Agate: The gemstone Agate is distinct from other forms of gemstones and is one of the widest source of colours chalcedony. Agate occurs in a variety of forms Agate has many colors. Agate mentioned in the Bible as being one of the stones of fire given to Moses and set in the breastplate of Aaron. A variety of agate, sardonyx is one of the twelve gemstones set in the foundations of the city walls of Jerusalem. Agate was especially valued during medieval times when one of the more outlandish uses was to bind an agate to each horn of an ox to ensure a good harvest. The danger here is that your agated beasts of burden may then become invisible and a little hard to find. Agate is believed to cure insomnia, offer protection from bad dreams, ensure pleasant dreams, protect against danger and promote strength and healing. The most famous of the european Agate mines where in Germany in Idar-oberstein these mines have now been worked out but can be chased back as far 16th century. The most important depsoits today are Brazil, and Uruguay as well as depsoits in Austrlia,China,India,Madagascar,Mexico,Mongolia,Namibia,United states as well as small depsoits being found around the world.
Amber is fossilized tree resin (not sap), which has been appreciated for its color and natural beauty since Neolithic times.[2] Amber is used as an ingredient in perfumes, as a healing agent in folk medicine, and as jewelry. There are five classes of amber, defined on the basis of their chemical constituents. Because it originates as a soft, sticky tree resin, amber sometimes contains animal and plant material as inclusions. Amber occurring in coal seams is also called resinite, and the term ambrite is applied to that found specifically within New Zealand coal seams. [3]Amber now has many synthetic and many are made containing all manner of bugs creatures which would never have been able to become trapped in the resin. One of the most famous things made from amber was the Amber Room in the Catherine Palace in Saint Petersburg, Russia. An intire chamber decorated and made of amber panels backed with gold leaf and mirrors. This room and what happened to it are one of the biggest mysterys of world war two the room was stolen by the germans and shipped away and then in the chaoes of the end of the war it was hidden some say destroyed but nobody knows for sure. A copy of this room has now been made and is back in the palace. The original covered more than 55 square meters and contained over six tons of amber . Many small musems have large collections of amber and some whole musems are dedicated to it completly in the former soviet block including Latvia And Estonia.
Amethyst is a violet variety of quartz often used in jewelry. The name comes from the Ancient Greek ἀ a- ("not") and μέθυστος methustos ("intoxicated"), a reference to the belief that the stone protected its owner from drunkenness; the ancient Greeks and Romans wore amethyst and made drinking vessels of it in the belief that it would prevent intoxication. It is one of several forms of quartz. Amethyst is the traditional birthstone for February.
Amethyst is the purple variety of quartz (SiO2), containing an impurity of iron, which gives the violet color to the mineral. The hardness of the mineral is the same as quartz's, thus it is suitable for use in jewelry. Amethyst is a variety of macrocrystalline quartz that occurs in transparent pastel roses to deep purples and violets. Now days Amethyst is also availible in green this is due to heating changing the colour from purple to green.
Andesine is a silicate mineral, a member of the plagioclase feldspar solid solution series. Its chemical formula is (Ca, Na)(Al, Si)4O8, where Ca/(Ca + Na) (% Anorthite) is between 30%-50%. The formula may be written as Na0.7-0.5Ca0.3-0.5Al1.3-1.5Si2.7-2.5O8.
The plagioclase feldspars are a continuous solid solution series and as such the accurate identification of individual members requires detailed optical study, chemical analysis or density measurements. Refractive indices and specific gravity increase directly with calcium content.
Andestine is a lesser know gemstone but is becoming more popular due to larger depsoits being found and worked. It comes in a range of colours from red to pink and also white, gray,yellow, and green it also ranges from opaque to transparent with the opaque the more common.
The plagioclase feldspars are a continuous solid solution series and as such the accurate identification of individual members requires detailed optical study, chemical analysis or density measurements. Refractive indices and specific gravity increase directly with calcium content.
Andestine is a lesser know gemstone but is becoming more popular due to larger depsoits being found and worked. It comes in a range of colours from red to pink and also white, gray,yellow, and green it also ranges from opaque to transparent with the opaque the more common.
Apatite is a group of phosphate minerals, usually referring to hydroxylapatite, fluorapatite, chlorapatite and bromapatite, named for high concentrations of OH−, F−, Cl− or Br− ions, respectively, in the crystal. The formula of the admixture of the four most common endmembers is written as Ca10(PO4)6(OH,F,Cl,Br)2, and the crystal unit cell formulae of the individual minerals are written as Ca10(PO4)6(OH)2, Ca10(PO4)6(F)2, Ca10(PO4)6(Cl)2 and Ca10(PO4)6(Br)2.Apatite is one of a few minerals that are produced and used by biological micro-environmental systems. Apatite is the defining mineral for 5 on the Mohs scale. Hydroxyapatite, also known as hydroxylapatite, is the major component of tooth enamel and bone mineral. A relatively rare form of apatite in which most of the OH groups are absent and containing many carbonate and acid phosphate substitutions is a large component of bone material.
Fluorapatite (or fluoroapatite) is more resistant to acid attack than is hydroxyapatite. For this reason, toothpaste typically contains a source of fluoride anions (e.g. sodium fluoride, sodium monofluorophosphate). Similarly, fluoridated water allows exchange in the teeth of fluoride ions for hydroxyl groups in apatite. Too much fluoride results in dental fluorosis and/or skeletal fluorosis.
Fission tracks in apatite are commonly used to determine the thermal history of orogenic (mountain) belts and of sediments in sedimentary basins. (U-Th)/He dating of apatite is also well established for use in determining thermal histories and other, less typical applications such as paleo-wildfire dating.
Phosphorite is a phosphate-rich sedimentary rock, that contains between 18% and 40% P2O5. The apatite in phosphorite is present as cryptocrystalline masses referred to as collophane.
The mineral beryl is a beryllium aluminium cyclosilicate with the chemical formula Be3Al2(SiO3)6. The hexagonal crystals of beryl may be very small or range to several meters in size. Terminated crystals are relatively rare. Pure beryl is colorless, but it is frequently tinted by impurities; possible colors are green, blue, yellow, red, and white. Beryl comes in a wide range of colours and is found in depsoits worldwide some of the better known varieties are Golden beryl, Goshenite, And also morganite because of this the colours also range widely as well as from opaque to transparent.
Calcite crystals are trigonal-rhombohedral, though actual calcite rhombohedra are rare as natural crystals. However, they show a remarkable variety of habits including acute to obtuse rhombohedra, tabular forms, prisms, or various scalenohedra. Calcite exhibits several twinning types adding to the variety of observed forms. It may occur as fibrous, granular, lamellar, or compact. Cleavage is usually in three directions parallel to the rhombohedron form. Its fracture is conchoidal, but difficult to obtain.
Calcite also know as limespar, limestone is found in a range of colours also ranging from transparent to translucent. It is a quite soft gem ranging at only 3 on the mohls hardness scale so great care must be taken when working with this item.
The mineral beryl is a beryllium aluminium cyclosilicate with the chemical formula Be3Al2(SiO3)6. The hexagonal crystals of beryl may be very small or range to several meters in size. Terminated crystals are relatively rare. Pure beryl is colorless, but it is frequently tinted by impurities; possible colors are green, blue, yellow, red, and white. Beryl comes in a wide range of colours and is found in depsoits worldwide some of the better known varieties are Golden beryl, Goshenite, And also morganite because of this the colours also range widely as well as from opaque to transparent.
Calcite crystals are trigonal-rhombohedral, though actual calcite rhombohedra are rare as natural crystals. However, they show a remarkable variety of habits including acute to obtuse rhombohedra, tabular forms, prisms, or various scalenohedra. Calcite exhibits several twinning types adding to the variety of observed forms. It may occur as fibrous, granular, lamellar, or compact. Cleavage is usually in three directions parallel to the rhombohedron form. Its fracture is conchoidal, but difficult to obtain.
Calcite also know as limespar, limestone is found in a range of colours also ranging from transparent to translucent. It is a quite soft gem ranging at only 3 on the mohls hardness scale so great care must be taken when working with this item.
A crystal or crystalline solid is a solid material whose constituent atoms, molecules, or ions are arranged in an orderly, repeating pattern extending in all three spatial dimensions. The scientific study of crystals and crystal formation is known as crystallography. Crystals is a solid substance in which the molecules, atoms, or ions are arranged in an orderly repeating pattern extending in all three spatial dimensions. The word crystal is a loan from the ancient Greek word. Crystals are often symmetrically which had the same meaning, but according to the ancient understanding of crystal.
Emerald is a variety of the mineral beryl (Be3Al2(SiO3)6) colored green by trace amounts of chromium and sometimes vanadium. Beryl has a hardness of 7.5–8 on the 10 point Mohs scale of mineral hardness. Most emeralds are highly included, so their toughness (resistance to breakage) is classified as generally poor. The word "Emerald" is derived (via Old French: Esmeraude and Middle English: Emeraude), from Vulgar Latin: Esmaralda/Esmaraldus, a variant of Latin Smaragdus, which originated in Greek: σμάραγδος (smaragdos; "green gem"); its original source being either the Hebrew word אזמרגד izmargad meaning "emerald" or "green"[ or the Sanskrit word मरकत marakata meaning "emerald." The name could also be related to the Semitic word baraq (בָּרָק ;البُراق; "lightning" or "shine") (cf. Hebrew: ברקת bareqeth and Arabic: برق barq "lightning"). It is the same source for the names Persian (زمرّد zomorrod), Turkish (zümrüt), Sanskrit (मरकत ; marakata), Kannada (ಪಚ್ಚೆ ; Pacche), Telugu (Paccha), Georgian (ზურმუხტი; zurmukhti), Russian (изумруд; izumrud)[4] and Armenian zmruxt.

















