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clays

A Wisdom Archive on clays

clays

A selection of articles related to clays

clays


ARTICLES RELATED TO clays

clays: Encyclopedia II - Shale - Formation

The fine particles that compose shale can remain suspended in water long after the larger and denser particles of sand have deposited out. Shales are typically deposited in very slow moving water and are often found in lake and lagoonal deposits, in river deltas, on floodplains, and offshore of beach sands. Fossils, animal tracks/burrows, and even raindrop impact craters are sometimes preserved on shale bedding surfaces. Shales may also contain concretions. Shales that are subject to heat and pressure alter into a hard, fissile, and metamorphic material known as slate that is o ...

See also:

Shale, Shale - Formation

Read more here: » Shale: Encyclopedia II - Shale - Formation

clays: Encyclopedia II - Bedfordshire - History

See also main Bedfordshire history article The first recorded use of the name was in 1011 as "Bedanfordscir," meaning "Beda's ford" (river crossing). Bedfordshire was historically divided into the nine hundreds: Barford, Biggleswade, Clifton, Flitt, Manshead, Redbournestoke, Stodden, Willey, Wixamtree, along with the liberty and borough of Bedford. Luton was part of Bedfordshire until 1997, when it was made a unitary authority. However, it remains part of the ceremonial county of Bedfordshire, with a single ...

See also:

Bedfordshire, Bedfordshire - History, Bedfordshire - Geography and geology, Bedfordshire - Transport, Bedfordshire - Roads, Bedfordshire - Railways, Bedfordshire - Waterways, Bedfordshire - Air, Bedfordshire - Towns and villages, Bedfordshire - Places of interest

Read more here: » Bedfordshire: Encyclopedia II - Bedfordshire - History

clays: Encyclopedia II - River Glen Lincolnshire - History

The Nennius text, Historia Britonum, tells us that Arthur, the war leader of the Britons fought his first battle against the Anglo-Saxons the mouth of the River Glein [sic]. People have speculated about the battle's placement in several places, in Northumberland for example. However, the history of the Lincolnshire site fits the text well. This aerial photo shows the River Glen at Guthram, halfway between Twenty and West Pinchbeck. To the south, the Roman road across the fen lies hidden, buried in Baston Fen and Pichbeck Common ...

See also:

River Glen Lincolnshire, River Glen Lincolnshire - Naming, River Glen Lincolnshire - Geography, River Glen Lincolnshire - History, River Glen Lincolnshire - Reference

Read more here: » River Glen Lincolnshire: Encyclopedia II - River Glen Lincolnshire - History

clays: Encyclopedia II - Carbon - Notable characteristics

Carbon is a remarkable element for many reasons. Its different forms include one of the softest (graphite) and one of the hardest (diamond) substances known. Moreover, it has a great affinity for bonding with other small atoms, including other carbon atoms, and its small size makes it capable of forming multiple bonds. Because of these properties, carbon is known to form nearly ten million different compounds, the large majority of all chemical compounds. Carbon compounds form the basis of all life on Earth and the carbon-nitrogen cycle prov ...

See also:

Carbon, Carbon - Notable characteristics, Carbon - Applications, Carbon - Other uses, Carbon - History and Etymology, Carbon - Allotropes, Carbon - Occurrence, Carbon - Organic compounds, Carbon - Carbon chains, Carbon - Carbon cycle, Carbon - Isotopes, Carbon - Precautions

Read more here: » Carbon: Encyclopedia II - Carbon - Notable characteristics

clays: Encyclopedia II - Carbon - Allotropes

The allotropes of carbon are the different molecular configurations (allotropes) that pure carbon can take. The three relatively well-known allotropes of carbon are amorphous carbon, graphite, and diamond. Several exotic allotropes have also been synthesized or discovered, including fullerenes, carbon nanotubes, lonsdaleite and aggregated diamond nanorods. In its amorphous form, carbon is essentially graphite but not held in a crystalline macrostructure. It is, rather, present as a powder which is the main constituent of substances such as charcoal, la ...

See also:

Carbon, Carbon - Notable characteristics, Carbon - Applications, Carbon - Other uses, Carbon - History and Etymology, Carbon - Allotropes, Carbon - Occurrence, Carbon - Organic compounds, Carbon - Carbon chains, Carbon - Carbon cycle, Carbon - Isotopes, Carbon - Precautions

Read more here: » Carbon: Encyclopedia II - Carbon - Allotropes

clays: Encyclopedia II - Suffolk - History

Suffolk was part of the kingdom of East Anglia which was settled by the Angles in the 5th century. In 1974, Suffolk was split into five administrative districts, Suffolk Coastal, West Suffolk, Babergh, Forest Heath and Mid Suffolk with Suffolk Coastal's council based in Woodbridge, Babergh's in Hadleigh, Mid-Suffolk's in Needham Market, Forest Heath's in Mildenhall and West Suffolk's in Bury St Edmunds. There is also Waveney (with its council based in ...

See also:

Suffolk, Suffolk - History, Suffolk - Geology landscape and ecology, Suffolk - Demographics, Suffolk - Cities towns and villages, Suffolk - Places of interest, Suffolk - Notable people from Suffolk

Read more here: » Suffolk: Encyclopedia II - Suffolk - History

clays: Encyclopedia II - Sugar Land Texas - History

Sugar Land Texas - Sugar Land's founding. Sugar Land has a heritage tracing its roots back to the original Mexican land grant to Stephen F. Austin. One of the first settlers of the land, Samuel M. Williams, called this land "Oakland Plantation" because there were many different varieties of oaks on the land, such as Pin Oak, Post Oak, Water Oak, Red Oak, and Live Oak. Williams' brother, Nathaniel, purchased the land in 1838. They operated the plantation by growing cotton, corn, and sugarcane. During these early y ...

See also:

Sugar Land Texas, Sugar Land Texas - History, Sugar Land Texas - Sugar Land's founding, Sugar Land Texas - Company town, Sugar Land Texas - A city emerges, Sugar Land Texas - A decade of growth, Sugar Land Texas - The new millennium, Sugar Land Texas - Geography and climate, Sugar Land Texas - Geography, Sugar Land Texas - Geology, Sugar Land Texas - Climate, Sugar Land Texas - Economy, Sugar Land Texas - Law and government, Sugar Land Texas - Mayors, Sugar Land Texas - Demographics, Sugar Land Texas - People and culture, Sugar Land Texas - Famous people, Sugar Land Texas - Local attractions, Sugar Land Texas - Districts and communities, Sugar Land Texas - Architectural landmarks, Sugar Land Texas - Transportation, Sugar Land Texas - Major thoroughfares, Sugar Land Texas - Airport, Sugar Land Texas - Education, Sugar Land Texas - Colleges and universities, Sugar Land Texas - Public schools and libraries, Sugar Land Texas - Private schools, Sugar Land Texas - Media and entertainment, Sugar Land Texas - Newspapers

Read more here: » Sugar Land Texas: Encyclopedia II - Sugar Land Texas - History

clays: Encyclopedia II - Panspermia - Evidence

Until a large portion of the galaxy is surveyed for signs of life or contact is made with other civilizations, the panspermia hypothesis in its fullest meaning will remain difficult to test. There is, however, circumstantial evidence for exogenesis: Panspermia - Narrow time window for geogenesis. The Precambrian fossil record indicates that life appeared soon after the Earth was formed. Unless the Earth just happened to be the site of a large number of fortuitous coincidences, this would imply that life ap ...

See also:

Panspermia, Panspermia - The panspermia theory, Panspermia - Evidence, Panspermia - Narrow time window for geogenesis, Panspermia - Extremophiles, Panspermia - Wider range of potential habitats for life, Panspermia - Evidence of extraterrestrial life, Panspermia - Objections to panspermia and exogenesis, Panspermia - Directed panspermia, Panspermia - Science fiction

Read more here: » Panspermia: Encyclopedia II - Panspermia - Evidence

clays: Encyclopedia II - Sandstone - Origins

Sandstones are clastic in origin (as opposed to organic, like chalk or coal). They are formed from the cemented grains that may be fragments of a pre-existing rock, or else just mono-minerallic crystals. The cements binding these grains together are typically calcite, clays and silica. Grain sizes in sands are in the range of 0.1mm to 2mm. (Rocks with smaller grainsizes include siltstones and shales and are typically called argillaceous sediments, as are also clays. Rocks with larger grainsizes include both breccias and conglomerates and are ...

See also:

Sandstone, Sandstone - Origins, Sandstone - Types of sandstone, Sandstone - Basic References

Read more here: » Sandstone: Encyclopedia II - Sandstone - Origins

clays: Encyclopedia II - Ammonite - Shell anatomy and diversity

Ammonite - Basic shell anatomy. The chambered part of the ammonite shell is called a phragmocone. The phragmocone contains a series of progressively larger chambers, called camerae (sing. camera) that are divided by thin walls called septa (sing. septum). Only the last and largest chamber, the body chamber, was occupied by the living animal at any given moment. As it grew, it adde ...

See also:

Ammonite, Ammonite - Classification, Ammonite - Life, Ammonite - Shell anatomy and diversity, Ammonite - Basic shell anatomy, Ammonite - Sexual dimorphism, Ammonite - Variations in shape, Ammonite - The aptychus, Ammonite - Size, Ammonite - Ammonite distribution, Ammonite - Trivia, Ammonite - References and further reading

Read more here: » Ammonite: Encyclopedia II - Ammonite - Shell anatomy and diversity

clays: Encyclopedia II - Oceanic trench - Accretionary prisms and sediment transport

Accretionary prisms grow by frontal accretion, whereby sediments are scraped off, bulldozer-fashion, near the trench, or by underplating of subducted sediments and perhaps oceanic crust along the shallow parts of the subduction decollement. Frontal accretion over the life of a convergent margin results in younger sediments defining the outermost part of the accretionary prism and the oldest sediments defining the innermost portion. Older (inner) parts of the accretionary prism are much more lithified and have steeper structures than the youn ...

See also:

Oceanic trench, Oceanic trench - Geographic distribution, Oceanic trench - History of the term trench, Oceanic trench - Modern understanding of trenches, Oceanic trench - Morphologic expression, Oceanic trench - Filled trenches, Oceanic trench - Accretionary prisms and sediment transport, Oceanic trench - Water and biosphere, Oceanic trench - Empty trenches and subduction erosion, Oceanic trench - Controls on trench depth, Oceanic trench - Major oceanic trenches

Read more here: » Oceanic trench: Encyclopedia II - Oceanic trench - Accretionary prisms and sediment transport

clays: Encyclopedia II - Nitrogen cycle - Ammonia

Another source of ammonia is the decomposition of dead organic matter by bacteria called decomposers, which produce ammonium ions (NH4+). In well-oxygenated soil, these are then oxygenated first by bacteria into nitrite (NO2-) and then into nitrate. This conversion of ammonia into nitrate is called nitrification. Ammonia is highly toxic to fish life and the water discharge level of ammonia from wastewater treatment plants must often be closely monitored. To prevent loss of fish ...

See also:

Nitrogen cycle, Nitrogen cycle - The Basics, Nitrogen cycle - Ammonia, Nitrogen cycle - Ways to convert N2

Read more here: » Nitrogen cycle: Encyclopedia II - Nitrogen cycle - Ammonia

clays: Encyclopedia II - Chuvashia - Economy

Chuvashia is Russia’s center for hops growing and is famous throughout the country for its long history of beer brewing. It is also a major center for electrical engineering, especially in the area of power transmission and control systems. Other leading industries are metalworking, electricity generation, and chemical manufacturing. Chuvashia - Transportation. The transport network in Chuvashia is one of the most developed in Russia. The republic's system of roads, railr ...

See also:

Chuvashia, Chuvashia - Geography, Chuvashia - Time zone, Chuvashia - Natural resources, Chuvashia - Climate, Chuvashia - Administrative divisions, Chuvashia - Demographics, Chuvashia - History, Chuvashia - Politics, Chuvashia - Economy, Chuvashia - Transportation, Chuvashia - Culture, Chuvashia - Education

Read more here: » Chuvashia: Encyclopedia II - Chuvashia - Economy

clays: Encyclopedia II - Desert - Desert features

Sand covers only about 20 percent of Earth's deserts. Most of the sand is in sand sheets and sand seas—vast regions of undulating dunes resembling ocean waves "frozen" in an instant of time. In general, there are 6 forms of deserts: Mountain and basin deserts; Hamada deserts, which comprise of a plateaux landforms; Regs which consist of rock pavements; Ergs which are formed by sand seas; Intermontane Basins; and Badlands which are located at the margins of arid ...

See also:

Desert, Desert - Types of desert, Desert - Montane deserts, Desert - Desert features, Desert - Soils, Desert - Vegetation, Desert - Water, Desert - Mineral resources, Desert - List of deserts, Desert - Americas, Desert - Africa, Desert - Asia-Pacific, Desert - Other

Read more here: » Desert: Encyclopedia II - Desert - Desert features

clays: Encyclopedia II - Suffolk - History

Suffolk was part of the kingdom of East Anglia which was settled by the Angles in the 5th century. In 1974, Suffolk was split into five administrative districts, Suffolk Coastal, West Suffolk, Babergh, Forest Heath and Mid Suffolk with Suffolk Coastal's council based in Woodbridge, Babergh's in Hadleigh, Mid-Suffolk's in Needham Market, Forest Heath's in Mildenhall and West Suffolk's in Bury St Edmunds. There is also Waveney (with its council based in Lowestoft) and Ipswich Borough which is the administrative council controlling the c ...

See also:

Suffolk, Suffolk - History, Suffolk - Geology landscape and ecology, Suffolk - Demographics, Suffolk - Cities towns and villages, Suffolk - Places of interest, Suffolk - Notable people from Suffolk

Read more here: » Suffolk: Encyclopedia II - Suffolk - History

clays: Encyclopedia II - Mount Adams Washington - History

Native Americans in the area have created a detailed legend concerning the three smoking mountains that guard the Columbia River. According to their Bridge of the Gods tale, Wyeast (Mount Hood) and Pahto (Mount Adams; also called Paddo or Klickitat by natives) were the sons of Great Spirit. The brothers both competed for the love of the beautiful La-wa-la-clough (Mount St. Helens). When La-wa-la-clough chose Pahto, Wyeast struck his brother so hard that Pahto's head was flattened and Wyeast took La-wa-la-clough from him (thus attempting to e ...

See also:

Mount Adams Washington, Mount Adams Washington - History, Mount Adams Washington - Glaciers, Mount Adams Washington - Geology, Mount Adams Washington - Summit area, Mount Adams Washington - Area around Adams, Mount Adams Washington - Reference, Mount Adams Washington - External link

Read more here: » Mount Adams Washington: Encyclopedia II - Mount Adams Washington - History

clays: Encyclopedia II - Industrial minerals - Examples and applications

Typical examples of industrial rocks and minerals are limestone, clays, sand, gravel, diatomite, kaolin, bentonite, silica, barite, gypsum, and talc. Some examples of applications for industrial minerals are construction, ceramics, paints, electronics, filtration, plastics, glass, detergents and paper. In some cases, even organic materials (peat) and industrial products or by-products (cement, slag, silica fume) are categorized under industrial minerals, as well as metallic compounds mainly utilized in nonmetallic form (as an example most of the titani ...

See also:

Industrial minerals, Industrial minerals - Examples and applications, Industrial minerals - List of industrial minerals

Read more here: » Industrial minerals: Encyclopedia II - Industrial minerals - Examples and applications

clays: Encyclopedia II - Chlorite group - Members of the Chlorite group:

Clinoclore, penninite, and chamosite are the most common varieties. Several other sub-varieties have been described. The name chlorite is from the Greek chloros, meaning "green", in reference to its color. ...

See also:

Chlorite group, Chlorite group - Chlorite structure, Chlorite group - Occurrence, Chlorite group - Members of the Chlorite group:

Read more here: » Chlorite group: Encyclopedia II - Chlorite group - Members of the Chlorite group:

clays: Encyclopedia II - Extractive metallurgy - Mineral processing

Mineral processing involves the use of physical processes to manipulate ore particle size, and concentrate valuable minerals using the processes of separation, based on such properties of the ore, as density, chemical composition, electrostatic, magnetic or fluorescence properties. A good example of a separation process is froth flotation. Also of interest to the mineral processor is the separation of mineral solids from wate ...

See also:

Extractive metallurgy, Extractive metallurgy - Mineral processing, Extractive metallurgy - Pyrometallurgy, Extractive metallurgy - Hydrometallurgy

Read more here: » Extractive metallurgy: Encyclopedia II - Extractive metallurgy - Mineral processing

clays: Encyclopedia II - Weathering - Mechanical Physical Weathering

Mechanical weathering is the cause of the disintegration of rocks or wood. Most of the times it produces smaller angular fragments (like scree) as compared to chemical weathering. However, chemical and physical weathering often go hand in hand. For example, cracks exploited by mechanical weathering will increase the surface area exposed to chemical action. Furthermore, the chemical action at minerals in cracks can aid the disintegration pr ...

See also:

Weathering, Weathering - Mechanical Physical Weathering, Weathering - Exfoliation, Weathering - Freeze-thaw, Weathering - Pressure release, Weathering - Salt-crystal growth, Weathering - Organic Activity, Weathering - Abrasion, Weathering - Chemical Weathering, Weathering - Carbonation-solution, Weathering - Hydration, Weathering - Hydrolysis, Weathering - Oxidation, Weathering - Acids rain and plants

Read more here: » Weathering: Encyclopedia II - Weathering - Mechanical Physical Weathering

clays: Encyclopedia II - Limestone - Limestone landscape

Limestone is partially soluble, especially in acid, and therefore forms many erosion landforms. These include limestone pavements, pot holes, caves and gorges. Such erosion landscapes are known as karsts. Limestone is less resistant than most igneous rocks, but more resistant than most other sedimentary rocks. Limestone is therefore usually associated with hills and downland and occurs in regions with other sedimentary rocks, typically clays. Bands of limestone emerge from the Earth's surface in often spectacular rocky outcrops and is ...

See also:

Limestone, Limestone - Limestone landscape, Limestone - Uses of limestone

Read more here: » Limestone: Encyclopedia II - Limestone - Limestone landscape

clays: Encyclopedia II - Nitrogen cycle - Ammonia

Another source of ammonia is the decomposition of dead organic matter by bacteria called decomposers, which produce ammonium ions (NH4+). In well-oxygenated soil, these are then oxygenated first by bacteria into nitrite (NO2-) and then into nitrate. This conversion of ammonia into nitrate is called nitrification. Ammonia is highly toxic to fish life and the water discharge level of ammonia from wastewater treatment plants must often be closely monitored. To prevent loss of fish ...

See also:

Nitrogen cycle, Nitrogen cycle - The Basics, Nitrogen cycle - Ammonia, Nitrogen cycle - Conversion of N2

Read more here: » Nitrogen cycle: Encyclopedia II - Nitrogen cycle - Ammonia






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