of the sun even on overcast days or after sunset.
The physical principle is sound: certain transparent crystals can polarize light differently depending on their orientation relative to the sun’s position, even when the sun is below the horizon or behind clouds. By rotating the crystal and observing where the polarization pattern changes, a navigator could determine the sun’s precise position.
Several minerals have been proposed as the historical sólarsteinn: Iceland Spar (transparent calcite), iolite (cordierite), and sunstone (oligoclase) are all candidates. A piece of Iceland Spar found in a 16th-century English shipwreck (the Alderney wreck, possibly associated with Elizabethan navigation) revived academic interest in the sunstone navigation hypothesis. Experimental studies have confirmed that skilled users can determine sun position using Iceland Spar to within approximately 1° — sufficient accuracy for ocean navigation.
Whether the Vikings used sunstone specifically or some other polarizing crystal remains unresolved, but the principle is scientifically validated and the cultural tradition is attested in saga literature.
Oregon State Gemstone: Oregon Sunstone was designated the official gemstone of Oregon in 1987. The Harney Lake area of southeast Oregon contains a Bureau of Land Management (BLM) public collecting site where visitors can dig for sunstones — one of the few places in the world where the public can collect a genuine precious gemstone from a natural deposit.
Sunstone value varies enormously depending on variety, color, and optical quality:
Oregon Sunstone commands the highest prices, especially for:
Pricing tiers for Oregon Sunstone (approximate):
Indian and Norwegian Sunstone: Generally much more affordable. Color and aventurescence intensity are the primary value drivers.
Orange, red, gold, green (with aventurescence)
Oregon Sunstone is a unique variety found only in the high deserts of Oregon, USA. Unlike other sunstones which contain hematite, Oregon Sunstone gets its glitter (schiller) from millions of microscopic copper platelets. It is the only sunstone that contains copper.
The glitter effect, known as aventurescence, is caused by light reflecting off tiny, flat mineral inclusions aligned within the stone. In most sunstone, these are hematite or goethite. The larger the inclusions, the more distinct the glitter; smaller inclusions create a reddish glow.
Sunstone has a hardness of 6 - 6.5 on the Mohs scale.
Sunstone is primarily found in United States (Oregon) - most famous source, Norway, India.
Sunstone typically occurs in orange, red, gold, green (with aventurescence).