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Yellow Gemmy Apatite

The apatite Mineral Group

Apatite is named for the Greek word apate, which means "deceit", since Apatite is similar in appearance to many other minerals. Apatite describes a group of similar isomorphous hexagonal phosphate minerals. The primary Apatite group includes Fluorapatite, Chlorapatite, and Hydroxylapatite. The extended Apatite supergroup describes additional minerals such as Pyromorphite, Mimetite, and Vanadinite, but these are described individually in this guide.

It can be difficult to distinguish between individual members of the primary Apatite group. A designation of the specific Apatite type is not usually made, being called simply "Apatite" by collectors and dealers. However, most of the fine crystals and collector specimens are of the Fluorapatite type, which is by far the most common form of Apatite.

Apatite is the most common phosphate mineral, and is the main source of the phosphorus required by plants. The bones and teeth of most animals, including humans, are composed of calcium phosphate, which is the same material as Apatite. (These biological Apatites are almost exclusively the Hydroxylapatite type.)
Chemical Formula Apatite is mineral group with the following chemical formula applied to the most common members of the primary group (excluding the extended Apatite supergroup):

Individual Apatite minerals are:
Fluorapatite - Ca5(PO4)3F
Chlorapatite - Ca5(PO4)3Cl
Hydroxylapatite - Ca5(PO4)3OH
Composition Apatite group - Calcium fluoro-chloro-hydroxyl phosphate

Common Individual Group Members:
Fluorapatite - Calcium fluoro-phosphate
Cholorapatite - Calcium chloro-phosphate
Hyldroxylapatite - Basic calcium phosphate
Variable Formula
Color Colorless, white, yellow, brown, gray, red, pink, purple, blue, green. Some specimens are multicolored.
Streak White
Hardness 5
Crystal System Hexagonal
3D Crystal Atlas
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Crystal Forms
and Aggregates
(The hexagonal crystal system designation is due to a hexagonal symmetry of most Apatite. However, positional ordering of chlorine atoms or the hydroxyl radical in Chlorapatite and Hydroxylapatite can lead to monoclinic symmetry.)

Apatite generally forms as well-shaped hexagonal crystals, which may be prismatic, dipyramidal, and stubby. Also as flat, tabular plates, columnar, in stacked parallel growths, as globular masses, acicular, grainy, stalactitic, botryoidal, and earthy. Also in enormous beds of massive material, from which industrial phosphorus is mined.
Transparency Transparent to translucent
Specific Gravity 3.1 - 3.2
Luster Vitreous
Cleavage Indiscernible
Fracture Conchoidal
Tenacity Brittle
Other ID Marks 1) Specimens from certain localities will fluoresce orange yellow in shortwave ultraviolet light.
2) Thermoluminescent bluish-white.
Complex Tests 1) May become fluorescent orange-yellow in longwave ultraviolet light after heating.
2) Dissolves in hydrochloric acid.
In Group Phosphates; True Phosphates; Apatite Group
Striking Features Hardness and crystal form
Environment As gemmy crystals in granite pegmatites; in hornfels in contact metamorphic rocks; in igneous diabase environments; in ore veins, and in nepheline syenite pegmatites.
Rock Type Igneous, Metamorphic
Popularity (1-4) 2
Prevalence (1-3) 1
Demand (1-3) 1

Apatite ON EBAY

 -  Variety of the Apatite group where the phosphate radical (PO4) is partially replaced by a carbonate radical (CO3). It has a chemical formula of Ca5(PO4,CO3)3(OH,F). Also known as Carbonate-rich Apatite.
 -  Individual member mineral of the Apatite group with chlorine being dominant in its structure. For a short period of time, it was renamed by the IMA as Apatite-(CaCl), but is now again favored again as Chlorapatite.
 -  Microcrystalline variety of botryoidal white Apatite.
 -  Individual member mineral of the Apatite group with fluorine being dominant in its structure. For a short period of time, it was renamed by the IMA as Apatite-(CaF), but is now again favored again as Fluorapatite.
 -  Individual member mineral of the Apatite group with hydroxyl being dominant in its structure. For a short period of time, it was renamed by the IMA as Apatite-(CaOH), but is now again favored again as Hydroxylapatite.
 -  Manganese-rich variety of Apatite.
 -  A strontium-rich form of Apatite containing some rare earth elements, described from Lovozero in the Kola peninsula of Russia.
 -  A botryoidal variety of Apatite, originally described from Staffel, Hesse, Germany.
 -  Rare, strontium-rich variety of Apatite, with the calcium partially replaced by strontium. Its chemical formula is (Sr,Ca)5(PO4)3(OH,F).

Apatite is the main source of phosphorus. Phosphorus was previously extracted from crystalline Apatite, but nowadays is extracted from enormous deposits of Apatite-rich rock. Apatite is essential in the manufacture of phosphate fertilizers, and is very important in the chemical and pharmaceutical industries. Apatite is also a popular collectors mineral, and some transparent specimens are faceted for collectors. The gemmy violet and reddish forms are very much valued by collectors and command high prices.

Apatite is very common; only the classic localities are mentioned here. European localities include Ehrenfriedersdorf, in the Erzgebirge, Saxony, Germany, which is the type locality for this mineral; and Panasqueira, Portugal, where thick gemmy crystals were found. Deep blue crystals come from Sludyanka, in Lake Baikal area, Russia; and interesting forms, especially botryoidal, come from the Lovozero Massif, Kola Peninsula, Russia. Purple Apatite comes from the Mawi Pegmatite, Nuristan (Laghman) Province, Afghanistan; and pink and red crystals from Pakistan in the Hunza Vallery, Gilgit; and at Skardu at Shengus, Dassu, and the Shigar Valley. Beautiful greenish-yellow Apatites with a excellent luster and transparency have been coming from the Imichil area in Morocco.

In Brazil, deep blue Apatite crystals come from Ipira, Bahia; and the state of Minas Gerais has several outstanding occurrences such as the Sapo mine, in Conselheiro Pena; Golconda, in Governador Valadares; Pederneira, in Sao Jose da Safira; and Galileia. A pink Apatite has recently come from the La Marina Mine, Boyaca, Colombia. One of the most famous localities of Apatite is Cerro de Mercado, Durango, Mexico, where gemmy prismatic crystals are plentiful.

In Canada, large glassy crystals in orange Calcite come from the Yates mine, Otter Lake, Quebec. Very large crystals also come from Ontario, at Bear Lake in Tory Hill, and at Cardiff, both in Haliburton Co.

In the U.S., the state of Maine has several excellent Apatite localities. Beautiful violet crystals come from the Mount Apatite area (especially the Pulsifier Quarry in Auburn, and the Mt. Rubellite Quarry in Hebron,) Androscoggin Co. Also in Maine are the Noyes Mountain Quarry (Harvard Quarry) and the Emmons Quarry, Uncle Tom Mt, both in Greenwood, Oxford Co. In New Hampshire, Apatite was found in the Palermo No. 1 Mine, Groton, Grafton Co. The Acushnet Quarry in Bristol Co., Massachusetts, produces an aesthetic association of transparent Apatite associated with sparkling dark Chlorite.

Prismatic green crystals, closely resembling Tourmaline, come from the Himalaya Mine, Mesa Grande, San Diego Co., California. Light blue crystals have come from the Butte mining district, in Silver Bow Co.,  Montana; and large yellow crystals from the Fulford District, Eagle Co., Colorado and Iron Mountain, Iron Co., Utah. Large opaque Apatite crystals come from Franklin, Ogdensburg (Sterling Hill), and Hamburg, all in Sussex Co., New Jersey; and across the state border in Amity, Orange Co., New York. Good specimens were once found in the Strickland Quarry, Portland, Middlesex Co., Connecticut.

Quartz, Feldspar, Calcite, Magnetite, Muscovite, Phlogopite, Nepheline, Diopside

Beryl, Tourmaline, and Quartz - Greater hardness.
Calcite - Lower hardness, effervescent in acid.
Pyromorphite, Mimetite, and Vanadinite - Slightly softer and usually occur in distinct localities.

apatite PHOTOS
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