Cavansite

Ca(V4+O)(Si4O10) · 4H2O
IMA status
  • Approved
IMA symbol
Cav
Discovered
1967
IMA approved
1967
Also known as
  • IMA1967-019

History

The name is a small chemistry lesson folded into a word. Cavansite packs together the three elements at the heart of the mineral — calcium, vanadium, and silicate, the silicon-and-oxygen framework most rock minerals are built on.

It is a young mineral by the standards of the field. The first specimens turned up in 1967 near the Owyhee Dam, in Malheur County, Oregon, and three American researchers — Lloyd W. Staples, Howard T. Evans Jr., and James R. Lindsay — described it as a species new to science. The same Oregon work turned up a near-twin, pentagonite. The two are dimorphous: identical in chemistry but built into two different crystal shapes, like the same bricks stacked two ways.

For its first decades cavansite was a rarity known mainly from that Oregon ground. Then the basalt quarries around Pune, in western India, began yielding it in quantity. These quarries cut into the Deccan Traps. That name covers vast stacked sheets of ancient volcanic basalt that blanket much of west-central India. The mineral grew best inside the cavities left by old gas bubbles in that rock. Specimens from the Wagholi quarries near Pune carry deep, almost electric blue crystals. They are now the ones most collectors picture when they hear the name.

Industrial & practical applications

Cavansite earns its keep on a shelf, not in a factory. The mineral carries vanadium, a metal industry does want, so in principle it could be an ore source for it. In practice it is not treated as one. It is too scarce and too scattered to mine for the metal, and is not generally considered an ore mineral.

What it does have is colour. Its rich, bright blue crystals, often gathered into small rounded sprays, make it a sought-after collector's mineral — prized for display rather than for any material it yields.

Where it forms, where it's found

Geological setting

In brown tuff of late Miocene age and in basalt and breccia of Eocene age.

Basalt vesicular filling.

Type locality
Owyhee Dam
  1. Lake Owyhee State Park
  2. Malheur County
  3. Oregon
  4. USA

43.6248°, -117.2354°

13recorded occurrences
Source · OpenStreetMap

Physical

Hardness
123456789103 – 4/ 10 MOHS
  1. 1Talc
  2. 2Gypsum
  3. 3Calcite
  4. 4Fluorite
  5. 5Apatite
  6. 6Orthoclase
  7. 7Quartz
  8. 8Topaz
  9. 9Corundum
  10. 10Diamond
Lustre
Vitreous
Transparency
Transparent
Colour
Greenish-blue to blue
Tenacity
brittle
Cleavage
Distinct/Good

Good on (010)

Density
2.21 g/cm³

Optical

Optical type
Biaxial (+) · 2V measured = 52° · 2V calc = 58°
Refractive index
1.542 – 1.551
Surface relief
Moderate
Principal indices
nα 1.542 · nβ 1.544 · nγ 1.551
Pleochroism
Visible

X=Z= colorless Y= blue

Dispersion
r < v extreme. Dispersion opposite to that of pentagonite.
Extinction
Parallel. X = b; Y = a; Z = c.
Michel-Lévy diagramhighlighted lineδ = 0.0090
Attainable Michel-Lévy rangeΔ ∈ [0, t·δmax]90 nm1st order
Δ = 0Δmax
Thin-section mosaic70 grains · random 3D orientations
PPLpleochroism per grain
XPLindependent extinctions · rotate the stage
Interference simulatorsingle grain · PPL ↔ XPL
PPLpleochroism only · colour blends on rotation
XPLinterference colour · extinct every 90°
Retardation90 nm
Order1st order
XPL colour

Crystallography

Crystal system
Orthorhombic
Cell parameters
a = 9.792(2) Å · b = 13.644(3) Å · c = 9.629(2) Å
Ratio a:b:c
1 : 1.393 : 0.983
Z
4
Morphology

Prismatic crystals, spherulitic rosettes.

Twinning

No twinning observed.

Type-locality form

Blue radiating clusters up to 25 mm in diameter and as single crystals up to 0.2 mm long.

Comment

Space group Pcnm.

Crystal structure

Chemical composition

Constituent elements
Mass composition breakdown
ElementAtoms At. mass g/mol Mass g/molMass share
8OOxygenOxygen1515.999239.985
53.16%
14SiSiliconSilicon428.085112.340
24.89%
23VVanadiumVanadium150.94250.942
11.28%
20CaCalciumCalcium140.07840.078
8.88%
1HHydrogenHydrogen81.0088.064
1.79%
Total451.409100.00%

Mass share = atoms × atomic mass ÷ molar mass × 100

From IMA formula

Synonyms

  • IMA1967-019

In other languages

French
cavansite
German
Cavansit · IMA 1967-019
Spanish
Cavansita
Italian
Cavansite
Japanese
カバンシ石
Chinese
水矽釩鈣石
Traditional Chinese
水矽釩鈣石
Russian
кавансит

Classification

Strunz
10th ed.

9.EA.50

  • 9SilicatesClass
  • 9.EPhyllosilicatesDivision
  • 9.EASingle nets of tetrahedra with 4-, 5-, (6-), and 8-membered ringsGroup
  • 9.EA.50CavansiteSpecies
Dana
8th ed.

74.03.07.01

  • 74Phyllosilicates Modulated LayersClass
  • 74.03Modulated Layers with joined stripsType
  • 74.03.07V phyllosilicatesGroup
  • 74.03.07.01CavansiteSpecies
CIM

14.14.1

  • 14Silicates not Containing AluminumClass
  • 14.14Silicates of V and BiGroup
  • 14.14.1CavansiteSpecies

Group, growth & confusion

Commonly confused with
1 mineral

Literature, links & citation

Citations
  1. 1967Staples, L.W., Evans, H.T Jr., Lindsay, J.R. (1967) Cavansite, a new calcium vanadium silicate mineral (abstr.). Geological Society of America, Program Annual Meeting: 211-212.
  2. 1968Fleischer, Michael (1968) New Mineral Names. American Mineralogist, 53 (3-4) 507-511
  3. 1973Staples, Lloyd W., Evans, Howard T., Lindsay, and James R. (1973) Cavansite and pentagonite, new dimorphous calcium vanadium silicate minerals from Oregon. American Mineralogist, 58 (5-6) 405-411
  4. 1973Evans, Howard T., Jr. (1973) The crystal structures of cavansite and pentagonite. American Mineralogist, 58 (5-6) 412-424
  5. 1989Wilke, Hans-Jürgen; Schnorrer-Köhler, Günther; Bahle, Arvind (1989) Cavansit aus Indien [Cavansite from India]. Lapis, 14 (1). 39-41; 50
Cite this entry
@misc{mineral2026,
  author    = {Mineral Index editorial board},
  title     = {Cavansite — Mineral Index},
  year      = {2026},
  url       = {https://mineralindex.org/minerals/cavansite-921},
  note      = {Accessed 2026-05-11}
}