Instruct: Given a question, retrieve passages that answer the question.
Query: Can you mine clay?
The fire brick company Thomas Wragg & Sons owned a Pot Clay mine immediately to the south east of the hamlet. Pot Clay is the impure version of Ganister and was in demand in the Sheffield steel industry to make bricks for the lining of furnaces. In the early 1970s the mine was producing 15,000 tons of clay per year, with the company quoting, “The mine can be worked at the present rate for 100 years”. A refractory brick works stood at the entrance to the mine. However the Ughill mine had drainage problems and although powerful pumps had been installed in the 1950s to pump between 600 and 800 gallons per minute from the mine, the mine closed on 17 November 1977. It had become uneconomic to mine the clay due to water problems and the owners found it more profitable to bring in clay from the Midlands. The site of the mine has been landscaped and returned to agricultural use. J&J Dyson mined fireclay at their open cast quarry at Wheatshire between Ughill and Sugworth. The quarry is closed but can still be seen from the nearby road. Thos. Wragg had small firebrick works at Load Brook (closed 1957) and Brookside (Stopes Road, Stannington, closed 1960) the former previously owned by the Trickett family, the latter by the Drabble family and a major works (Old Wheel Brick Works) in the nearby Loxley Valley. Wraggs along with its local competitors, J&J Dyson of Griffs Works, Stannington and Thos. Marshall of Storrs Bridge Works, Loxley, mined the Stannington Pot Clay seam and manufactured fireclay-based casting pit holloware refractories for use in steel making worldwide. All three plants closed following a collapse in demand for casting pit refractories of the type made locally mainly because of the introduction of continuous casting of steel worldwide and the general demise of the British steel industry.
Silicon is a chemical element with symbol Si and atomic number 14. It is a hard and brittle crystalline solid with a blue-grey metallic lustre; and it is a tetravalent metalloid and semiconductor. It is a member of group 14 in the periodic table: carbon is above it; and germanium, tin, and lead are below it. It is relatively unreactive. Because of its high chemical affinity for oxygen, it was not until 1823 that Jöns Jakob Berzelius was first able to prepare it and characterize it in pure form. Its melting and boiling points of 1414 °C and 3265 °C respectively are the second-highest among all the metalloids and nonmetals, being only surpassed by boron. Silicon is the eighth most common element in the universe by mass, but very rarely occurs as the pure element in the Earth's crust. It is most widely distributed in dusts, sands, planetoids, and planets as various forms of silicon dioxide (silica) or silicates. More than 90% of the Earth's crust is composed of silicate minerals, making silicon the second most abundant element in the Earth's crust (about 28% by mass) after oxygen.
The major industry in the town is cereal storage. The National Cereals Board has a cereal storage depot located in the town which consists of eight large silos with a capacity of approximately 5 million tonnes of grain. It is one of the largest in the country and plays a significant role in Kenya's food security. In the recent past, Moisbridge has since taken a new shape with great engineers. Some of the growing industries includes quarry mining and milling firms.
Compared to other metals, gold is malleable, ductile, rare, and it is the only solid metallic element with a yellow color. It may easily be melted, fused, and cast without the problems of oxides and gas that are problematic with other metals such as bronzes, for example. It is fairly easy to "pressure weld", wherein similarly to clay two small pieces may be pounded together to make one larger piece. Gold is classified as a noble metal—because it does not react with most elements. It usually is found in its native form, lasting indefinitely without oxidization and tarnishing.
Volcanic bombs are extrusive igneous rocks ranging from the size of books to small cars, that are explosively ejected from stratovolcanoes during their climactic eruptive phases. These "bombs" can travel over away from the volcano, and present a risk to buildings and living beings while shooting at very high speeds (hundreds of kilometers/miles per hour) through the air. Most bombs do not themselves explode on impact, but rather carry enough force so as to have destructive effects as if they exploded.
There is varying and sometimes inconsistent nomenclature differentiating substances, which include truly non-stoichiometric examples, from chemical compounds, which require the fixed ratios. Many solid chemical substances—for example many silicate minerals—are chemical substances, but do not have simple formulae reflecting chemically bonding of elements to one another in fixed ratios; even so, these crystalline substances are often called "non-stoichiometric compounds". It may be argued that they are related to, rather than being chemical compounds, insofar as the variability in their compositions is often due to either the presence of foreign elements trapped within the crystal structure of an otherwise known true "chemical compound", or due to perturbations in structure relative to the known compound that arise because of an excess of deficit of the constituent elements at places in its structure; such non-stoichiometric substances form most of the crust and mantle of the Earth. Other compounds regarded as chemically identical may have varying amounts of heavy or light isotopes of the constituent elements, which changes the ratio of elements by mass slightly.
Ray is a one side infinite geodesic which is minimizing on each interval
Metal tools first appeared in Wales about 2500 BC, initially copper followed by bronze. The climate during the Early Bronze Age (c. 2500–1400 BC) is thought to have been warmer than at present, as there are many remains from this period in what are now bleak uplands. The Late Bronze Age (c. 1400–750 BC) saw the development of more advanced bronze implements. Much of the copper for the production of bronze probably came from the copper mine on the Great Orme, where prehistoric mining on a very large scale dates largely from the middle Bronze Age. Radiocarbon dating has shown the earliest hillforts in what would become Wales, to have been constructed during this period. Historian John Davies, theorises that a worsening climate after around 1250 BC (lower temperatures and heavier rainfall) required more productive land to be defended.
Longkou Mining Group, subsidiary of Shandong Energy, produces oil shale as a coal mining byproduct. It operates shale oil plant which is equipped with 40 Fushun retorts. The shale oil production is about 120,000 tonnes per year and the planned full capacity is 200,000 tonnes of shale oil per year. The company also plans to utilize Enefit-280 technology. In addition, the company plans to burn shale char mixed with particulate oil shale in fluidized bed combustion for power generation, and the shale ash would be utilized for production of building material.
The Marange diamond fields are an area of widespread small-scale diamond production in Chiadzwa, Mutare West, Zimbabwe. 'Although estimates of the reserves contained in this area vary wildly, some have suggested that it could be home to one of the world's richest diamond deposits'. The hugely prolific fields are regarded by some experts as the world's biggest diamond (in carats, not by value) find in more than a century. Production from Marange is controversial due to ongoing legal wrangles and government crackdowns on illegal miners and allegations of forced labour. In terms of carats produced, the Marange field is the largest diamond producing project in the world, estimated to have produced 16.9 million carats in 2013, or 13% of global rough diamond supply. Marange is estimated to have produced 12.0 million carats in 2012, 8.7 million carats in 2011, and 8.2 million carats in 2010. While some diamond mines produce rough valued at over $1000 per carat, average production at Marange is estimated at under $50 per carat.
Lahars (from a Javanese term for volcanic mudflows) are mixtures of volcanic debris and water. Lahars usually come from two sources: rainfall or the melting of snow and ice by hot volcanic elements, such as lava. Depending on the proportion and temperature of water to volcanic material, lahars can range from thick, gooey flows that have the consistency of wet concrete to fast-flowing, soupy floods. As lahars flow down the steep sides of stratovolcanoes, they have the strength and speed to flatten or drown everything in their paths. Hot ashes, lava flows and pyroclastic surges ejected during 1985 eruption of Nevado del Ruiz in Colombia melted snow and ice atop the high Andean volcano. The ensuing lahar flooded the city of Armero and nearby settlements, killing 25,000 people.
Silicon is a crystalline solid with a blue-grey metallic lustre. Like boron, it is less dense (at 2.33 g/cm) than aluminium, and is hard and brittle. It is a relatively unreactive element. According to Rochow, the massive crystalline form (especially if pure) is "remarkably inert to all acids, including hydrofluoric". Less pure silicon, and the powdered form, are variously susceptible to attack by strong or heated acids, as well as by steam and fluorine. Silicon dissolves in hot aqueous alkalis with the evolution of hydrogen, as do metals such as beryllium, aluminium, zinc, gallium or indium. It melts at 1414 °C. Silicon is a semiconductor with an electrical conductivity of 10 S•cm and a band gap of about 1.11 eV. When it melts, silicon becomes a reasonable metal with an electrical conductivity of 1.0–1.3 × 10 S•cm, similar to that of liquid mercury.
Fluorapatite (Ca(PO)F) is mined along with other apatites for its phosphate content and is used mostly for production of fertilizers. Most of the Earth's fluorine is bound in this mineral, but because the percentage within the mineral is low (3.5%), the fluorine is discarded as waste. Only in the United States is there significant recovery. There, the hexafluorosilicates produced as byproducts are used to supply water fluoridation.
Cybertron is a fictional planet, the homeworld of the Transformers
Platinum exists in higher abundances on the Moon and in meteorites. Correspondingly, platinum is found in slightly higher abundances at sites of bolide impact on Earth that are associated with resulting post-impact volcanism, and can be mined economically; the Sudbury Basin is one such example.
These ceramic eggs were common in Kievan Rus', and had a characteristic style. They were slightly smaller than life size (2.5 by 4 cm, or 1 by 1.6 inches), and were created from reddish pink clays by the spiral method. The majolica glazed eggs had a brown, green or yellow background, and showed interwoven yellow and green stripes. The eggs made in large cities like Kiev and Chernihiv, which had workshops that produced clay tile and bricks; these tiles (and pysanky) were not only used locally, but were exported to Poland, and to several Scandinavian and Baltic countries.
Yellowstone National Park has one of the world's largest petrified forests, trees which were long ago buried by ash and soil and transformed from wood to mineral materials. This ash and other volcanic debris are believed to have come from the park area itself as the central part of Yellowstone is the massive caldera of a supervolcano. The park contains 290 waterfalls of at least , the highest being the Lower Falls of the Yellowstone River at .
A proppant is a solid material, typically sand, treated sand or man-made ceramic materials, designed to keep an induced hydraulic fracture open, during or following a fracturing treatment. It is added to a "fracking fluid" which may vary in composition depending on the type of fracturing used, and can be gel, foam or slickwater–based. In addition, there may be unconventional fracking fluids. Fluids make tradeoffs in such material properties as viscosity, where more viscous fluids can carry more concentrated proppant; the energy or pressure demands to maintain a certain flux pump rate (flow velocity) that will conduct the proppant appropriately; pH, various rheological factors, among others. In addition, fluids may be used in low-volume well stimulation of high-permeability sandstone wells (20k to 80k gallons per well) to the high-volume operations such as shale gas and tight gas that use millions of gallons of water per well.
The cave consists of Chert (known as the Lost River Chert), which is overlaid by the Ste. Genevieve Limestone and St. Louis Limestone, both of which were laid down in the middle to late Mississippian Period. The river appears above ground in three short sections before flowing into the mouth of the cave. The most interesting section is the blue hole, which is the cause of the Lost River being listed by Ripley's Believe it or Not as the "Shortest, deepest river in the world." Plumb bobs indicated that the blue hole was 437 feet deep, while the river itself is only 400 feet long. In fact, the blue hole is only 16 feet deep, but is linked to a further underground river. This caused plumb bobs to be swept underground, returning erroneous measurements.
In addition to protecting against mining contamination, Idaho Conservation League works to protect Idaho’s ground water from hydraulic fracturing, otherwise known as “fracking,” a process used in natural gas extraction. When a natural gas company began exploration in western Idaho in 2011, ICL asked the Idaho oil and Gas Conservation Commission to prohibit carcinogenic chemicals and require companies to provide a bond protecting Idaho communities in the case of a fracking emergency. ICL has one main goal in regards to fracking, that "Idaho has rules protective of the people's groundwater" that set limitations on the use of hazardous substances.
Cobalt-based blue pigments (cobalt blue) have been used since ancient times for jewelry and paints, and to impart a distinctive blue tint to glass, but the color was later thought by alchemists to be due to the known metal bismuth. Miners had long used the name "kobold ore" (German for "goblin ore") for some of the blue-pigment producing minerals; they were so named because they were poor in known metals, and gave poisonous arsenic-containing fumes when smelted. In 1735, such ores were found to be reducible to a new metal (the first discovered since ancient times), and this was ultimately named for the "kobold".
Well-crystallized and pure samples are ideal for x-ray diffraction, but this is rarely the case for clay. Clay minerals are almost always mixed with very small amounts of nonclay minerals which can produce intense peaks, even when there is very little of the sample is not a clay. If additional minerals are known to be presents, attempts should be made to separate clays from nonclays otherwise additional peaks should be expected. Some common minerals associated with naturally occurring clays are; quartz, feldspars, zeolites, and carbonates organic matter is sometimes present. Synthesis of clays can reduce the presence of some of these associated materials but does not guarantee pure samples as quartz or other associated materials are still commonly produced alongside synthetic clays.
According to Jainism, causes are of two types – "Upādanā kārana" (substantial or material cause) and "Nimitta kārana" (instrumental cause). "Upādanā kārana" is always identical with its effect. For example, out of clay, you can only produce a clay pot; hence the clay is the "upādanā kārana" or material cause and clay pot its effect. Wherever the effect is present, the cause is present and vice versa. The effect is always present in latent form in the material cause. For transforming the clay to pot, the potter, the wheel, the stick and other operating agents are required that are merely nimitta or instrumental cause or catalysts in transformation. The material cause always remains the clay. Hence the cause and effect are always entirely identical in nature. Potter cannot be the material cause of pot. If this were the case, then Potter might as well prepare the pot without any clay. But this is not so. Thus a clay pot can only be made from clay; gold ornaments can be made only from gold. Similarly the different modes of existence of a soul are a result of activities of soul itself. There cannot be any contradiction or exceptions.
Clay is chosen largely based on local materials available. There is an abundance of most basic types of clay in Japan. Due to naturally occurring kaolin deposits, many porcelain clays are found in Kyushu. Kilns were traditionally built at the sites of clay deposits, and most potters still use local clays, having developed a range of glazes and decoration techniques especially suited to that clay. The pottery clays found in the Japanese archipelago range from fusible earthenwares to refractory kaolins. From the Jōmon period to the Yayoi period, Japanese potters relied on high plastic iron-bearing shale and alluvial clays. Organic materials appear in much of the early Jōmon period work, but sand or crushed stone predominates thereafter. Further refinements came about under the Chinese influence in the 8th and 9th centuries AD, when creators of Nara three-color wares and Heian ash glazed wares sought out white, refractory clays and enhanced their fineness through levigation. In Kyoto, where demand makes it both practical and profitable, the clay is crushed, blunged (made into slip), and filtered commercially. To use the clay, you must first break it up into small pieces, pour a small amount of water over it, and beat it with a "kine", a wooden mallet, until you obtain the plasticity and uniformity of texture you want. Then you put it through an "aramomi" or "rough wedging" process, a kneading movement, after which the clay is stored for two or three days, or sometimes up to a week. Before the clay is ready to be thrown, it must pass through the "nejimomi" ("screw-wedge") process, which produces a bullet-shaped mass from which all air bubbles have been removed and in which the granular structure is arranged so that it radiates outwards from the center of the mass.
There are several materials that are referred to as clay. The properties which make them different include:
Plasticity, the malleability of the body; the extent to which they will absorb water after firing; and shrinkage, the extent of reduction in size of a body as water is removed. Different clay bodies also differ in the way in which they respond when fired in the kiln. A clay body can be decorated before or after firing. Prior to some shaping processes, clay must be prepared. Each of these different clays are composed of different types and amounts of minerals that determine the characteristics of resulting pottery. There can be regional variations in the properties of raw materials used for the production of pottery, and this can lead to wares that are unique in character to a locality. It is common for clays and other materials to be mixed to produce clay bodies suited to specific purposes. A common component of clay bodies is the mineral kaolinite. Other mineral compounds in the clay may act as fluxes which lower the vitrification temperature of bodies. Following is a list of different types of clay used for pottery.