Quartzite is a metamorphic rock and is aptly named due to its high quartz content and resulting hardness. Comprising of greater than 90% quartz, quartzite is the largest and purest concentration of silica in the earths crust. Quartzite is commonly regarded as metamorphic rocks in origin and formed when Chert or Quartz Rich Sandstone has been exposed to high temperatures and pressures (metamorphism). These conditions fuse the quartz grains together forming a dense, hard, equigranular metamorphic rock. A metamorphic rock must contain at least 80% quartz by volume to be classified as a quartzite. The process of metamorphism combined with minerals within its environment will determine the quartzite appearance. Harder and more resistant than granite, its uses of quartzite are commonly in construction and more increasingly in decor. All though outcrops are found all over the earth, there are several Quartzite deposits in the United Kingdom also.
Chemical formula SiO2 'Silicon dioxide', also known as silica, is an oxide of silicon, and is porrly soluble. Most commonly found as quartz and in living organisms, silica is the major constituent of sand and is one of the most complex and most abundant materials. Uses of silica are wide and varied and include the following: Silica and aerogels Gels, Concrete, Casting, Glass, Optical Fibres, Ceramics, Food, Cosmetics, Pharmaceutical, Semiconductors & Dielectrics, and as a Fining agent (clarifying) Wine, Beer and juice (E number E551). Despite its uses, quartzite is a form of silica which is a possible cause for concern in various workplaces. All aspects of working with this material whether it is natural, engineered quartz or porcelain can release hazardous levels of crystalline silica dust particles into the air As a recognized human carcinogen it may lead to diseases of the lungs such as silicosis and pulmonary fibrosis.
Diatomaceous earth is a naturally occurring, soft, siliceous sedimentary rock crumbled into a whitish anrasive textured powder. Oven-dried diatomaceous earth is 80–90% silica, 2–4% alumina, and trace iron oxide and consists of fossilized remains of hard-shelled diatoms. Each deposit of diatomaceous earth differs by the concentrations of other natural clays and minerals, the diatom may species differ and in each deposit contain varying amounts of silica which depends on the sedimentation conditions. Common uses include: Filtration Aid, Metal Polishes, Toothpastes, Insecticides, Absorbents, Matting Agents, Fillers, Cat litter, Activators, Stabilizers, insulators and Soil
Despite its poor solubility, silica occurs in many living organisms. Plant materials with high silica phytolith content (Rigid microscopic structures made of silica) appear to be of importance to grazing animals. it certainly does occur in the living body, although exact reasoning is uncertain, it is thought that it is important to the growth, strength, and management of many connective tissues including bone, tooth and cell structures. silicification also occurs in bacteria and single-celled organisms such as shells diatoms, Radiolaria and testate amoebae.
Mainly of biological origin from Biogenic Sediment, but can also occur as a precipitate of chemicals or Diagenesis. The boundary between diagenesis and metamorphism is not defined but metamorphism occurs at higher temperatures and pressures. The colour of Chert depends wholly on the trace elements and minerals from the environment it is formed, for example red and green are most often related to traces of iron oxides.
An ocean sediment containing more than 30% skeletal debris from microorganisms and petrified skeletal microfossil remains of diatoms, silicoflagellates, radiolarians, cyanobacteria and occasional macrofossils that are found in the siliceous and biogenic sediment that cover deep ocean floors.
Carbonate Sediment (Skeletal Material) is of calcium carbonate in the form of the mineral calcite or 'aragonite' which is the crystal form of calclium carbonate and covers around half of the worlds seafloor above 4500 metres, most dominantly near the equator.
Siliceous Sediment are most prominent in the ocean around antarctica where approximately 75% of all oceans silica supply is deposited. Siliceous skeletons dissolve quickly in seawater, therefore, only robust skeletal remains are found in the siliceous sediments.
Erosion of rock under ground (deposition) settles into a sedimentary layers with microbial activity and minerals that condensate and precipate from solution (dissolution). Further deposition causes compaction whilst expelling fluids (lithification), gradually forming solid sedimentary rock. This continuous process of depsoition causes the sedimentary rock to be carried deeper into the earth where increased pressure and temperature transforms the organic content into kerogens and bitumens or replaced by other minerals such as calcite, siderite and pyrite.
High temperature and pressure causes metamorphism when applied to sedimentary rock and results in the recrystallization of individual quartz grains along with the former cementing material and the vitrification of the original sedimentary structures of the sandstone. The recrystallized quartz grains are roughly equal in size, forming what is called a granoblastic texture (course crystals of equal sizes), interlocked so tightly that when broken the rock will fracture through the grains forming an irregular or conchoidal fracture. The key difference between an orthoquartzite and a metaquartzite is the onset of recrystallization of existing grains.
Pure quartz sandstone sedimentary rock, converted by metamorphism into Metaquartzite through heat and pressure (tectonic compression) into a hard, non-foliated metamorphic rock metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Metaquartzite contains approximately 90% quartz with the remaining materials being of minerals.
It is likely that the sediments that form Orthoquartzite would of took longer to settle having been purified by ocean currents. Orthoquartzite is a quartzite of sedimentary origin, or pure quartz sandstone, with very low percentage of Chert grains with optical and geometric crystal lattice structures (crystallographic). Contains approximately 99% SiO2, lacks fossils and has scarce amounts of iron oxide and trace resistant minerals such as zircon, tourmaline, rutile and magnetite. Orthoquartzite is so highly cemented that it will fracture across grains, not around them.
Quartzite is a very hard nonfoliated metamorphic rock composed predominantly of an interlocking mosaic of quartz crystals, it is grainy/sugary in appearance with a glassy lustre. Although pure quartzite is usually opaque white to grey, other colours are a consequence of impurities being incorporated during metamorphism. The migration of former cementing materials during recrystallization and metamorphosis causes streaks and lenses to form within the quartzite. the former cementing materials include iron oxide, silica, carbonate and clay. Quartzite can sometimes appear similar to marble, however, a metal blade will not scratch a piece of quartzite and will not fizz on contact with dilute hydrochloric acid unlike marble.
Quartzite is harder and more resistant to stains than granite, used in slab form for flooring, walls, steps and tiles and more increasingly as countertops and kitchen worktops. It is heavily used as crushed stone for road construction and as a source of silica for production of silicon and silicon compounds.
Quartzite is very resistant to weathering and often forms ridges, crags and hilltops. The high silica content provides little material for soil so quartzite outcrops are often bare or covered only with a very thin layer of soil and void of anything more than grassess and heathers. A few examples of the most prominent quartzite outcrops found within the united kingdom.
A craggy ridge of quartzite runs parallel with the Pontesford-Linley fault.
5 miles west of Telford with an elevation of 407m it sits on the border of Shropshire.
Large abandoned and flooded quarry to the South East of Hartshill village.
Northern and western Anglesey and the adjacent Holy Island in North Wales.
Far north-west running in a narrow band from Loch Eriboll south-west toward Skye.
Across the northwest, with Errigal in Donegal as the most prominent outcrop.