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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 - Durdle Door - Geology

The arch has formed on a concordant coastline where bands of rock run parallel to the shoreline. Here the rock strata run near vertical, and the bands of rock are quite narrow. Originally a band of resistant Portland Limestone ran along the shore, the same band which can be seen two miles down the coast forming the narrow entrance to Lulworth Cove. Behind this is a 400 ft (120 metre) band of various weaker rocks which are easily eroded, and behind this is a stronger and much thicker band of chalk, which forms the Purbeck Hills. The limestone ...

See also:

Durdle Door, Durdle Door - Geology, Durdle Door - Tourism

Read more here: » Durdle Door: Encyclopedia II - Durdle Door - Geology

clays: Encyclopedia II - Salisbury Plain - History

Salisbury Plain is famous for its history. In Neolithic times there was an extensive population and much of the original vegetation had been cleared. The population was centred around the causeway camps of Whitesheet Hill and Robin Hood's Ball. By 2200 BC, Stonehenge and Avebury had become a focus for building, including a large quantity of round barrows and long barrows. Around 600 BC, large Bronze Age hill forts were constructed at Scratchbury and Battlesbury. Roman roads are visible features, probably serving a settlement near Old Sarum. Villas are sparse, however, and Anglo-Saxon place names suggest that the plain wa ...

See also:

Salisbury Plain, Salisbury Plain - History

Read more here: » Salisbury Plain: Encyclopedia II - Salisbury Plain - History

clays: Encyclopedia II - Sediment - Sediment transport

Sediment - Rivers and streams. If a fluid, such as water, is flowing, it can carry suspended particles. The settling velocity is the minimum velocity a flow must have in order to transport, rather than deposit, sediments, and (for a dilute suspension) is given by Stoke's Law: where w is the settling velocity, ρ is density (the subscripts p and f indicate particle and fluid respectively), g is the acceleration due to gravity, r is the radius of the particle and < ...

See also:

Sediment, Sediment - Sediment transport, Sediment - Rivers and streams, Sediment - Shores and shallow seas

Read more here: » Sediment: Encyclopedia II - Sediment - Sediment transport

clays: Encyclopedia II - Jurassic Coast - Formation

At the start of the Jurassic period a sea level rose flooding the Triassic landscape. For most of the Jurassic period Dorset was under a tropical sea, and marine life flourished. Sediments accumulated over time, mud in deep parts, sand in shallow parts, forming shale (Kimmeridge), limestone (Lulworth to Portland) and sandstone (Studland). The bodies of dead marine animals, including dinosaurs were preserved in these sediments. A large number of particularly high quality finds were uncovered at Kimmeridge and Lyme Regis. The waters slowly fell and dinosaur footp ...

See also:

Jurassic Coast, Jurassic Coast - Formation, Jurassic Coast - Features of interest, Jurassic Coast - Gateway towns

Read more here: » Jurassic Coast: Encyclopedia II - Jurassic Coast - Formation

clays: Encyclopedia II - Collecting fossils - Equipment

It is important to have the right kind of field equipment when looking for fossils, and safety should always be your primary concern. A hard hat is essential to protect you from loose stones which may be dislodged from cliffs above, but remember that this will not protect you from larger falling rocks. Hard hats are normally a requirement in operating quarries. Safety goggles and protective gloves are also essential. Rocks can be sharp and dangerous, safety goggles will protect your eyes from chips whil ...

See also:

Collecting fossils, Collecting fossils - Finding fossils, Collecting fossils - Collecting ethics, Collecting fossils - Field collecting, Collecting fossils - Equipment, Collecting fossils - Preservation and documentation

Read more here: » Collecting fossils: Encyclopedia II - Collecting fossils - Equipment

clays: Encyclopedia II - Karachay-Cherkessia - Geography

Karachay-Cherkessia - Time zone. Karachay-Cherkessia is located in the Moscow Time Zone (MSK/MSD). UTC offset is +0300 (MSK)/+0400 (MSD). Karachay-Cherkessia - Rivers. There are 172 rivers on the territory of the republic. Major rivers include: Aksaut River Bolshaya Laba River Bolshoy Zelenchuk River Daut River Kuban River Kuna River Kyafar River Laba River Maly Zelenchuk River < ...

See also:

Karachay-Cherkessia, Karachay-Cherkessia - Geography, Karachay-Cherkessia - Time zone, Karachay-Cherkessia - Rivers, Karachay-Cherkessia - Lakes, Karachay-Cherkessia - Mountains, Karachay-Cherkessia - Natural Resources, Karachay-Cherkessia - Climate, Karachay-Cherkessia - Administrative divisions, Karachay-Cherkessia - Demographics, Karachay-Cherkessia - History, Karachay-Cherkessia - Politics, Karachay-Cherkessia - Economy, Karachay-Cherkessia - maps

Read more here: » Karachay-Cherkessia: Encyclopedia II - Karachay-Cherkessia - Geography

clays: Encyclopedia II - Headlands and bays - Geology and geography

Headlands and bays are usually found together on the same stretch of coastline. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form where weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, granite) forming a headland, or peninsula. Wave refraction occurs on headlands concentrating wave energy on them, so many other landforms, such as caves, natural archs and stacks, f ...

See also:

Headlands and bays, Headlands and bays - Geology and geography, Headlands and bays - List of some well-known headlands, Headlands and bays - List of some well-known bays

Read more here: » Headlands and bays: Encyclopedia II - Headlands and bays - Geology and geography

clays: Encyclopedia II - Alum - Pliny's writings

The word "alumen," which we translate "alum," occurs in Pliny's Natural History. In the 15th chapter of his 35th book he gives a detailed description of it. By comparing this with the account of stupteria given by Dioscorides in the 123rd chapter of his 5th book, it is obvious that the two are identical. Pliny informs us that alumen was found naturally in the earth. He calls it salsugoterrae. Different substances were distinguished by the name of "alumen"; but they were all characterized by a certain degree of astringency, and ...

See also:

Alum, Alum - Alchemical and later discoveries and uses, Alum - Pliny's writings, Alum - Alum from alunite, Alum - Alum from clays or bauxite, Alum - Types of alum, Alum - Potash alum, Alum - Soda alum, Alum - Chrome alum, Alum - Ammonium alum, Alum - Alum solubility, Alum - Uses

Read more here: » Alum: Encyclopedia II - Alum - Pliny's writings

clays: Encyclopedia II - Dry cleaning - Process

A dry cleaning machine is somewhat similar to combination of a domestic washing machine, and clothes dryer. Garments are placed into a washing/extraction chamber (referred to as the "basket"). This is the core of the dry cleaning machine. The washing chamber contains a horizontal, perforated drum that rotates within an outer shell. The shell holds the solvent while the rotating drum holds the garment load. Depending on the size of the machine the basket capacity w ...

See also:

Dry cleaning, Dry cleaning - History, Dry cleaning - Solvents used, Dry cleaning - Modern, Dry cleaning - Historical, Dry cleaning - Process, Dry cleaning - Solvent processing, Dry cleaning - Dry Cleaning wastes, Dry cleaning - Cooked muck, Dry cleaning - Sludge, Dry cleaning - Environment

Read more here: » Dry cleaning: Encyclopedia II - Dry cleaning - Process

clays: Encyclopedia II - Geography of the United Kingdom - Physical geography

The physical geography of the UK varies greatly. It includes the chalk cliffs of Kent and Dorset, the rolling hills and fields of southeast England, the granite cliffs of Cornwall, the mountains of Wales, the uplands of the Peak District and the Pennines, the lakes and mountains of Cumbria, the Scottish lowlands, highlands and islands, and the fields, lakes and mountains of Northern Ireland. The country can be roughly divided into highland and lowland along the Tees-Exe line. The overall geomorphology of the UK was shaped by the comb ...

See also:

Geography of the United Kingdom, Geography of the United Kingdom - Physical geography, Geography of the United Kingdom - Geology, Geography of the United Kingdom - Mountains and hills, Geography of the United Kingdom - Rivers and lakes, Geography of the United Kingdom - Artificial waterways, Geography of the United Kingdom - Coastline, Geography of the United Kingdom - Islands, Geography of the United Kingdom - Climate, Geography of the United Kingdom - Human geography, Geography of the United Kingdom - Political geography, Geography of the United Kingdom - Demographics, Geography of the United Kingdom - Economic geography, Geography of the United Kingdom - Natural resources, Geography of the United Kingdom - Environment, Geography of the United Kingdom - Current issues, Geography of the United Kingdom - International agreements

Read more here: » Geography of the United Kingdom: Encyclopedia II - Geography of the United Kingdom - Physical geography

clays: Encyclopedia II - Hampshire - Physical geography

Hampshire's geology falls into two categories. In the south, along the coast is the "Hampshire Basin", an area of relatively non-resistant Eocene and Oligocene clays and gravels which are protected from sea erosion by the Isle of Purbeck, Dorset, and the Isle of Wight. These low, flat lands support heathland and woodland habitats, a large area of which form part of the New Forest. The New Forest has a mosaic of heathland, grassland, coniferous and deciduous woodland habitats that host diverse wildlife. The forest is protected as a national p ...

See also:

Hampshire, Hampshire - Physical geography, Hampshire - History, Hampshire - Economy, Hampshire - Demographics, Hampshire - Politics, Hampshire - Cities towns and villages, Hampshire - Culture arts and sport, Hampshire - Transport, Hampshire - Notes

Read more here: » Hampshire: Encyclopedia II - Hampshire - Physical geography

clays: Encyclopedia II - Houston Texas - History

Houston Texas - Houston's founding. In the mid-1800s, two brothers who were New York real estate promoters, John Kirby Allen and Augustus Chapman Allen, sought a location where they could begin building "a great center of government and commerce." In August 1836, they purchased 6,642 acres (27 km²) of land from T. F. L. Parrot, John Austin's widow, for $9,428. The Allen brothers named their town after Sam Houston and eventually persuad ...

See also:

Houston Texas, Houston Texas - History, Houston Texas - Houston's founding, Houston Texas - Early settlers, Houston Texas - 20th century, Houston Texas - The new millennium, Houston Texas - Geography and climate, Houston Texas - Geography, Houston Texas - Geology, Houston Texas - Climate, Houston Texas - Economy, Houston Texas - Government and politics, Houston Texas - Demographics, Houston Texas - People and culture, Houston Texas - A cosmopolitan city, Houston Texas - Health and fitness, Houston Texas - Cultural institutions, Houston Texas - Local attractions, Houston Texas - Architecture, Houston Texas - Downtown Houston, Houston Texas - Uptown Houston, Houston Texas - Districts and communities, Houston Texas - Healthcare and medical research, Houston Texas - Transportation, Houston Texas - Highways, Houston Texas - Mass transit, Houston Texas - Airports, Houston Texas - Education, Houston Texas - Colleges and universities, Houston Texas - Public schools and libraries, Houston Texas - Private schools, Houston Texas - Professional sports, Houston Texas - Media and entertainment, Houston Texas - Sister cities, Houston Texas - Sources

Read more here: » Houston Texas: Encyclopedia II - Houston Texas - History

clays: Encyclopedia II - Geology of Hampshire - Hampshire Basin

In the south, along the coast, soft Eocene and Oligocene clays and gravels form low flat terrain, the Hampshire Basin. Protected from sea erosion by the Isle of Purbeck, Dorset, and the Isle of Wight, this land supports heathland and woodland habitats, a large area of which form part of the New Forest. The New Forest has a mosaic of heathland, grassland, coniferous and deciduous woodland habitats that host diverse wildlife. The forest is protected as a national park, limiting development and agricultural use to protect the landscape and wild ...

See also:

Geology of Hampshire, Geology of Hampshire - Hampshire Basin, Geology of Hampshire - Chalk Downs

Read more here: » Geology of Hampshire: Encyclopedia II - Geology of Hampshire - Hampshire Basin

clays: Encyclopedia II - Geology of the Capitol Reef area - Jurassic events

Geology of the Capitol Reef area - Glen Canyon Group. All three formations of the Glen Canyon Group were laid down in the Mid to Late Triassic during a time of increasing aridity. Slightly clockwise and northward movement of the North American Plate was bringing the area into a dryer climatic belt. The direction of cross-bedding in Glen Canyon Group sand dunes suggests that prevailing winds from the north transported the sand into the region. Outcrops of the Glen Canyon Group's three formations are the most promi ...

See also:

Geology of the Capitol Reef area, Geology of the Capitol Reef area - Permian events, Geology of the Capitol Reef area - Cutler Group, Geology of the Capitol Reef area - Kaibab Limestone, Geology of the Capitol Reef area - Triassic events, Geology of the Capitol Reef area - Moenkopi Formation, Geology of the Capitol Reef area - Chinle Formation, Geology of the Capitol Reef area - Jurassic events, Geology of the Capitol Reef area - Glen Canyon Group, Geology of the Capitol Reef area - San Rafael Group, Geology of the Capitol Reef area - Morrison Formation, Geology of the Capitol Reef area - Cretaceous events, Geology of the Capitol Reef area - Cedar Mountain and Dakota Sandstone, Geology of the Capitol Reef area - Mancos Shale, Geology of the Capitol Reef area - Mesaverde Formation, Geology of the Capitol Reef area - Uplift and Cenozoic events, Geology of the Capitol Reef area - Waterpocket Fold and Lake Uinta, Geology of the Capitol Reef area - Volcanism, Geology of the Capitol Reef area - Erosion

Read more here: » Geology of the Capitol Reef area: Encyclopedia II - Geology of the Capitol Reef area - Jurassic events

clays: Encyclopedia II - Geology of the British Isles - Geological history

Geology of the British Isles - Proterozoic Era. The Gneisses, the oldest rocks in Britain or Ireland, date from at least 2,700 Ma (Ma = millions of years ago) in the Archean period of this era, the Earth itself being only about 4,600 Ma old. They are found in the far north west of Scotland and in the Hebrides, with a few small outcrops elsewhere. Formed from rock originally deposited at the surface of the planet, the rocks were later buried d ...

See also:

Geology of the British Isles, Geology of the British Isles - Geological history, Geology of the British Isles - Proterozoic Era, Geology of the British Isles - Paleozoic Era, Geology of the British Isles - Mesozoic Era, Geology of the British Isles - Cenozoic Era, Geology of the British Isles - Geological features, Geology of the British Isles - Geological resources, Geology of the British Isles - Events, Geology of the British Isles - Institutions, Geology of the British Isles - People, Geology of the British Isles - Awards

Read more here: » Geology of the British Isles: Encyclopedia II - Geology of the British Isles - Geological history

clays: Encyclopedia II - Flax - Cultivating flax

The major fibre flax-producing countries are the former USSR, Poland, France, Belgium and the Czech Republic. The soils most suitable for flax, besides the alluvial kind, are deep friable loams, and such as contain a large proportion of organic matter in their composition. Strong clays do not answer well, nor soils of a gravelly or dry sandy nature. But whatever be the kind of soil, it ought neither to be in too poor nor too rich a condition because, in the latter case, the flax is apt to grow too luxuriant and produce a coarse sort and, in the former case, the plant affords ...

See also:

Flax, Flax - Usage of Flax, Flax - Flax seed, Flax - Flax fiber, Flax - Cultivating flax, Flax - Dressing flax, Flax - Trivia

Read more here: » Flax: Encyclopedia II - Flax - Cultivating flax

clays: Encyclopedia II - Flax - Cultivating flax

The major fibre flax-producing countries are the former USSR, Poland, France, Belgium and the Czech Republic. The soils most suitable for flax, besides the alluvial kind, are deep friable loams, and such as contain a large proportion of organic matter in their composition. Strong clays do not answer well, nor soils of a gravelly or dry sandy nature. But whatever be the kind of soil, it ought neither to be in too poor nor too rich a condition because, in the latter case, the flax is apt to grow too luxuriant and produce a coarse sort and, in the former case, the plant affords ...

See also:

Flax, Flax - Usage of Flax, Flax - Cultivating flax, Flax - Dressing flax, Flax - Trivia

Read more here: » Flax: Encyclopedia II - Flax - Cultivating flax

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 - 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: i.Mountain and basin deserts; ii. Hamada deserts, which comprise of a plateaux landforms; iii. Regs which consist of rock pavements; iv. Ergs which are formed by sand seas; v. Intermontane Basins; and vi. 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 - Sakhalin - History

Sakhalin was inhabited in the Neolithic Stone Age. Flint implements, like those found in Siberia, have been found at Dui and Kusunai in great numbers, as well as polished stone hatchets, like European examples, primitive pottery with decorations like those of the Olonets, and stone weights for nets. Afterwards a population to whom bronze was known left traces in earthen walls and kitchen-middens on the Aniva Bay. The indigenous people of Sakhalin are the Xianbei and Xiazhe tribes, who had a way of life based on fishing. The Chinese in ...

See also:

Sakhalin, Sakhalin - History, Sakhalin - Geography, Sakhalin - Demographics, Sakhalin - Climate, Sakhalin - Flora and fauna, Sakhalin - Transportation, Sakhalin - Economy

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

clays: Encyclopedia II - Thallium - Applications

The odorless and tasteless thallium sulfate was widely used in the past as a rat poison and ant killer. In the United States and many other countries this use is no longer allowed due to safety concerns. Other uses: thallium sulfide's electrical conductivity changes with exposure to infrared light therefore making this compound useful in photocells. thallium bromide-iodide crystals have been used as infrared optical materials. thallium oxide has been used to manufacture glasses that have a high index of refract ...

See also:

Thallium, Thallium - Notable characteristics, Thallium - Applications, Thallium - History, Thallium - Occurrence, Thallium - Isotopes, Thallium - Precautions, Thallium - Famous uses

Read more here: » Thallium: Encyclopedia II - Thallium - Applications

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