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Morton And Hanthorpe
__NOTOC__ Morton and Hanthorpe is a civil parish, formerly known as Morton by Bourne in the South Kesteven district of Lincolnshire, England. It is situated north from Bourne, and south-east from Grantham. According to the 2011 Census the parish had a population of 2,406. History The village is in two parts, one each side of the fen-edge road, the A15. To the fenward side is Morton and to the upland side is Hanthorpe. The earlier name is that of Morton which will come from the acid peat land which the Anglian settlers found in the fen in around the year 500. The name therefore indicates that the fen was to a significant extent better called the bog in modern terminology. They were Germanic speakers so they called it a moor. Hanthorpe is a name indicating a subsidiary settlement established in the period of the Danish settlements, probably in the tenth century. The church and the later signs of the manorial centre are in Morton. The church is built in the Early English ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Kesteven
South Kesteven is a Non-metropolitan district, local government district in Lincolnshire, England, forming part of the traditional Kesteven division of the county. It covers Bourne, Lincolnshire, Bourne, Grantham, Market Deeping and Stamford, Lincolnshire, Stamford. The 2011 census reports 133,788 people at 1.4 per hectare in 57,344 households. The district borders the counties of Cambridgeshire, Leicestershire, Northamptonshire, Nottinghamshire and Rutland. It is also bounded by the Lincolnshire districts of North Kesteven and South Holland, Lincolnshire, South Holland. History The district was formed on 1 April 1974, under the Local Government Act 1972, from the municipal boroughs of Grantham and Stamford, along with Bourne Urban District, South Kesteven Rural District, and West Kesteven Rural District. Previously the district was run by Kesteven County Council, based in Sleaford. Geography South Kesteven borders North Kesteven to the north, as far east as Horbling, where the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Creek (tidal)
A tidal creek or tidal channel is a narrow inlet or estuary that is affected by the ebb and flow of ocean tides. Thus, it has variable salinity and electrical conductivity over the tidal cycle, and flushes salts from inland soils. Tidal creeks are characterized by slow water velocity, resulting in buildup of fine, organic sediment in wetlands. Creeks may often be a dry to muddy channel with little or no flow at low tide, but with significant depth of water at high tide. Due to the temporal variability of water quality parameters within the tidally influenced zone, there are unique biota associated with tidal creeks which are often specialised to such zones. Nutrients and organic matter are delivered downstream to habitats normally lacking these, while the creeks also provide access to inland habitat for salt-water organisms. Terminology A "creek" normally refers to a tidal water channel in British English and in other parts of the Anglosphere. This is the case in many countries ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Terrington Beds
Terrington is a large village and civil parish in the Ryedale district of North Yorkshire, England. It is situated in the Howardian Hills, west of Malton. History The village is mentioned four times in the ''Domesday Book'' as ''Teurintone''. The lands were divided between the manors of ''Bulmer'' and ''Foston''. At the time of the time of Norman conquest, lands in the manor were held by ''Ligulf'', ''Northmann'', '' Earl Morcar'', ''Earl Waltheof'' and ''Gamal, son of Karli''. Afterwards the lands were granted to ''Robert, Count of Mortain'', ''Count Alan of Brittany'' and ''Berengar of Tosny''. The manor was held soon after by ''Niel Fossard'' and then followed the descent of the manor of nearby Sheriff Hutton. Other lands were tenanted in the 13th century by the ''Latimer'' family and followed the descent of his manor at Danby until the 16th century. The manor was not held in demesne like other manors. In 1427 the manor was held by the lord of Sessay manor, Edmund Darell, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay particles, but become hard, brittle and non–plastic upon drying or firing. Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. Clay is the oldest known ceramic material. Prehistoric humans discovered the useful properties of clay and used it for making pottery. Some of the earliest pottery shards have been dated to around 14,000 BC, and clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oxidation
Redox (reduction–oxidation, , ) is a type of chemical reaction in which the oxidation states of substrate change. Oxidation is the loss of electrons or an increase in the oxidation state, while reduction is the gain of electrons or a decrease in the oxidation state. There are two classes of redox reactions: * ''Electron-transfer'' – Only one (usually) electron flows from the reducing agent to the oxidant. This type of redox reaction is often discussed in terms of redox couples and electrode potentials. * ''Atom transfer'' – An atom transfers from one substrate to another. For example, in the rusting of iron, the oxidation state of iron atoms increases as the iron converts to an oxide, and simultaneously the oxidation state of oxygen decreases as it accepts electrons released by the iron. Although oxidation reactions are commonly associated with the formation of oxides, other chemical species can serve the same function. In hydrogenation, C=C (and other) bonds ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muck (soil)
A sapric is a subtype of a histosol where virtually all of the organic material has undergone sufficient decomposition to prevent the identification of plant parts. Muck is a sapric soil that is naturally waterlogged or is artificially drained. Classification The soils are deep, dark colored, and friable, often underlain by marl, or marly clay. World Reference Base The World Reference Base for Soil Resources (WRB) defines "sapric" (sa) as a histosol having less than one-sixth (by volume) of the organic material consisting of recognizable plant tissue within 100 cm of the soil surface. Canada Muck soils fall under the Organic Order in the Canadian system of soil classification. Muck soils are organic soils, with at minimum of 30% organic matter and a depth of at least 40 cm. United States In the USDA soil taxonomy, sapric may be a subtype of a haplohemist or glacistel type, and may also be a diagnostic organic soil material where the fiber content is less than one-sixth of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Drift
In geology, drift is a name for all sediment (clay, silt, sand, gravel, boulders) transported by a glacier and deposited directly by or from the ice, or by glacial meltwater. Drift is often subdivided into (unsorted and) unstratified drift (glacial till) that forms moraines and stratified drift (glaciolacustrine and fluvioglacial sediments) that accumulates as stratified and sorted sediments in the form of outwash plains, eskers, kames, varves, and so forth. The term drift clay is a synonym for boulder clay. Both are archaic terms for glacial tills with a fine-grained matrix.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds., 2005. ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. In the United Kingdom, drift is also applied as a general term for all surficial, unconsolidated, rock debris and sediment that is moved from one place to accumulate in another and mapped separately or otherwise diffrerentiated from underlying bedroc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
First Terrace Gravel
First or 1st is the ordinal form of the number one (#1). First or 1st may also refer to: *World record, specifically the first instance of a particular achievement Arts and media Music * 1$T, American rapper, singer-songwriter, DJ, and record producer Albums * ''1st'' (album), a 1983 album by Streets * ''1st'' (Rasmus EP), a 1995 EP by The Rasmus, frequently identified as a single * '' 1ST'', a 2021 album by SixTones * ''First'' (Baroness EP), an EP by Baroness * ''First'' (Ferlyn G EP), an EP by Ferlyn G * ''First'' (David Gates album), an album by David Gates * ''First'' (O'Bryan album), an album by O'Bryan * ''First'' (Raymond Lam album), an album by Raymond Lam * ''First'', an album by Denise Ho Songs * "First" (Cold War Kids song), a song by Cold War Kids * "First" (Lindsay Lohan song), a song by Lindsay Lohan * "First", a song by Everglow from ''Last Melody'' * "First", a song by Lauren Daigle * "First", a song by Niki & Gabi * "First", a song by Jonas Brot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cornbrash
The Cornbrash Formation is a Middle Jurassic geological formation in England. It ranges in age from Bathonian to Callovian, the uppermost part of the Middle Jurassic. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. The name Cornbrash is an old English agricultural name applied in Wiltshire to a variety of loose rubble or brash which, in that part of the country, forms a good soil for growing corn. The name was adopted by William Smith for a thin band of shelly limestone which, in the south of England, breaks up in the manner indicated. Although only a thin group of rocks (10–25 feet c. 3–7 m), it is remarkably persistent; it may be traced from Weymouth to the Yorkshire coast, but in north Lincolnshire it is very thin, and probably dies out in the neighborhood of the Humber. It appears again, however, as a thin bed in Gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kellaways Formation
The Kellaways Formation is a geological formation of the Callovian Series from the Jurassic. It is found in the British Isles, immediately above the Great Oolite Series: below the Oxford Clay Formation and above the Cornbrash. It consists of two layers, the Kellaways Sand, a light green-grey clayish silt and sand with layers of sand concretions, overlying the Kellaways Clay, a dark grey plastic fissile clay. They were laid down during the Callovian, offshore from the London-Brabant Island, between 165 and 160 million years ago, in the latitude of the modern Mediterranean Sea, when the structure of Britain was still taking shape. At this stage, the coal swamps of the north-western shore of the island had subsided below the sea so that the Kellaways clay was formed in fairly deep water and the Kellaways sand was blown and washed from what had become the hot desert land. The holotype of the indeterminate eusauropod ''"Ornithopsis" leedsii'' has been recovered from this formation.N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
