In terms Amazonite can be found in a Green type of formation that comes from several Microcline Feldspars. Generally the name for Amazonite is considered to have came from the Amazon as it became obtained within this river. Many people once believed that the Green in Amazonite had came from copper compounds but more recently the Blue-Green Colour is considered to come from small amounts of Lead and Water within Feldspar.
Feldspar is rather considered to come in formation with its own group that's known as Tectossillicate Minerals, which make up 60% of the Earths Crust. In general Feldspar comes in the form of a crystallization that formed by Magma as a vein structure in both Intrusive and Extrusive Igneous Rock formation, that also represent in many different types of Metamorphic Rock. Most of its whole entire formation is formed by Calcic Plagioclase feldspar that identified as Anorthosite. In several case Feldspar comes from the German word Feldspat that means field, and Spat. Its also widely found in the Province of Ontario, Canada.
This mineral comprises of phyllosilicate mineral, which is commonly found in the Mica Group of materials. In most cases Biotite is determined to be called Dark Mica that's has its own Solid Solution Series between Magnesium, Aluminous, Iron, Phlogopite, Siderophyllite, and Annite. More so this mineral was rather believed to have been named after J.F.L. Hausmann in 1847. Nevertheless, it became named in honor of French Physicist Jean Baptiste Bio, who made several discoveries of Mica, and would have also research the optical properties of Mica. This mineral it self is more of a sheet silicate that contains Silicon, Oxygen, Iron, Aluminium, Hydrogen, and Magnesium contents, which are bounded together with Potassium Ion. Many geologist refer this mineral to be also considered as Iron Mica because the iron content is determined to be more richer than Phlogopite. The properties of this mineral are identified to be its crystal formation. Biotite is known to also occur in the formation of Igneous, and Metamorphic Rocks. This mineral can also be found in Bancroft, Ontario, Canada.
Beryl is also considered as a mineral that's composed of Beryllium Aluminium Cyclosilicate, and is commonly known as the second hardest rock after Diamond. Most of this name was adapted from the Greek Word meaning Precious Blue-Green Colour of Sea-Water Stone. In general Beryl is commonly considered to be formed Mica Schist, limestone, and even granitic Pegmatite's. It also known to be formed in a Crystal like structure and has 6 different types of Beryl Cattagories. All of these are identified as Aquamarine, Emerald, Golden Beryl, Goshenite, Morganite, and not least read Beryl. This type of crystaline mineral can be found at the Quadeville Beryl Pit in Quadeville, Ontario, Canada.
Rose Quartz are more of a pale pine to Red types of quartz that are formed by small trace amounts of Iron, Manganese, and Titanium. This Mineral can also be found in the Province of Ontario, at a mine known as the Aqua Rose Pegmatite, in Quadeville.
Talc is characterized as a mineral that's considered as a Hydrated Magnesium Silicate compound. It also known as a Metamorphic Mineral, which is formed from Metamorphism of Magnesian minerals that included amphibole. Serpentine, Olivine, pyroxene, that comes in presence of Carbon Dioxide, and Water. This is also referred to as Talc Carbonation or Steelization, which forms a suite of rocks known as Talc Carbonates. Sometimes Talc is also formed with the reaction of other minerals like for example Dolomite, and Silica. Another formation of talc can be produced by the combination of Magnesian Chlorite, and quartz
Gypsum is considered as another mineral that's known to be a soft sulphate, which is strongly known to be compose with Calcium Sulphate Dehydrate It was rather believe to have came from the Ancient Greek Word that means Moon. Its formation is rather said to come in a crystalized form, and is found at the Lafarge Quarry, in Dundas, Ontario, Canada.
This mineral is rather known to be one of the major compounds of Zink Sulphide thats fromed in crystals. When it Iron Purities are high its considered to be black, and called Marmatite. Most of this mineral can usually be uncovered within patches of pyrite, and Galena Sulphides that consist of Fluorite, Dolomite, and not least Calcite. It another Mineral that's found the Lincoln Quarry in Beamsville, Ontario, Canada.
Galena is determined to be a type of lead sulphide and is sometimes referred as Lead Glance. In nature geologist have examined this mineral to be one of the most important lead ore that's considered to usually be found with silver, which averages 1 to 2 %. Its chemical compounds are rather said to be identified as Sulphide type of mineralization. Most of its own formation rather comes from cubic Crystal system that sometime come in contact with Octahedral formations. It comes in association with the minerals that are known as Flouride, Sphalerite, and not least Calcite. This mineral can be found at the Dundas Quarry in, Dundas, Ontario, Canada.
This mineral is rather referred as an amphibole Silicate mineral that's also found in Frontenac, Ontario, Canada, at the Star Gold Mine. Most of the name Actinolite is known to come from the Greek word known as Aktis that means Beam or Ray. It mineralogy is said to be determined as a member in Solid Solution series of Tremolite, and Iron Rich Ferro Actinolite Most of this mineral is rather uncovered in metamorphic rocks that contain intrusive igneous Rocks. It occurrence is formed from metamorphism of Magnesium Rich Limestone.