Mineral

Leucite

KAlSi₂O₆Lösit

The white mineral of potassium-rich volcanic lavas: cube-like crystals once mistaken for white garnet.

Also known as: Amphigène (French, Haüy) · White garnet (old name)

  • Popularly: Common stone
  • Everyday
Leucite crystal (Ariccia, Alban Hills, Italy)Photo: Giorgio Agostinelli · Public domain · Wikimedia Commons

In short

Leucite is a mineral made of potassium, aluminium, silicon and oxygen (KAlSi₂O₆). It belongs to the feldspathoids, feldspar-like minerals that are poorer in silica. It forms white or grey, twenty-four-faced crystals that resemble cubes, and is most often found in potassium-rich, silica-poor lavas. Its name comes from the Greek for “white”. It used to be called “white garnet” as well.

Photos

How does it form?

Leucite crystallises in potassium-rich, silica-poor lavas and near-surface rocks; according to the Handbook of Mineralogy it can make up these rocks almost entirely. Because it forms in a silica-poor setting, it is not found with quartz, and according to the 1911 Britannica it is unstable in pre-Tertiary rocks, turning into secondary minerals. Above about 500 °C leucite behaves as a cubic (isotropic) mineral; as the lava cools, the crystal structure changes in two steps to tetragonal, which produces its many fine twins (Handbook of Mineralogy).

What is it used for?

  • Dentistry: Some glass-ceramics used for dental prostheses contain leucite crystals made artificially. In this “leucite-reinforced glass-ceramic” the crystals make up 35–45% of the volume and measure 1–5 microns; it is mainly used for front-tooth crowns, inlays and onlays (Ritzberger et al., 2010).
  • Geology: Leucite is a sign that the rock came from a magma very rich in potassium and poor in silica; geologists recognise such magmas by leucite-bearing lavas (leucitites).
  • History of chemistry: Leucite played a part in the discovery that potassium is present in minerals.
  • Collecting: Large, sharp crystals appeal to mineral collectors.

In Türkiye

Leucite is known in Türkiye in the ultrapotassic volcanic rocks around Afyonkarahisar. A master’s thesis completed at Pamukkale University in 2020 reports trachyte, trachyandesite, leucitite (leucite-bearing lava), phonolite, lamproite and basaltic lava and dykes in the Haydarlı area south of Afyonkarahisar, and says most of the volcanic rocks are ultrapotassic and high-potassium alkaline. For the large sanidine crystals in trachytes of the same region, see the sanidine page.

What determines its value?

Leucite is mainly a rock-forming mineral and has no price of its own. Collectors look for large, sharp, well-formed crystals, specimens where the whole crystal shows clearly in the rock, and those from well-known places such as the Alban Hills in Italy or Vesuvius. Leucite in rock is often altered and dull; clean, lustrous crystals are rare.

This information is educational, not buying, selling or investment advice. Value varies enormously with quality and treatment.

How to recognise it

  1. 1

    In the rock it appears as white or grey, round, twenty-four-faced (trapezohedral) crystals; these look like cubes but are not really cubic (pseudocubic, tetragonal). Crystals can reach 9 cm.

  2. 2

    Its hardness is 5.5–6; a steel knife scratches it only with difficulty. Its cleavage is very poor and it breaks along curved, shell-like surfaces.

  3. 3

    Crystals are usually covered in very fine twin lines, which can be seen with a microscope or hand lens.

  4. 4

    In potassium-rich, silica-poor rocks such as lavas it occurs with potassium feldspar, nepheline and analcime; it is not seen in the same rock as quartz.

Fakes and imitations

What shops usually don’t tell you:

  • Leucite is most often confused with analcime, nepheline and garnet; its crystal form is very like some of these. A microscope or chemical analysis is needed for a certain identification.

Myths and misconceptions

  • MythLeucite is a white garnet.

    FactLeucite used to be called “white garnet” because its crystals resemble the twenty-four-faced crystals of garnet (1911 Britannica). But leucite is a feldspathoid; it has nothing to do with garnet, and its structure, composition and host rocks are different.

  • MythLeucite occurs only at Vesuvius.

    FactVesuvius is where leucite is best known, but the Handbook of Mineralogy says the mineral occurs at many places in the world: other volcanoes in Italy, the Eifel in Germany, Wyoming, Montana and Arkansas in the USA, Uganda, Tanzania and Australia. Leucite-bearing rocks are known in Türkiye too.

What is it believed to be good for?

This section reports beliefs; it is not health information. There is no scientific evidence for these claims and no stone replaces medical treatment.

The meanings people give this stone, and who holds them:

  • Crystal-therapy websites claim that leucite helps with insomnia, headaches and immune deficiency, and speeds recovery from illness or injury.
  • The same sites say leucite strengthens confidence and relationships, stops stress from clouding judgement, and is a suitable stone for the “crown chakra”.

What science says

No study supports these claims. Leucite is an ordinary mineral of potassium-rich lavas, and no effect of a rock mineral on the body or on relationships is known. Lasting sleeplessness, headaches or immune problems call for a doctor.

Did you know?

Its name comes from the Greek for “white” and was first suggested by A. G. Werner in 1791. Early observers called it “white garnet” because of its look; another name used by French mineralogists is “amphigène”.

When leucite crystals are heated above about 500 °C they become optically isotropic (they behave like cubic crystals in light) and the fine twin lines on their faces disappear; these lines form as the crystal structure changes while lava cools.

The chemist M. H. Klaproth found potassium in leucite and lepidolite; L. N. Vauquelin then reasoned that potassium might be present in many other minerals too, and in 1797 showed that alum is a double salt.

The lavas of Vesuvius and Monte Somma in Italy are classic examples of the leucite-bearing rocks called “leucite tephrite” and “leucite basanite” (1911 Britannica).

Where is it found?

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  • Mount Vesuvius and Monte Somma, Campania, Italy · Historic sourceThe place best known for leucite in its lavas; the 1911 Britannica takes the Vesuvius lavas as an example of leucite rocks
  • Alban Hills (Ariccia, Frascati, Villa Senni), Lazio, Italy · Known localityLarge, well-formed leucite crystals; crystals of 2.5 cm are known from Ariccia
  • Roccamonfina, Campania, Italy · Known localityA volcano named by the Handbook of Mineralogy in Italy
  • Vulcano, Aeolian (Lipari) Islands, Italy · Known localityA locality named by the Handbook of Mineralogy
  • Laacher See area, Eifel, Germany · Known localityThe German locality named by the Handbook of Mineralogy
  • Leucite Hills, Sweetwater County, Wyoming, USA · Known localityThe Wyoming locality named by the Handbook of Mineralogy
  • Bears Paw Mountains, Hill County, Montana, USA · Known localityThe Montana locality named by the Handbook of Mineralogy
  • Magnet Cove, Arkansas, USA · Known localityThe Arkansas locality named by the Handbook of Mineralogy
  • Rwenzori Mountains area, Uganda · Known localityThe Handbook of Mineralogy names the Ruwenzori area of Uganda
  • Haydarlı area, Dinar, Afyonkarahisar, Türkiye · Known localityUltrapotassic volcanic rocks include leucitites, leucite-rich lavas; described in a master’s thesis

Locations are approximate to protect sites. Red dots mark places in Türkiye. Open in the big map →

Frequently asked questions

What is leucite?

Leucite is a mineral made of potassium, aluminium, silicon and oxygen (KAlSi₂O₆). It belongs to the feldspathoids, feldspar-like minerals that are poorer in silica. It forms white or grey, twenty-four-faced crystals that resemble cubes, and is most often found in potassium-rich, silica-poor lavas. Its name comes from the Greek for “white”. It used to be called “white garnet” as well.

What is leucite used for?

Dentistry: Some glass-ceramics used for dental prostheses contain leucite crystals made artificially. In this “leucite-reinforced glass-ceramic” the crystals make up 35–45% of the volume and measure 1–5 microns; it is mainly used for front-tooth crowns, inlays and onlays (Ritzberger et al., 2010). Geology: Leucite is a sign that the rock came from a magma very rich in potassium and poor in silica; geologists recognise such magmas by leucite-bearing lavas (leucitites). History of chemistry: Leucite played a part in the discovery that potassium is present in minerals.

How hard is leucite?

It has a hardness of 5.5–6 on the Mohs scale. It can scratch glass; a steel knife scratches it only with difficulty. Its specific gravity is 2.45–2.5 g/cm³.

Where is leucite found?

Its best-known localities: Mount Vesuvius and Monte Somma, Campania, Italy; Alban Hills (Ariccia, Frascati, Villa Senni), Lazio, Italy; Roccamonfina, Campania, Italy; Vulcano, Aeolian (Lipari) Islands, Italy; Laacher See area, Eifel, Germany.

Where is leucite found in Türkiye?

Known localities in Türkiye: Haydarlı area, Dinar, Afyonkarahisar, Türkiye.

How can you tell if leucite is real?

In the rock it appears as white or grey, round, twenty-four-faced (trapezohedral) crystals; these look like cubes but are not really cubic (pseudocubic, tetragonal). Crystals can reach 9 cm. Its hardness is 5.5–6; a steel knife scratches it only with difficulty. Its cleavage is very poor and it breaks along curved, shell-like surfaces. Crystals are usually covered in very fine twin lines, which can be seen with a microscope or hand lens. Leucite is most often confused with analcime, nepheline and garnet; its crystal form is very like some of these. A microscope or chemical analysis is needed for a certain identification.

Is leucite valuable?

On the “street to diamond” value ladder it sits on step 3 of nine: Building and industrial stone. Leucite is mainly a rock-forming mineral and has no price of its own. Collectors look for large, sharp, well-formed crystals, specimens where the whole crystal shows clearly in the rock, and those from well-known places such as the Alban Hills in Italy or Vesuvius. Leucite in rock is often altered and dull; clean, lustrous crystals are rare.

What is leucite good for?

Crystal-therapy websites claim that leucite helps with insomnia, headaches and immune deficiency, and speeds recovery from illness or injury. The same sites say leucite strengthens confidence and relationships, stops stress from clouding judgement, and is a suitable stone for the “crown chakra”. No study supports these claims. Leucite is an ordinary mineral of potassium-rich lavas, and no effect of a rock mineral on the body or on relationships is known. Lasting sleeplessness, headaches or immune problems call for a doctor. This section reports beliefs; it is not health information. There is no scientific evidence for these claims and no stone replaces medical treatment.

Sources

  1. Leucite · Wikipedia
  2. Handbook of Mineralogy: Leucite · Mineralogical Society of America
  3. Leucite · Webmineral
  4. Leucite · Encyclopaedia Britannica, 11th edition (Wikisource), 1911
  5. Alum · Encyclopaedia Britannica, 11th edition (Wikisource), 1911
  6. Properties and Clinical Application of Three Types of Dental Glass-Ceramics and Ceramics for CAD-CAM Technologies (Ritzberger et al.), Materials 3 · MDPI, 2010
  7. Haydarlı bölgesi (Afyonkarahisar güneyi) volkanik kayaçların mineralojik petrografik ve jeokimyasal özellikleri (E. Ercen, yüksek lisans tezi) · Pamukkale Üniversitesi, 2020
  8. Haydarlı, Dinar · Wikipedia
  9. Alban Hills · Wikipedia
  10. Roccamonfina · Wikipedia
  11. Vulcano · Wikipedia
  12. Mount Vesuvius · Wikipedia
  13. Laacher See · Wikipedia
  14. Leucite Hills · Wikipedia
  15. Bears Paw Mountains · Wikipedia
  16. Magnet Cove, Arkansas · Wikipedia
  17. Rwenzori Mountains · Wikipedia

External links

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