Fluorapophyllite-(K)

KCa4Si8O20F · 8H2O
IMA status
  • Approved
  • Grandfathered
IMA symbol
Fapo-K
Discovered
1976
IMA approved
1976
Also known as
  • Apophyllite-(KF)
  • Fluorapophylliet-(K)
  • Fluorapophyllit
  • +1 more

History

Hold a clear crystal of this mineral over a flame and the surface peels in tiny silvery sheets. That party trick is the entire reason for its name.

In 1806 the French mineralogist René Just Haüy named the broader family apophyllite. He built the word from two Greek roots: apo, "off", and phyllon, "leaf". The name describes what happens when the crystal is heated. Water locked inside the structure escapes, and the mineral flakes apart along flat parallel sheets. A later Greek-derived form, apophyllízo, glosses the same idea — "it flakes off".

For most of the 19th and 20th centuries "apophyllite" referred to a single species. That changed once chemical analyses revealed real variation inside the structure. Two sites in the crystal proved swappable: potassium against sodium in one, fluorine against hydroxide in the other. In 1978 the American mineralogists Pete J. Dunn, Roland C. Rouse, and Julie A. Norberg formally recognised those variants. They proposed splitting apophyllite into a group of related species.

A nomenclature revision approved by the International Mineralogical Association in 2013 finalised the split. The old name was retired, and each end-member received its own species name with prefixes and suffixes describing its dominant chemistry. Fluorapophyllite-(K) — fluorine-dominant in one site, potassium-dominant in the other — is the most common of those end-members. Most specimens once labelled simply "apophyllite" turn out, on analysis, to be this one.

Industrial & practical applications

Fluorapophyllite-(K) has no industrial role. The mineral is too soft, too scattered, and too rare in concentrated deposits to interest any commodity producer. Its demand sits entirely with collectors and with the geologists who read it as a marker of basalt alteration.

The collector market is the larger of the two. The mineral forms large, well-developed crystals in many colours, and that combination is unusually photogenic for a non-gem species. The most wanted variation is the green one. It comes from the Deccan Traps of western India — the immense flood-basalt province that covers much of Maharashtra. Other prized localities include the Harz Mountains of Germany, Mont Saint-Hilaire in Canada, and Kongsberg in Norway. Classic specimens also come from Trentino in Italy, Belfast in Northern Ireland, the Faroe Islands, Kimberley in South Africa, and Guanajuato in Mexico.

For the field geologist, the mineral has a quieter but more practical use. It grows as a secondary mineral inside the gas bubbles — the vesicles — left in cooling basalt and other volcanic rocks. It is also structurally related to the zeolites, a family of porous aluminosilicate minerals that trap and release water. It tends to crystallise alongside them when warm groundwater circulates through the rock long after eruption. Finding it inside a vesicle is, in practice, a sign that the host basalt has been through that low-temperature alteration history.

Where it forms, where it's found

Geological setting

Secondary mineral in cavities in basalts, cavities in granite, in tactites, some hydrothermal veins.

295recorded occurrences
Source · OpenStreetMap

Physical

Hardness
123456789104.5 – 5/ 10 MOHS
  1. 1Talc
  2. 2Gypsum
  3. 3Calcite
  4. 4Fluorite
  5. 5Apatite
  6. 6Orthoclase
  7. 7Quartz
  8. 8Topaz
  9. 9Corundum
  10. 10Diamond
Transparency
Transparent · Translucent
Colour
Colourless · pale green · aquamarine · white · pink · yellow
Streak
White
Tenacity
brittle
Cleavage
Perfect

Perfect on (001) Imperfect on (110)

Fracture
Irregular/Uneven
Density
2.33 g/cm³

Optical

Optical type
Uniaxial (+)
Refractive index
1.53 – 1.538
Surface relief
Moderate
Principal indices
nω 1.53 – 1.536 · nε 1.532 – 1.538
Dispersion
High, may be anomalous
UV response
May fluoresce white or yellow
Michel-Lévy diagramhighlighted lineδ = 0.0020
Attainable Michel-Lévy rangeΔ ∈ [0, t·δmax]20 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°
Retardation20 nm
Order1st order
XPL colour

Crystallography

Crystal system
Tetragonal
Space group
#182
Cell parameters
a = 8.963(2) Å · c = 15.804(2) Å
Z
2
Morphology

Tabular to prismatic

Twinning

Rare on (111)

Crystal structure

Chemical composition

Constituent elements
Mass composition breakdown
ElementAtoms At. mass g/mol Mass g/molMass share
8OOxygenOxygen2815.999447.972
49.38%
14SiSiliconSilicon828.085224.680
24.77%
20CaCalciumCalcium440.078160.312
17.67%
19KPotassiumPotassium139.09839.098
4.31%
9FFluorineFluorine118.99818.998
2.09%
1HHydrogenHydrogen161.00816.128
1.78%
Total907.188100.00%

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

From IMA formula

Impurities
  • Al
  • Na

Synonyms

  • Apophyllite-(KF)
  • Fluorapophylliet-(K)
  • Fluorapophyllit
  • IMA1976-001

In other languages

French
fluorapophyllite-(K)
German
Apophyllit-(KF) · Fischaugenstein · Fluorapophyllit · Fluorapophyllit- · Fluorapophyllit-(K) · Ichthyophthalmit
Spanish
Fluorapofilita- · Fluorapofilita-(K)
Italian
apofillite-(KF) · Fluorapofillite- · fluorapofillite-(K)

Classification

Strunz
10th ed.

9.EA.15

  • 9SilicatesClass
  • 9.EPhyllosilicatesDivision
  • 9.EASingle nets of tetrahedra with 4-, 5-, (6-), and 8-membered ringsGroup
  • 9.EA.15Fluorapophyllite-(K)Species
Dana
8th ed.

72.03.01.01

  • 72Phyllosilicates Two-dimensional Infinite Sheets with Other Than Six-membered RingsClass
  • 72.03Two-Dimensional Infinite Sheets with Other Than Six-Membered Rings with 3-, 4-, or 5-membered rings and 8-membered ringsType
  • 72.03.01Apophyllite group (4- & 8-membered rings)Group
  • 72.03.01.01Fluorapophyllite-(K)Species
CIM

17.1.5

  • 17Silicates Containing other AnionsClass
  • 17.1Silicates with fluoride (not containing Al)Group
  • 17.1.5Fluorapophyllite-(K)Species

Group, growth & confusion

Commonly confused with
1 mineral

Literature, links & citation

Citations
  1. 1971Chao, George Y. (1971) The refinement of the crystal structure of apophyllite: II. Determination of the hydrogen positions by X-ray diffraction. American Mineralogist, 56 (5-6) 1234-1242
  2. 1975Kostov, I. (1975) Apophyllite morphology as an example of habit modification of planar crystals. Neues Jahrbuch für Mineralogie Abhandlungen: 123(2): 128-137.
  3. 1978Dunn, Pete J.; Rouse, Roland C.; Norberg, Julie A. (1978) Hydroxyapophyllite, a new mineral, and a redefinition of the apophyllite group. I. Description, occurrences, and nomenclature. American Mineralogist, 63 (1-2). 196-198
  4. 1978Rouse, Roland C., Peacor, Donald R., Dunn, Pete J. (1978) Hydroxyapophyllite, a new mineral, and a redefinition of the apophyllite group. II. Crystal structure. American Mineralogist, 63 (1-2). 196-202
  5. 1978Wilson, Wendell E., Dunn, Pete J. (1978) Nomenclature revisions in the apophyllite group: hydroxyapophyllite, apophyllite, fluorapophyllite. The Mineralogical Record, 9 (2) 95-98
Cite this entry
@misc{mineral2026,
  author    = {Mineral Index editorial board},
  title     = {Fluorapophyllite-(K) — Mineral Index},
  year      = {2026},
  url       = {https://mineralindex.org/minerals/fluorapophyllite-k-1573},
  note      = {Accessed 2026-05-11}
}