• Chemistry: (Na, Ca, Ce)2BeSi2(O, OH, F)7, Sodium Calcium Cerium Beryllium Silicate Hydroxide Fluoride.
  • Class: Silicates
  • Subclass: Sorosilicates
  • Group: Melilite - Fresnoite
  • Uses: Very minor source of cerium and as mineral specimens.
  • Specimens

Leucophanite is a rare beryllium silicate that was first discovered from the mines of Langesundsfjord district of Norway, a classic mineral locality filled with rare minerals. It was discovered early in the areas mining history and was one of the first minerals described from there in 1840. Of interest was the trace amounts of rare earth elements in its chemistry, especially cerium which substitutes for some calcium. Leucophanite is also found at Mont Saint-Hilaire, Quebec, Canada from where some of the best specimens are found. Another classic locality from where this mineral comes from is the Lovozero intrusion on the Kola Peninsula, Russia. All these locations have unusual rocks that are quite unique and are called agpaitic pegmatites.

Leucophanite forms nice crystals that belie their true symmetry. They appear to be tetragonal or even cubic forming rectangular box or cube shaped crystals. But their true symmetry is triclinic, pedion class which is the lowest symmetry possible in a three dimensional system. The only symmetry element is translational shift as it lacks any mirrors, rotations, or even a center. The symmetry is noted by a 1 which represents a one fold rotation (as in if you rotate the crystal one full 360 degree turn, it will look the same as when you started; overstating the obvious). Crystals from minerals that belong to this class can be fascinating with their complex non-symmetrical faces. Unfortunately leucophanite does not show its true symmetry but exhibits an impostor symmetry, and a rather ordinary one at that.

Leucophanite is named for the white flashes that are seen as a crystal is rotated. Leucophanite loosely translated from the Greek means "white appearing". There are a few similar sounding minerals such as leucophoenicite, leucophosphite, leucosphenite and even leucite. But leucophanite is very different from all of these. A synonm of leucophanite is "leucophane" which is not official but is still in limited use.


  • Color is white to yellowish, yellow and green.
  • Luster is vitreous.
  • Transparency: Specimens are translucent to transparent.
  • Crystal System is triclinic, 1.
  • Crystal Habits are pseudotetragonal and pseudocubic forming rectangular box or cube shaped crystals. Penetration twinning is common and forms flat square and elongated crystals. Aggregate rosettes are also seen.
  • Cleavage is perfect in one direction and fair in two others.
  • Hardness is 4.
  • Specific Gravity is approximately 3.0 (average)
  • Streak is white.
  • Associated Minerals include many rare and beautiful minerals such as aegirine, fluorite, rhodochrosite, serandite, albite, astrophyllite, natrolite, rhabdophane, analcime, ancylite, catapleiite, epididymite, microcline and behoite.
  • Notable Occurrence includes the type locality of Langesundsfjord district, Norway as well as Mont Saint-Hilaire, Quebec, Canada and Kola Peninsula, Russia.
  • Best Field Indicators are crystal habit, color, associations, locality and cleavage.
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LEUCOPHANITE specimen lcp-1
$ 75.00
Dims:1.9x1.5x1.5" (4.8x3.8x3.8 cm)
Wt: 1.8oz. (52g)
Mt. St. Hilaire, Quebec, Canada
This is an excellent triclinic crystal of leucophanite included by aegirine on a matrix of feldspar and aegirine. This crystal is tabular and nearly transparent. It measures 0.2" (0.5cm) across. The crystal appears almost orthorhombic until one closely examines the corners of the crystal to find additional faces. There is no damage to this specimen.
no photo
lcp-1 ($ 75.00)
Mt. St. Hilaire, Quebec, Canada
LEUCOPHANITE specimen lcp-2
$ 30.00
Dims: 1.12x0.71x0.66" (2.85x1.80x1.67cm)
Wt: 0.32oz (8.95g)
Saga quarry, Tvedalen, Norway
This specimen displays many green crystals of leucophanite in a colorless transparent to translucent host rock that also contains many black aegirine crystals. The best of the leucophanite crystals are transparent and a lovely dark olive-green, with a vitreous luster. The crystals are relatively long, with a rectangular cross section. Most of the sparkle on this specimen comes from the leucophanite. The aegirine looks relatively dull, and the host rock (which looks like quartz except for a few areas that look disturbingly like cleavage) is not very specular.
no photo
lcp-2 ($ 30.00)
Saga quarry, Tvedalen, Norway


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