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Newport, Shropshire
Newport is a constituent market town in Telford and Wrekin in Shropshire, England. It lies north of Telford, west of Stafford, and is near the Shropshire-Staffordshire border. The 2001 census recorded 10,814 people living in the town's parish, which rose to 11,387 by the 2011 census. Toponym The Normans planned a new town called Novus Burgus roughly on the Anglo-Saxon settlement of Plesc. The first market charter was granted by Henry I, and over time the name changed from Novus Burgus, to Nova Porta, to Newborough and finally to Newport in about 1220. Location The site was chosen partly because of its location near the Via Devana (Roman Road, which ran from Colchester to Chester), and partly because of the number of fisheries (which are mentioned in the Domesday Survey). The River Meese, which flows from Aqualate Mere, lies to the north of the town. Newport sits on a sandstone ridge on the eastern border of the Welsh Marches and west of the Aqualate Mere, the largest natu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Telford And Wrekin
Telford and Wrekin is a borough and unitary authority in Shropshire, England. In 1974, a non-metropolitan district of Shropshire was created called The Wrekin. In 1998, the district became a unitary authority and was renamed "Telford and Wrekin", which remains part of the Shropshire ceremonial county and shares institutions such as the Fire and Rescue Service and Community Health with the rest the county. The borough's major settlement is Telford, which was designated a "new town" in the 1960s and incorporated the towns of Dawley, Madeley, Oakengates, and Wellington. After the Telford conurbation, which includes the aforementioned towns, the next-largest settlement is Newport which is located in the northeast of the borough and isn't part of the original new town of Telford. The borough borders Staffordshire, but is surrounded by the unitary district of Shropshire which covers the area previously administrated by Shropshire County Council. History The district was created on ... [...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] |
Edgmond
Edgmond is a village in the borough of Telford and Wrekin and ceremonial county of Shropshire, England. The village population at the 2011 Census was 2,062. It lies north-west of the town of Newport. The village has two pubs (the Lion and the Lamb), a Methodist chapel and hall (neither of which are in use), a village hall, and a village shop with a co-located post office. There is a recreation field called simply "The Playing Fields", where there are Sunday cricket games, pub football matches, and a playground for young children. The village also has many areas for walking and biking including an area called the Rock Hole, an old sandstone quarry from which the rock used to build the local church was taken . Also popular is the canal walk, which leads down to the local town of Newport along the old canals. The canals are now often used for fishing competitions. There has been much speculation about the possibility of reopening the old Shrewsbury and Newport Canal route. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harper Adams University
Harper Adams University, founded in 1901 as Harper Adams College, is a public university located close to the village of Edgmond, near Newport, in Shropshire, England. Established in 1901, the college is a specialist provider of higher education for the agricultural and rural sector. It gained university college status in 1998, and university status in 2012 when the requirements were relaxed. The university provides more than 50 foundation, undergraduate and postgraduate degree programmes to students from over 30 countries. The university is set within a 550 hectare (1360 acre) working farm. History Harper Adams College, which would become the university, was founded in 1901. Its first Principal was Headworth Foulkes (1901–1922). Thomas Harper Adams, a wealthy Shropshire gentleman farmer, died in 1892, bequeathing the estate which was the original foundation. The college had just six students to begin with. In 1909 a specialist poultry husbandry was created. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Log Boat
A dugout canoe or simply dugout is a boat made from a hollowed tree. Other names for this type of boat are logboat and monoxylon. ''Monoxylon'' (''μονόξυλον'') (pl: ''monoxyla'') is Greek – ''mono-'' (single) + '' ξύλον xylon'' (tree) – and is mostly used in classic Greek texts. In German, they are called Einbaum ("one tree" in English). Some, but not all, pirogues are also constructed in this manner. Dugouts are the oldest boat type archaeologists have found, dating back about 8,000 years to the Neolithic Stone Age. This is probably because they are made of massive pieces of wood, which tend to preserve better than others, such as bark canoes. Along with bark canoes and hide kayaks, dugouts were also used by Indigenous peoples of the Americas. Construction Construction of a dugout begins with the selection of a log of suitable dimensions. Sufficient wood must be removed to make the vessel relatively light in weight and buoyant, yet still strong enough to supp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Shropshire
North Shropshire was a local government district in Shropshire, England from 1974 to 2009. The district council was based at Edinburgh House in Wem. Other settlements included the towns of Ellesmere, Market Drayton, Wem and Whitchurch, as well as the large villages of Shawbury and Baschurch. The district bordered onto Wales, Cheshire and Staffordshire as well as the Shropshire districts of Oswestry, Shrewsbury and Atcham and the unitary Telford and Wrekin. History The district was formed on 1 April 1974, under the Local Government Act 1972, by a merger of Market Drayton Rural District and North Shropshire Rural District. The district and its council were abolished on 1 April 2009, when the new Shropshire Council unitary authority was established, as part of the 2009 structural changes to local government in England. Settlements The district council classified Wem, Market Drayton, Whitchurch and Ellesmere as the market towns of North Shropshire, while it gave the classific ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Lapworth
Lake Lapworth was a postulated glacial lake in Great Britain, believed to have formed during the Last Glacial Period, last ice age when glaciers ended the northern outlet of the River Severn, Severn. This ran through the River Dee, Wales, Dee (which passes by Chester). At some point or points it ran into glaciers and backed up to form a resultant lake. This overflowed southwards cutting the Ironbridge Gorge, near Telford in Shropshire. This permanently diverted most of the Severn drainage basin to its current basin which flows south. Etymology The lake was named in 1924 by Leonard Johnston Wills for the late Charles Lapworth ( 1920), who suggested its existence in 1898. Frederic William Harmer (1835-1923) proposed the same causation and timing in 1907 having considered glacial lake sediments found on the Shropshire Plain. Geography and geology Lake Lapworth is one of several glacial lakes that are thought to have existed during the Ice Age in the late Pleistocene. This was the geol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Welsh Marches
The Welsh Marches ( cy, Y Mers) is an imprecisely defined area along the border between England and Wales in the United Kingdom. The precise meaning of the term has varied at different periods. The English term Welsh March (in Medieval Latin ''Marchia Walliae'') was originally used in the Middle Ages to denote the marches between England and the Principality of Wales, in which Marcher lords had specific rights, exercised to some extent independently of the king of England. In modern usage, "the Marches" is often used to describe those English counties which lie along the border with Wales, particularly Shropshire and Herefordshire, and sometimes adjoining areas of Wales. However, at one time the Marches included all of the historic counties of Cheshire, Shropshire, Herefordshire, Worcestershire and Gloucestershire. In this context the word ''march'' means a border region or frontier, and is cognate with the verb "to march," both ultimately derived from Proto-Indo-European ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aqualate Mere
Aqualate Mere, in Staffordshire, is the largest natural lake in the English Midlands and is managed as a national nature reserve (NNR) by Natural England. The Mere lies within the borough of Stafford in Staffordshire, England, some east of the market town of Newport, Shropshire. It is within the grounds of Aqualate Hall, a country house, with a landscaped deer park. Although large in extent (1.5 km long and 0.5 km wide), the Mere is remarkably shallow and is nowhere much more than one metre (3.3 ft) deep. Aqualate Mere is an example of an esker system (rare in the Midlands) formed by glacial meltwaters during the late Devensian glaciation. The depression in which the Mere lies, thought to be a kettle hole, and the surrounding higher ground which comprises glacial sand and gravel deposits were all formed at the same time. It is fed by streams coming from the north, south and east (including Back Brook), and its outflow to the west forms the River Meese which joi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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