To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.

From Wikipedia, the free encyclopedia

CategoryTectosilicate, feldspathoid
(repeating unit)
Strunz classification9.FA.05
Crystal systemHexagonal
Crystal classPyramidal (6)
H-M Symbol: (6)
Space groupP63
Formula mass146.08 g/mol
ColorWhite, Gray, Brown, Brownish gray, Reddish white
Crystal habitMassive granular to prismatic
TwinningOn [1010], [3365], and [1122]
Cleavage[1010] Poor
Mohs scale hardness6
LusterVitreous – greasy
Specific gravity2.55 – 2.65, average = 2.59
Optical propertiesUniaxial (-)
Refractive indexnω = 1.529 – 1.546 nε = 1.526 – 1.542
Birefringenceδ = 0.003 – 0.004
Other characteristicsnon-radioactive, non-magnetic, non-fluorescent

Nepheline, also called nephelite (from Greek: νεφέλη, "cloud"), is a rock forming mineral in the feldspathoid group: a silica-undersaturated aluminosilicate, Na3KAl4Si4O16, that occurs in intrusive and volcanic rocks with low silica, and in their associated pegmatites. It is used in glass and ceramic manufacturing and other industries, and has been investigated as an ore of aluminium.

Description and properties

Grayish-white nepheline crystals with dark schorlomite from Bou-Agrao Mt., Tamazeght complex, High Atlas Mts, Morocco (size: 6.0 x 4.4 x 3.8 cm)
Grayish-white nepheline crystals with dark schorlomite from Bou-Agrao Mt., Tamazeght complex, High Atlas Mts, Morocco (size: 6.0 x 4.4 x 3.8 cm)

Nepheline crystals are rare and belong to the hexagonal system, usually having the form of a short, six-sided prism terminated by the basal plane.[4] The crystals appear to have more symmetry than they actually possess,[5] but unsymmetrical etched figures produced artificially on the prism faces indicate that the crystals are hemimorphic and tetartohedral, the only element of symmetry being a polar hexad axis.[6] It is found in compact, granular aggregates, and can be white, yellow, gray, green, or reddish. The hardness is 5.5 – 6, and the specific gravity 2.60 – 2.65. It is often translucent with a greasy luster.[4]

The low index of refraction and the feeble double refraction in nepheline are nearly the same as in quartz; but since in nepheline the sign of the double refraction is negative, while in quartz it is positive, the two minerals are readily distinguished under the microscope.[4] An important determinative character of nepheline is the ease with which it is decomposed by hydrochloric acid, with separation of gelatinous silica (which may be readily stained by coloring matters) and cubes of salt.[7] For this reason, a clear crystal of nepheline becomes cloudy when immersed in acid.[4]

The mineral is prone to alteration to zeolites (especially natrolite), sodalite, kaolin, or compact muscovite. [7][8]

Structure and composition

The aluminosilicate backbone of nepheline has a fairly open structure of interlocked six-member rings. This resembles the structure of tridymite, with aluminum substituting for every other silicon atom. This structure produces one nearly hexagonal interstitial site and three irregular interstitial sites per unit cell. In ideal nepheline, the hexagonal sites are occupied by potassium ions and the irregular sites by smaller sodium ions, yielding an atomic ratio of sodium to potassium of (3:1). This corresponds to an ideal weight percentage of K2O of 8.1% The range of compositions seen in natural nepheline is 3% to 12% K2O.[9] Small amounts of calcium may be present as well.[8]

At elevated temperature, nepheline forms a complete solid solution series with kalsilite, KAlSiO4. At temperatures below about 1,000 °C (1,830 °F), there is a wide miscibility gap between nepheline and kalsilite, similar to the miscibility gap between microcline and albite. A composition falling in this gap will experience exsolution as it cools, where nepheline and kalsilite separate into separate microscopic layers (lamellae).[4]


Nephelinite is a rock-forming mineral found in silica-poor igneous rocks. These include nepheline syenite, foidite, and phonolite. It is often found along with leucite, sodalite, potassium feldspars, and sodium-rich plagioclase, amphiboles, or pyroxenes, but almost never in association with quartz.[8] Notable outcrops of nepheline-bearing rocks are found on the Kola Peninsula; in Norway and South Africa; and at Litchfield, Maine; Magnet Cove, Arkansas; and Beemerville, New Jersey, in the United States. Syenites found near Bancroft, Ontario contain large deposits of high-purity nepheline.[10]

Elaeolite (a name given by M. H. Klaproth 1809, from Greek words for oil [ἔλαίον] and stone [λίθος]; German: Fettstein)[7] is a massive form of translucent nepheline with a darker color and greasy luster.[11]


Because of its high alumina content, iron-free nepheline is valued for use in glass manufacturing in place of feldspar. Most of the nepheline used for this purpose comes from Ontario. Nepheline produced as a byproduct of apatite mining in the Kola Peninsula has found uses in ceramics, leather, rubber, textiles, wood, and the oil industry.[10] It can be used as a filler in paints, plastics, and foam rubber, and has been investigated as an alternative to bauxite for aluminium manufacturing.[8]


  1. ^ Webmineral data
  2. ^ Mindat
  3. ^ Handbook of Mineralogy
  4. ^ a b c d e Klein, Cornelis; Hurlbut, Cornelius S., Jr. (1993). Manual of mineralogy : (after James D. Dana) (21st ed.). New York: Wiley. pp. 546–547. ISBN 047157452X.
  5. ^ Nesse, William D. (2000). Introduction to mineralogy. New York: Oxford University Press. p. 35. ISBN 9780195106916.
  6. ^ Borchardt-Ott, Walter (1995). Crystallography (2nd ed.). Berlin: Springer. p. 159. ISBN 3540594787.
  7. ^ a b c Spencer, Leonard James (1911). "Nepheline" . In Chisholm, Hugh (ed.). Encyclopædia Britannica. 19 (11th ed.). Cambridge University Press. p. 383.
  8. ^ a b c d Nesse 2000, p. 226.
  9. ^ Klein & Hurlbut 1993, pp. 544-545.
  10. ^ a b Klein & Hurlbut 1993, p. 547.
  11. ^ "eleolite". Dictionary of Gems and Gemology: 298. 2009. doi:10.1007/978-3-540-72816-0_7337. ISBN 978-3-540-72795-8.

External links

This page was last edited on 3 January 2021, at 18:41
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.