Mica
X₂Y₄–₆Z₈O₂₀(OH,F)₄ (General Formula)
Ca(VO)Si₄O₁₀·4H₂O
Cavansite is one of the most visually explosive, incredibly rare, and structurally breathtaking collector’s minerals discovered in the 20th century. It is instantly recognizable by its spectacular, vibrant, neon-blue to deep ultramarine crystal aggregates that burst like tiny, perfect fireworks or fuzzy pom-poms against a stark background of white, sparkling zeolite crystals. It is a true marvel of geology, and its intense beauty belies an incredibly fragile, delicate structure that demands the utmost respect from those lucky enough to handle it.
The mineral was first officially discovered and described in 1967 by a team of American mineralogists (Lloyd Staples, Howard Evans, and James Lindsay) who found tiny, millimeter-sized blue crystals in Malheur County, Oregon. Struck by its unique chemistry, they named it “Cavansite,” a simple acronym derived from its primary elemental makeup: CAlcium, VANadium, and SIlica. However, it wasn’t until a massive, spectacular discovery in India decades later that Cavansite truly captured the attention of the global gem and mineral world.
Cavansite (Ca(VO)Si₄O₁₀·4H₂O) is a complex, hydrous calcium vanadium silicate. It is a secondary mineral that forms almost exclusively in a very specific, low-temperature hydrothermal environment: the vesicles (gas bubbles) and fractures of cooling basaltic lava flows.
Millions of years ago, as massive volcanic eruptions of basalt lava cooled, trapped gases created thousands of empty, spherical pockets within the solid rock. Later, relatively cool groundwater (around 50°C to 100°C), highly saturated with dissolved calcium, silica, and the rare metal vanadium, slowly percolated through these porous basalts.
When the chemical conditions were absolutely perfect, the water deposited these elements into the empty gas bubbles. Cavansite rarely crystallizes first; it almost always forms as brilliant blue, secondary “rosettes” growing directly on top of a bed of pre-existing, sparkling white zeolite minerals—most commonly stilbite, heulandite, or apophyllite—creating a spectacular, high-contrast natural display.
To see a high-quality piece of Cavansite on a white stilbite matrix is an unforgettable experience. Because its formula is dominated by vanadium (V⁴⁺), it is idiochromatic. The high concentration of this transition metal inherently gives the mineral an intense, uniform, brilliant, glowing blue or greenish-blue color.
Crystallizing in the orthorhombic system, Cavansite’s habit is legendary. It almost exclusively forms distinct, spherical, radiating aggregates of tiny, prismatic crystals. These clusters are universally known to collectors as “rosettes” or “puffs,” often measuring from a few millimeters to over an inch across.
It is an incredibly soft and fragile mineral, rating only 3 to 4 on the Mohs scale, meaning it can easily be scratched by a copper coin. Furthermore, it possesses good cleavage in one direction, making the tiny radiating needles highly susceptible to snapping, flaking, or crushing if handled improperly or subjected to pressure.
Because of its extreme fragility, softness, and radiating habit, Cavansite is never faceted for commercial jewelry. Its immense value lies entirely within the mineral specimen collector’s market.
The absolute finest, largest, most spectacular, brilliantly blue, and perfectly formed rosettes in the world come almost exclusively from a single location: a small group of basalt quarries (specifically the Wagholi Quarry) near the city of Pune in Maharashtra, India. The specimens extracted from this single volcanic complex in the late 20th century are legendary, commanding premium prices from museums and advanced collectors worldwide.
In the crystal healing community, Cavansite is considered a premier stone of intense revelation, profound psychic transition, and clear, joyful communication. Because of its vibrant blue color and striking, star-burst shape, it is powerfully connected to the throat and third eye chakras. Practitioners believe it provides a massive surge of high-frequency energy that clears the mind of confusion, anxiety, and rigid thinking. It is often used to foster a deep sense of confident, articulate self-expression, encouraging the user to quickly access deep, intuitive wisdom, overcome major life obstacles, and embrace sudden, positive spiritual changes with radiant optimism.
Brilliant blue, greenish-blue
Yes, exceptionally rare. While it was originally discovered in tiny amounts in Oregon in 1967, almost all of the world's supply of large, spectacular, brilliant blue Cavansite comes from a single, small group of basalt quarries near the village of Wagholi in Pune, India. Because of this single, isolated source, high-quality specimens are highly prized and expensive.
Unlike many minerals that are colored by tiny trace impurities, Cavansite is idiochromatic. Its intense, glowing, neon-blue to greenish-blue color is caused directly by its fundamental chemical composition—specifically, the high concentration of the transition metal vanadium (V⁴⁺) within its complex silicate crystal lattice.
No, but they are incredibly similar. They are dimorphs, meaning they share the exact same chemical formula (Ca(VO)Si₄O₁₀·4H₂O) but crystallize in slightly different structures based on the temperature of the water they formed in. Cavansite (forming at lower temperatures) typically grows as distinct, round "rosettes" or puffballs. Pentagonite (forming at higher temperatures) tends to grow as longer, spikier, more elongated radiating prisms. They are often found in the exact same quarry in India.
It is highly discouraged for daily wear. Cavansite has a hardness of only 3 to 4 on the Mohs scale, meaning it can be easily scratched by a copper coin or everyday dust. More importantly, it forms as delicate, radiating clusters of tiny needles. These rosettes will easily crush, flake, or snap off the matrix rock if bumped or handled roughly. It is strictly a display mineral for advanced collectors, though uncut rosettes are sometimes carefully set in highly protected pendants.
The name is a clever, literal description of its chemical composition. Coined in 1967 by the American mineralogists who discovered it in Oregon (Staples, Evans, and Lindsay), "Cavansite" is an acronym for its primary elements: **CA**lcium, **VAN**adium, and **SI**lica.