Coconino Lapidary Club




Fluorite, A Collectors Favorite


The rich, often “electric” rainbow colors of fluorite specimens from world-wide locations, the frequent appearance of different colors within regions, bound with the lattice planes within a crystal, and the sculptural appearances of stepped cubic and octahedral crystals, as shown in Figures 1-5, make fluorite a favorite among collectors. 

In this blog I’ll describe those structural properties of fluorite that are relevant to lapidary practices, and the sources of its’ color, (Figure 8).  I’ll describe how the regions, or zones, of different colors within a fluorite crystal develop. Also, because of their beauty, I am including a gallery of the beautiful fluorite specimens from around the world, that I found as I searched the web.

Figure 1. Stepped color-zoned fluorite crystals with boundaries parallel to the cubic faces of the crystals, Ozark-Mahoning Mione, Cave-in-Rock sub-District, Illlinois-Kentucky Fluorite District, Hardin County, Illinois [Ref 1]
Figure 2. Color-zoned fluorite on quartz with diagonal boundaries between the green and purple regions directed along dodecahedral planes in the fluorite crystals, Kudubis Farm 19, Karibib District, Erongo Region, Namibia [Ref 2].
Figure 3. Color-zoned fluorite with boundaries along diagonal dodecahedral planes within the cubo-octahedral crystal, White Water, Pigeon Rock Mountain, Mourne Mountains, County Down, Northern Ireland, UK [Ref 3].
Figure 4. Stepped fluorite cubic crystal, Spain [Ref 4]
Figure 5. Stepped fluorite cubo-octahedron, Shangbao Mine, Leiyang, County, Hengyang Prefecture, Hunan Province, China [Ref 5].

Properties of Fluorite [Ref 6]

Crystal Structure and Crystallography

The crystal lattice of fluorite exhibits cubic symmetry with the calcium and fluorine ions positioned within the basic unit cell, as shown in Figure 6. The four fluorine ions F-1are positioned centrally in the unit cell with the calcium ions Ca2+distributed at the corners and the center of each face of the unit cell. In this array, each calcium ion has two fluorine ions as neighbors. Imperfections in the lattice underlie the presence of color in fluorite, as described below.

The lattice structure of fluorite results in its crystallizing in the isometric crystal system. Fluorite typically exhibits the basic crystal forms of the cube, octahedron, and rhombic dodecahedron shown in Figures 7 & 8. Fluorite also exhibits ball-like or grape-like botryoidal forms, but only rarely. (Figure 9)

The Mohs hardness of Fluorite is 4 and it exhibits a perfect cleavage on octahedral planes and less-well developed cleavage or parting on dodecahedral planes. A cleavage octahedron is shown in Figure 12 [Ref 14]. The ready cleavage and softness of fluorite requires the lapidarist to minimize the generation of stresses during the cutting and polishing of a stone.

Figure 6. the crystal lattice of fluorite [Ref 6].

Typical Crystal forms of Fluorite

Typical crystal forms are the cube, oxctahedron, and dodecahedron; fluorite also occurs in botryoidal form.

Figure 7. Cubic crystals of fluorite, Las Causses, France [Ref 7].
Figure 8. Fluorite octahedrons on smoky quartz, Argentiere Massif,
Mont Blanc, Chamonix, France [Ref 8]
Figure 9. Cubic fluorite crystal with edges modified by dodecahedral faces, La Cabana, Asturias, Spain [Ref 9].
Figure 10. Botryoidal fluorite with calcite on quartz, Mahodari Quarry, Nasik, State of Maharashtra, India [Ref 10].

Twinning in Fluorite

Fluorite forms both penetration twins [Ref 11] and Spinel Twins [Ref 12] on octahedral planes, as shown in Figures 10 and 11.

Figure 11. Fluorite penetration twin, Lake George, Florissant, Colorado [Ref 13].
Figure12. Fluorite spinel Twin, Erongo, Namibia [Ref 12]. The octahedral face of one crystal is seen on the upper surface of the twin. The other face is hidden by the crystal. The outside trace of the twin plane is irregular [Ref 14].

Cleavage in Fluorite 

Figure 13. Fluorite cleavage octahedron. Cave-in-Rock District, Hardin County, Illinois [Ref 15]. The cleavage is perfect

Colors in Fluorite 

As shown in Figure 6, fluorite can occur in colorless form. Color, as described in Table I, is induced by the presence of an impurity ion, by nanoparticles of calcium metal, which scatter light preferentially according to size, or by inclusions of organic material such as bitumen.

Figure13. Color center in fluorite [Ref 22]. REE = rare earth element
 Ref 22. Page 27, Schematic of photochromic center color center–:

Color Zoning in Fluorite Crystals 

The establishment of discrete geometric zones of color in a fluorite crystal comes from the sequestration of a specific impurity, advancing along a crystallizing plane during sectorial growth [Ref 23].  A sketched example of sectorial growth in a fluorite crystal is shown in Figure 15, which is taken from Figure 4 of [Ref 24]. In the example, growth of octahedral and cubic planes are shown.  In Figure11, showing a fluorite specimen from Namibia, growth is seen to have proceeded along both dodecahedral and cubic planes. Growth proceeded along advancing dodecahedral planes, forming the green diamond-shaped region, and along cubic planes, forming the deep green corner regions.

Figure 14. Schematic of growth of sectors in a fluorite crystal. In generation of dodecahedral and cubic sectors as in Figure 14, growth proceeds towards the four cube corners and faces, forming four-sided pyramids within the crystal [Ref 23]. 
Figure 14. Color-zoned fluorite, Okorusu mine, Namibia [Ref 24].


In this Gallery I’ve included specimens from France, Morocco, Germany, Spain, and Mexico, which are not as well known to collectors as specimens from England the United States.

Ref 25.

Ref 26.

Ref 27.

Ref 28.

Ref 29.

Ref 30.

Ref 31.

Ref 32.

Ref 33.

Ref 34.