|
Geology Of Cheshire
The geology of Cheshire in England consists mainly of Triassic sandstones and mudstones. To the north west of Cheshire, these rocks are heavily faulted and the underlying Carboniferous Coal Measures are thrown up. Around the areas of Poynton and Macclesfield, the coal is close to the surface and was easily mined. Below the Coal Measures is the Millstone Grit, which appears towards the Derbyshire border on the flanks of the Peak District dome. The Cheshire Basin is a major sedimentary basin which comprises the larger part of the county. This fault-bounded half-graben structure is bounded to the east and southeast by a series of faults of which the most significant is the Red Rock Fault. Numerous faults trend north-south through the basin, some of which help to define the series of hills which are known collectively as the Mid Cheshire Ridge. The basin was flooded on several occasions in the Permian and early Triassic periods resulting in the laying down of massive halite (salt) be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Red Rock Fault
The Wem-Bridgemere-Red Rock Fault System is a complex zone of intersecting faults which defines the eastern boundary of the Cheshire Basin, a deep sedimentary basin in the northwest of England and extending south into the northern Midlands. It includes the Red Rock Fault, Bridgemere Fault and Wem Fault and reaches from Shropshire through eastern Cheshire to southeast Lancashire.Plant et al. (eds) 1999 ''The Cheshire Basin: basin evolution , fluid movement and mineral resources in a Permo-Triassic rift setting''. British Geological Survey At Norbury Brook, Poynton, on the border of Cheshire and Greater Manchester, the Millstone Grit of the Pennines makes a downfall to be covered to the west by the glacial tills of the Cheshire Plain, formed by the retreating ice age glaciers. To the east of the fault there are the coal measures of the Carboniferous period, which unlike those in the Lancashire Coalfield are missing the top layers. Here there are outcrops of the Middle Coal Measur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chester
Chester is a cathedral city and the county town of Cheshire, England. It is located on the River Dee, close to the English–Welsh border. With a population of 79,645 in 2011,"2011 Census results: People and Population Profile: Chester Locality"; downloaded froCheshire West and Chester: Population Profiles, 17 May 2019 it is the most populous settlement of Cheshire West and Chester (a unitary authority which had a population of 329,608 in 2011) and serves as its administrative headquarters. It is also the historic county town of Cheshire and the second-largest settlement in Cheshire after Warrington. Chester was founded in 79 AD as a "castrum" or Roman fort with the name Deva Victrix during the reign of Emperor Vespasian. One of the main army camps in Roman Britain, Deva later became a major civilian settlement. In 689, King Æthelred of Mercia founded the Minster Church of West Mercia, which later became Chester's first cathedral, and the Angles extended and strengthene ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alderley Edge
Alderley Edge is a village and civil parish in Cheshire, England. In 2011, it had a population of 4,780. Alderley Edge is northwest of Macclesfield and south of Manchester, at the base of a steep and thickly wooded sandstone escarpment, Alderley Edge, which is the area's chief topographical feature and overlooks the Cheshire Plain. Alderley Edge is known for its affluence and expensive houses, falling inside Cheshire's Golden Triangle. Alderley Edge has a selection of cafes and designer shops and has attracted numerous Premier League footballers, actors and multi-millionaire businesspeople. It is one of the most expensive and sought-after places to live in the UK outside central London. History The area around Alderley Edge provides proof of occupation since the Mesolithic period with flint implements being found along the line of the sandstone outcrop. Evidence of copper mining in the Bronze Age has also been found to the south of the area. In 1995 members of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheshire Plain
The Cheshire Plain is a relatively flat expanse of lowland within the county of Cheshire in North West England but extending south into Shropshire. It extends from the Mersey Valley in the north to the Shropshire Hills in the south, bounded by the hills of North Wales to the west and the foothills of the Pennines to the north-east. The Wirral Peninsula lies to the north-west whilst the plain merges with the South Lancashire Plain in the embayment occupied by Manchester to the north. In detail, the plain comprises two areas with distinct characters, the one to the west of the Mid Cheshire Ridge and the other, larger part, to its east. The plain is the surface expression of the Cheshire Basin, a deep sedimentary basin that extends north into Lancashire and south into Shropshire. It assumed its current form as the ice-sheets of the last glacial period melted away between 20,000 and 15,000 years ago leaving behind a thick cover of glacial till and extensive tracts of glacio-flu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flintshire Coalfield
The Flintshire Coalfield in north-east Wales is one of the smaller Great Britain, British coalfields. It is in the county of Flintshire and extends from the Point of Ayr in the north, along the Dee Estuary through Connah's Quay to Caergwrle in the south. A small part extends onto the Wirral Peninsula, Wirral i.e. England, English coast of the estuary at Neston, Cheshire which was the site of a coalmine for a period. The coal-bearing stratum, strata continue southwards of Caergwrle as the Denbighshire Coalfield. Together the two coalfields are known as the North Wales Coalfield. Geology Several coal seams are named in the sequence. Some seams are absent in the northern part of the coalfield and are labelled as (S) whilst the others occur across the coalfield as a whole. The Chwarelau Seam which appears only in the north actually occurs within the underlying Millstone Grit sequence rather than the Coal Measures proper. The seams are listed stratigraphically with the uppermost (young ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neston
Neston is a town and civil parish on the Wirral Peninsula, in Cheshire, England. It is part of the unitary authority of Cheshire West and Chester. The village of Parkgate is located to the north west and the villages of Little Neston and Ness are to the south of Neston. At the 2001 census the population of Neston ward was recorded as 3,521, increasing to 4,329 at the 2011 census. The civil parish also includes Little Neston, Parkgate, Willaston and part of Burton and Ness, and had a population of 15,162 in 2001, increasing to 15,221 in 2011. History The name is of Viking origin, deriving from the Old Norse ''Nes-tún'', meaning 'farmstead or settlement at/near a promontory or headland'. Another Nesttun town can be found near Bergen, Norway. It is also mentioned in the Domesday Book as ''Nestone'' under the ownership of a William Fitznigel, with a population of eight households. Civic history A royal charter was granted to Neston in 1728 in support of its status as a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newbold Astbury
Newbold Astbury (often just Astbury) is a village and civil parish in the unitary authority of Cheshire East and the ceremonial county of Cheshire, in the north-west of England. Newbold Astbury is situated to the south-west of Congleton on the A34 road to Scholar Green; the A34 forms one side of the triangular village green. The civil parish holds a combined parish council meeting with the adjacent civil parish of Moreton-cum-Alcumlow, which is consequently called Newbold Astbury-cum-Moreton Parish Council. History Newbold Astbury is mentioned in the Domesday book as belonging to Gilbert de Venables in 1086 having previously belonged to Wulfgeat of Madeley in 1066. In 1066 the annual value was 1 pound income for its lord but in 1086 it was just 8 shillings possibly due to the Harrying of the North. For its households In 1086 the manor had 3 villagers, 2 smallholders, 1 priest (meaning it also had a church), and one rider. For its ploughlands in 1086 it had 4 ploughlands, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous Limestone
Carboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain and Ireland that were deposited during the Dinantian Epoch of the Carboniferous Period. These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones and some thin sandstones, is known as the Carboniferous Limestone Supergroup. Depositional basins Within Great Britain the suite of rocks known traditionally as the Carboniferous Limestone Series was deposited as marine sediments in three distinct ‘provinces’ separated by contemporary landmasses. One of these landmasses was the Wales-London-Brabant Massif, an east–west aligned belt of land stretching through central Wales and the English Midlands to East Anglia and on into Belgium. The limestones deposited to its south form a distinct South Wales-Mendip province which extends from Pembrokeshire in the west through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheshire Meres
Cheshire ( ) is a ceremonial and historic county in North West England, bordered by Wales to the west, Merseyside and Greater Manchester to the north, Derbyshire to the east, and Staffordshire and Shropshire to the south. Cheshire's county town is the cathedral city of Chester, while its largest town by population is Warrington. Other towns in the county include Alsager, Congleton, Crewe, Ellesmere Port, Frodsham, Knutsford, Macclesfield, Middlewich, Nantwich, Neston, Northwich, Poynton, Runcorn, Sandbach, Widnes, Wilmslow, and Winsford. Cheshire is split into the administrative districts of Cheshire West and Chester, Cheshire East, Halton, and Warrington. The county covers and has a population of around 1.1 million as of 2021. It is mostly rural, with a number of towns and villages supporting the agricultural and chemical industries; it is primarily known for producing chemicals, Cheshire cheese, salt, and silk. It has also had an impact on popular culture, producin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northwich
{{Infobox UK place , static_image_name = Northwich - Town Bridge.jpg , static_image_caption = Town Bridge, the River Weaver and the spire of Holy Trinity Church , official_name = Northwich , country = England , region = North West England , population = 50,531 , population_ref = (2021){{NOMIS2021 , id=E35001305 Overview Profile: Northwich Town Council"; downloaded fro.gov.uk/find_out_more/datasets_and_statistics/statistics/census_2011/population_profiles Cheshire West and Chester: Population Profiles 16 May 2019 , os_grid_reference = SJ651733 , coordinates = {{coord, 53.259, -2.518, display=inline,title , post_town = NORTHWICH , postcode_area = CW , postcode_district = CW8,CW9 , dial_code = 01606 , constituency_westminster = Weaver Vale , constituency_westminster1 = Tatton , civil_pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brine
Brine is a high-concentration solution of salt (NaCl) in water (H2O). In diverse contexts, ''brine'' may refer to the salt solutions ranging from about 3.5% (a typical concentration of seawater, on the lower end of that of solutions used for brining foods) up to about 26% (a typical saturated solution, depending on temperature). Brine forms naturally due to evaporation of ground saline water but it is also generated in the mining of sodium chloride. Brine is used for food processing and cooking (pickling and brining), for de-icing of roads and other structures, and in a number of technological processes. It is also a by-product of many industrial processes, such as desalination, so it requires wastewater treatment for proper disposal or further utilization (fresh water recovery). In nature Brines are produced in multiple ways in nature. Modification of seawater via evaporation results in the concentration of salts in the residual fluid, a characteristic geologic deposit call ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
