Pseudomorph Riebeckite

Pseudomorph Riebeckite From Ontario. Copyright © Rob Lavinsky

Riebeckite

Riebeckite is not a well known mineral although most people have probably seen stones that at one time were composed of riebeckite crystals. The typically dark blue mineral was named after a famous eighteenth century German explorer and minerologist, Emil Riebeck. Riebeckite is an important mineral for two main reasons: one for when it is there and one for when it isn't.

First, some forms of riebeckite are asbestiform and can be used as asbestos. Asbestos has many industrial uses despite some health risks and is made of different minerals all with a fibrous habit. Serpentine and tremolite form most of the asbestos that is used for industrial purposes. But riebeckite has a variety called "crocidolite" that is asbestiform in habit and is a significant percentage of the total tonage of asbestos that is mined annually. The largest deposit of crocidolite occurs in South Africa and is mined there in large quantities. A second deposit in Australia is significantly smaller but is still productive. Crocidolite is also known as "blue asbestos" and "riebeckite asbestos".

Secondly, crocidolite is often found pseudomorphed by quartz into an attractive ornamental stone. The stone is extremely popular as a semi-precious stone and is known by many trade names such as Tiger's Eye, Hawk's Eye, Falcon's Eye, etc. A pseudomorph is an atom by atom replacement of one mineral for another, without significant destruction of the original mineral's outward shape. The pseudomorphing of riebeckite's asbestos fibers does two things; it preserves the beauty of the fibers and their lustrous light effects and it produces a much more durable stone that is now, thanks to the silicification, suitable for carving and jewelry. Blue tiger's eye has preserved the original blue color of the riebeckite while the more common brown color is the result of some oxidation of the iron into limonite inclusions. Although it is improper to refer to tiger's eye as being a form of riebeckite because there is no riebeckite present in the stone, credit must be given to this mineral for the aid in producing this wonderfully beautiful ornamental stone.

The chemistry of riebeckite is odd in that it includes two different iron atoms. One is ferric (with a plus 3 charge) and one is ferrous (with a plus 2 charge). The ferrous iron occupies the same position as and substitutes with the plus 2 manganese because both ions are of nearly the same size. The formula is written the way it is to show the different iron ions.

Riebeckite is a part of several solid solution series. A solid solution series is where two or more elements can substitute for each other without changing the structure of the mineral. In the case of riebeckite, there exists two such series. The easiest to explain series exists with a mineral called magnesioriebeckite. Riebeckite is the ferrous iron rich member of the series and as the name implies, magnesioriebeckite is the magnesium rich member. Magnesioriebeckite formula, Na₂(Mg₃Fe³⁺₂)Si₈O₂₂(OH)₂, is nearly identical to riebeckite and so are the properties of the two minerals.

The other solid solution series is incomplete, meaning there are gaps in the percentages between the minerals. The other members of this series include one that is much more well know than magnesioriebeckite and one that is almost as obscure. The common mineral is glaucophane and its formula is [Na₂][Mg₃Al₂]Si₈O₂₂(OH)₂. Glaucophane is the magnesium and aluminum rich member and riebeckite is the ferrous and ferric iron rich member. The obscure mineral crossite is the intermediate member of the series. This series is really a series between two series; the Riebeckite Series and the Glaucophane Series. Glaucophane is really the same as magnesioriebeckite, except with aluminums, and riebeckite is the the same as glaucophane's own series partner ferroglaucophane, except with iron. The formulas in the table below are representing the pure state of each mineral for clearity.


Chemical Formula Na₂Si₈O₂₂(OH)₂
Color is usually dark blue to black.
Luster is vitreous or silky in fibrous forms.
Transparency: Crystals are translucent.
Crystal System is monoclinic; 2/m.
Crystal Habits include slender prismatic to acicular, often aggregated crystals, columnar, granular and fibrous, asbestiform masses. A moss-like aggregate habit has been described when found in some igneous rocks.
Cleavage: is perfect in two directions at 56 and 124 degree angles.
Fracture is splintery to uneven.
Hardness is 5 - 6.
Specific Gravity is approximately 3.2 - 3.4 (average to slightly above average).
Streak is blue-gray.
Other Characteristics: Weakly pleochroic and crystals are striated lengthwise.
Associated Minerals are nepheline, quartz, almandine, aegirine, feldspars, micas and hematite.
Notable Occurrences include Socotra Island, South Yemen; Transvaal, South Africa; Schirmeck, Germany; Langesund, Norway; Krivoi Rog, Ukraine; Hamersley Range in Western Australia; Scotland; Madagascar; Quincy, Massachusetts; St Peter's Dome, El Paso County, Colorado; California; Oregon and Cumberland Hill, Rhode Island, USA.
Best Field Indicators are crystal habit, color, streak, cleavage and hardness.


Locality: Atikokan, Hutchinson Township, Rainy River District, Ontario, Canada