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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] |
Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-bloc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead plant matter decays into peat and is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous ( Pennsylvanian) and Permian times. Many significant coal deposits are younger than this and originate from the Mesozoic and Cenozoic eras. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energy and over a third of its electricity. Some iron ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anglian Stage
The Anglian Stage is the name used in the British Isles for a middle Pleistocene glaciation. It precedes the Hoxnian Stage and follows the Cromerian Stage in the British Isles. The Anglian Stage is correlated to Marine Isotope Stage 12 (MIS 12), which started about 478,000 years ago and ended about 424,000 years ago. Lisiecki, L.E. (2005Ages of MIS boundaries. Boston MA:Boston University Description The Anglian stage has often been correlated to the Elsterian Stage of northern Continental Europe and the in the |
Tunnel Valley
A tunnel valley is a U-shaped valley originally cut under the glacial ice near the margin of continental ice sheets such as that now covering Antarctica and formerly covering portions of all continents during past glacial ages. They can be as long as , wide, and deep. Tunnel valleys were formed by subglacial erosion by water and served as subglacial drainage pathways carrying large volumes of meltwater. Their cross-sections often exhibit steep-sided flanks similar to fjord walls. They presently appear as dry valleys, lakes, seabed depressions, and as areas filled with sediment. If they are filled with sediment, their lower layers are filled primarily with glacial, glaciofluvial or glaciolacustrine sediment, supplemented by upper layers of temperate infill. They can be found in areas formerly covered by glacial ice sheets including Africa, Asia, North America, Europe, Australia and offshore in the North Sea, the Atlantic and in waters near Antarctica. Tunnel valleys appear in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Melverley
Melverley is a village in Shropshire, England, situated on the River Severn and the River Vyrnwy, near the Powys hills and the border with Wales. The population of the civil parish at the 2011 census was 156. The village, and the large rural area that surrounds it, was years ago famous for flooding from the nearby rivers but since the extensive defences being installed in Shrewsbury and improvements to the flood defences in and around the Melverley area flooding causes no problems for the majority of residents. It is a controlled flood area, meaning that water is allowed to flow across the open fields and held for a few hours until the river levels fall. Melverley Green is a small village to the north of Melverley. St Peter's Church The notable building in Melverley is the black and white timber-framed St Peter's Church which stands on the banks of the River Vyrnwy; it is one of only three such churches to be found in Shropshire and one of 27 in England and the oldest of its ... [...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 Boats
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] |
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] |
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] |
Industrial Revolution
The Industrial Revolution was the transition to new manufacturing processes in Great Britain, continental Europe, and the United States, that occurred during the period from around 1760 to about 1820–1840. This transition included going from hand production methods to machines, new chemical manufacturing and iron production processes, the increasing use of steam power and water power, the development of machine tools and the rise of the mechanized factory system. Output greatly increased, and a result was an unprecedented rise in population and in the rate of population growth. Textiles were the dominant industry of the Industrial Revolution in terms of employment, value of output and capital invested. The textile industry was also the first to use modern production methods. The Industrial Revolution began in Great Britain, and many of the technological and architectural innovations were of British origin. By the mid-18th century, Britain was the world's leadi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ironbridge Gorge Museum Trust
The Ironbridge Gorge Museum Trust is an industrial heritage organisation which runs ten museums and manages multiple historic sites within the Ironbridge Gorge World Heritage Site in Shropshire, England, widely considered as the birthplace of the Industrial Revolution. The Gorge includes a number of settlements important to industrial history and with heritage assets, including Ironbridge, Coalport and Jackfield along the River Severn, and also Coalbrookdale and Broseley. The area was among the first sites in the United Kingdom to be declared a World Heritage Site by UNESCO in 1986. Museums The ten museum sites run by the Trust, collectively known as The Ironbridge Gorge Museums are: # Blists Hill Victorian Town, including the Hay Inclined Plane # Broseley Pipeworks # Coalbrookdale Museum of Iron # Coalport China Museum # Tar Tunnel # Darby Houses # Enginuity # Iron Bridge and Tollhouse # Jackfield Tile Museum # Museum of the Gorge The Trust The Ironbridge Gorge Museum Tr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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