Pink Quartz (2) Raw Minerals Stones Rocks Collecting

Description

Origin : Brazil

Pink Quartz 26-40 gr - cm 3-5 Raw Minerals Stones Rocks for Collection.

Pink Quartz is a type of quartz that has a pale pink to pinkish red hue. The color is generally thought to be due to traces of titanium, iron or manganese in the material. Some rose quartz contain microscopic rutile needles which produce an asterism in transmitted light. Recent X-ray diffraction studies suggest that the color is likely due to fine microscopic dumortierite fibers within the quartz.
Pink quartz can also be crystalline, with a color that is thought to be caused by traces of phosphate or aluminum, up to being almost transparent or translucent in the most precious and sought-after varieties; the color of the powder is white, while it has a glassy sheen and excellent light diffusion. The color in the crystals is apparently photosensitive and prone to fading. Like all stones belonging to the quartz family, it has the property of piezoelectricity.
The first crystals have been found in Maine, the United States, and Brazil.

Quartz (silicon dioxide, SiO2, is the second most abundant mineral in the earth's crust (about 12% of its volume) after feldspars.
The etymology of the name is not certain, but for the ancient Greeks quartz was defined as crystal (from the Greek κρύσταλλος, krýstallos, ice). In fact, they considered this mineral a variety of ice cold to the point that it could no longer be dissolved.
Quartz has a crystalline structure made up of silicon and oxygen tetrahedrons joined together by the 4 vertices to form spirals. The habitus (the shape) is a hexagonal prism with the faces of two rhombohedrons at the vertices arranged in such a way as to form a hexagonal bipyramid. Quartz can have an elongated prismatic shape.
Quartz is a common constituent of acidic intrusive magmatic rocks, among which the best known is granite; it is also abundant as a component of sedimentary rocks, preferably in sandstones due to its high resistance to chemical degradation by atmospheric agents and its insolubility in water and in metamorphic rocks.
Being one of the most common minerals of the earth's crust, quartz has a large number of different varieties, with macroscopic crystals visible to the naked eye, or crystals so small as to be visible only under a microscope or even invisible with such an instrument. Although many of the variety names have historically come from the colors of the mineral, current scientific naming schemes refer primarily to the microstructure of the mineral. Usually, but not always, color is a secondary identifier.
In addition to hyaline quartz, perfectly colorless and clear, there are numerous other varieties of quartz, many of which are for sale on our site:
Chalcedony, Agate, Moss Agate, Chrysoprase, Onyx, Carnelian, Sardonyx, Jasper, Heliotrope, Aventurine, Tiger's Eye, Cat's Eye, Bull's Eye, Hawk's Eye, Amethyst, Ametrine, Citrine or Madeira, Rose Quartz, Quartz blue, Prasiolite, Milky Quartz, Smoky Quartz, Morion, Rutilated Quartz, Tourmaline Quartz, Dendritic Quartz, etc.
Quartz is a material with remarkable chemical stability and is resistant to acids except hydrofluoric acid. It has high hardness (7 on the Mohs scale), mechanical and heat resistance. The quartz has no cleavage. Some physical properties of quartz crystals are piezoelectricity and pyroelectricity, i.e. the ability to electrically polarize the opposite faces of the crystal following the mechanical deformation caused by compression or after heating. From an optical point of view, quartz has high transmissibility in the visible and especially in the ultraviolet.