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THE FELDSPAR GROUP

The Feldspar group of minerals (calcium, sodium, or potassium aluminum silicates) is the most abundant building block in the Earth’s crust. It is commonly found in granite, pegmatite, & other igneous rocks. Clay (shale & slate) is formed from decomposed Feldspar.

Like the Garnet group, the Feldspar group, also, splits into two distinct sub-groups:

The Sodium Potassium “Alkali” Feldspar – (Sodium/Potassium Aluminum Silicates).

Orthoclase
Sanidine
Adularia
Microcline (Amazonite)


The Sodium Calcium “Plagioclase” Feldspar – (Sodium/Calcium Aluminum Silicates).

Oligoclase
Sunstone
Peristerite - Labradorite
Bytownite

Andesine
Anorthite

Between the two sub-groups is Albite – (Sodium Aluminum Silicate).

The varieties in each subgroup are caused by the percentage of (Alkali Feldspar) Sodium & Potassium ions, or (Plagioclase Feldspar) Sodium & Calcium ions, within the mineral’s molecules. Also, it is common to have two different varieties of Feldspar intertwined in a single crystal. This intertwining of varieties can produce the visual effects we see in Feldspar gemstones.

All Feldspar Gems share the following characteristics:
Mohs’ hardness: 6~6 ½ Crystal system: Prismatic & Tabular
Cleavage: Good to poor Fracture: Conchoidal.
Transparency: Transparent to translucent, opaque. Luster: Glassy, pearly

Listed below, are the major varieties of Gem Feldspars, along with their specific descriptions and histories.

The Sodium Potassium “Alkali” Feldspars – (Sodium/Potassium Aluminum Silicates).

Adularia – Moonstone
Moonstone got its’ name from the “moon like’, shimmering white to blue sheen that flashes across its’ surface. This gemstone has been valued since, at least, the 14th century BC when the Egyptian pharaohs wore Moonstones as protective amulets.

Moonstones are found in a variety of pale shades from beige, green, peach, brown, and white. Uncut, these gemstones can be rather dull, but when cut by a master cutter, who, before cutting, aligns the crystal axis exactly at the zenith of the stone, produces a wonderful cabochon that shows off the Moonstones’ exciting sheen (adularescence). Moonstones’ adularescence is caused by light being refracted and scattered when it hits the microscopic lamellar structures (an intertwining of two different forms of Feldspar) within the crystal. “Cats’ Eye” and multi-rayed “star” Moonstones are found in India. The wonderful “Rainbow” Moonstone, with its’ blue sheen comes from Sri Lanka. Moonstones’ classic discovery point is in the Adula massif in the Swiss Alps. Adula is the origin of “Adularia” and “adularescence”. Other deposits are found in Brazil, Myanmar, Australia, and North America. In the Los Angeles (California) area, I believe that the beach suburb of Redondo Beach was originally called “Moonstone Beach” because (before the beach was artificially covered with sand) there was an abundance of moonstones along the pebble-strewn seashore. This is also true for a few other California beaches.

Historically, the gemstone Moonstone has been associated with the Moon and love. Currently, Moonstone is associated with the month of June (the wedding month). It is said that prosperity and good fortune are promised to those born in this month. Throughout the world, Moonstone is the birthstone for June, but here in the USA we also add Pearls and Alexandrite as Junes’ birthstone. Many cultures claim Moonstone to have mystical and magical powers. In India, it is a bringer of sweet and beautiful dreams. To Arabs, it is a symbol of fertility. In the USA, Moonstones are the official state stones for the states of Florida and New York.

In general, Moonstone is cut into cabochons, but it is also cut into cameos, spheres, and beads. A century ago Moonstones were very popular, in particular, when the famous French Master Goldsmith, Rene Lalique and his buddies used the gem, extensively, in their jewelry. Moonstones, in particular the Rainbow Moonstone with its’ blue flash, are seeing a renaissance of popularity.

I told you about its’ most famous member, Moonstone. I find it interesting, that while investigating Moonstone, I have found many conflicting statements as to which form(s) of Feldspar are included. At this point, I have determined the soft pastel Moonstones to be Adularia and Sanidine, and the “Rainbow Moonstone” to be Oligoclase (“Plagioclase” subgroup).

As a reminder, lets’ review these two Feldspar sub-groups.

The Sodium Potassium “Alkali” Feldspar – (Sodium/Potassium Aluminum Silicates).
Orthoclase
Sanidine (Moonstone)
Adularia (Moonstone)
Microcline (Amazonite)


The Sodium Calcium “Plagioclase” Feldspar – (Sodium/Calcium Aluminum Silicates).
Oligoclase (Rainbow Moonstone)
Sunstone
Peristerite – (Labradorite)
Bytownite
Andesine
Anorthite

Between the two sub-groups is Albite – (Sodium Aluminum Silicate).

The next important gem in the Sodium Potassium “Alkali” Feldspar sub-group is Microcline. Amazonite is a form of Microcline Feldspar.

Although Microcline Feldspar is found in the following colors; colorless, white, yellowish, pinkish, and green, only the light to dark green variety is considered to be Amazonite. There seem to be two varieties of Amazonite. In one, the color is a mottled soft blue-green to pale blue. The other, “Russian Amazonite” (also found in other parts of the world), is a deeper green and can have green or white striations.

The stories behind the name Amazonite vary. Some references claim the name is ancient and the gem was supposedly connected with the ancient female warriors (Amazons) of Mediterranean mythologies. Other references claim the gem was named for the Amazon River, a place where Amazonite was found. I could not find a definitive answer.

Historically, the deep green “Russian” Amazonite has been used, throughout the Middle East and Asia Minor, as beads and amulets and for décor, for thousands of years. I’ve seen beautiful green Amazonite antiquities and beads from ancient Egypt and Asia Minor that are over 5,000 years old. Currently, in Morocco and North Africa, this same deep green gemstone (can be striated) is called “Green Stone”, and it is cherished in the same way that Turquoise is cherished by the American Indians.

The soft green-blue form of Amazonite is said to be a “soothing stone”, and believe it or not, it is, also, claimed to wake up lazy teenagers and give them energy. The deeper green “Russian Amazonite” is said to be a “stone of courage”.

Amazonite is found in Colorado (USA), Russia, Brazil, East Africa, Madagascar, etc.

Another gem Feldspar in this subgroup is Orthoclase. Although Adularia (Moonstone) is a form of Orthoclase, when this Champaign-colored Feldspar gem is clear (rare), it is faceted and used in jewelry or held in rare gem collections.

Orthoclase is found in: Twentynine Palms, CA (USA) [“well formed crystals & twin crystals up to 200mm across”]; Elba, Italy; Czech Republic; Poland; Itrongay, Madagascar [“Yellow gemmy crystals up to 70mm across”]; Black Hills, South Dakota (USA) [“Gigantic crystals up to tens of meters long”]; Germany; Switzerland; Sri Lanka.

The last gem in this subgroup is smokey-brown Sanidine. Like Orthoclase, opaque gem Sanidine can be found as a Moonstone, and when clear, this gem is faceted for jewelry and rare gem collections.

Sanindine is found in: Germany [“Well formed crystals…up to 400mm in size”]; France; British Columbia, Canada; Bulgaria.

Let us explore the Gems in the Sodium/Calcium “Plagioclase” Feldspar sub-group. The minerals in this sub-group are similar and primarily differentiated by the percentage of Sodium vs. Calcium in their molecules. Most of the gemstones in this sub-group are known for their optical phenomena, and this is produced by internal light interference caused by the intertwining of two, or more, related feldspar minerals in their crystal lattice. Because of this, I will mention each of the minerals in this sub-group, and go in depth in describing the gemstones.

Below is a listing of the different minerals in the “Plagioclase” sub-group. They are listed in the order of their Sodium/Calcium percentages.

The Sodium Calcium “Plagioclase” Feldspar sub-group– (Sodium/Calcium Aluminum Silicates).
Oligoclase (Rainbow Moonstone)
Andesine
Peristerite – (Labradorite)
Bytownite
Anorthite
Sunstone
Between the two sub-groups is Albite – (Sodium Aluminum Silicate).

The first mineral in this sub-group is Oligoclase. Oligoclase is second, only, to Albite in its’ high percentage of sodium vs. calcium (90-70% sodium to 10-30% calcium). As a gemstone it has three different forms:

1) Gem Oligoclase - A clear, colorless to yellow crystal that is usually cut into a faceted gemstone. Although these cut gems can be used in jewelry, they are primarily kept in gemstone collections. Gem Oligoclase is found in the Ural Mtns, Russia

2) Rainbow Moonstone – aka, Oligoclase Moonstone. This transparent to translucent white gem with a blue shimmer floating across its’ surface is one of the most popular forms of Moonstone. The blue, moonlike shimmer is created by the gems’ scale like internal structure that causes light rays entering the stone to refract and scatter into a blue shimmer

A century ago, during the Art Nouveau period, the French jewelry artist, Rene Lalique and his contemporaries, would feature Rainbow Moonstone in their wonderful creations. Today, these pieces of classic jewelry are primarily found in museums and private collections. The classic source is Sri Lanka, but it is also found in the USA; Brazil; Australia; Myanmar; Madagascar

3) Sunstone – aka, Aventurine Feldspar. This opaque to translucent to transparent, glitter filled, Oligoclase gem can have a reddish or golden shimmer floating across its’ surface. Small, plate like, inclusions of hematite or goethite produce the colorful “glitter” that can define Sunstone. Light interference, caused by these inclusions, produces the glitter colors – red and gold are common, green and blue are more rare. Sunstone is usually cabochon cut, but some of the most beautiful transparent stones are facet cut.

Sunstone is found in: Oregon, USA; Colorado, USA; India; Russia

4) Peristerite – (Labradorite – Spectrolite). Labradorite has a spectacular, metallic tinted, schiller effect known as Labradorescence, floating across the surface of this colorless to gray to brownish gemstone. The most common schiller colors are blues and greens, but golds, reds, purples, and a full spectrum of colors can be seen. Spectrolite is a most spectacular Labradorite from Finland.

Labradorescence is produced by the interference of light. This interference is caused by light bouncing off microscopic layers of different forms of Plagioclase Feldspar within the gems’ crystal lattice. Because labradorescence is produced by light bouncing off of layers within the stone, this gem has a “grain” and must be aligned before cutting, although, a cross-grain cut stone is, also, quite beautiful.

Labradorite is found in Labrador, Canada; Ukraine; Madagascar; Finland; USA; Mexico; Australia

Bytownite – This colorless to light pale yellow to champaign gem is usually faceted. Cut Bytownite is both set in jewelry and held in rare gemstone collections.

This gem is found around Bytown – (now Ottawa), Canada; Japan; USA, (New Mexico – transparent red).

This completes the Feldspar family of gems and minerals.

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