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Darlaston All Saints F
Darlaston is an industrial town, industrial town in the Metropolitan Borough of Walsall in the West Midlands (county), West Midlands of England. It is located near Bilston, Walsall, Wednesbury, Willenhall and Tipton. It was historically part of Staffordshire. Topography Darlaston is situated between Wednesbury and Walsall in the valley of the River Tame, West Midlands, River Tame in the angle where the three major head-streams of the river converge. It is located on the South Staffordshire coalfield and has been an area of intense coal-mining activity. The underlying coal reserves were most likely deposited in the Carboniferous Period. Disused coal mines are found near Queen Street in Moxley, behind Pinfold Street JMI School, near Hewitt Street and Wolverhampton Street, in George Rose Park, and behind the police station in Victoria Park. Mining subsidence, which has taken its toll on many buildings across central England, has also made its mark in Darlaston. In 1999, a council ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Darlaston Loop
The Darlaston Loop was a railway which connected the towns of Walsall, Darlaston and Wednesbury in the West Midlands (county), West Midlands of England. It was so named because it passed through the town of Darlaston. Opening The line was opened in 1863 to bypass the recently constructed railway through Walsall. It operated as a single track until a second track was added in 1872, and the only Darlaston railway station (1863–1887), station on the line was located in Darlaston town centre. Closure It closed in 1887 but the line remained open to goods trains for another 80 years or so, when it finally closed during the 1960s. The site today A public footpath has been created along some of the trackbed, including the section which passed through Darlaston Station although the section to Wednesbury Town is now built on by both industrial and housing. A disused railway building stood on Crescent Road nearly 50 years after falling into disuse. References [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wednesbury
Wednesbury ( ) is a market town in the Sandwell district, in the county of the West Midlands (county), West Midlands, England; it was historically in Staffordshire. It is located near the source of the River Tame, West Midlands, River Tame and is part of the Black Country. Wednesbury is situated 5 miles (8km) south-east of Wolverhampton, 3 miles (4.4km) south-west of Walsall and 7 miles (11.8km) north-west of Birmingham. At the United Kingdom 2021 Census, 2021 Census, the town's built-up area had a population of 20,313. History Medieval and earlier The substantial remains of a large ditch excavated in St Mary's Road in 2008, following the contours of the hill and predating the Early Medieval period, has been interpreted as part of a hilltop enclosure and possibly the Iron Age hillfort long suspected on the site. The first authenticated spelling of the name was Wodensbyri, written in an endorsement on the back of the copy of the will of Wulfric Spot, dated 1004. Wednesbury (" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Birmingham Canal Navigations
Birmingham Canal Navigations (BCN) is a network of canals connecting Birmingham, Wolverhampton, and the eastern part of the Black Country. The BCN is connected to the rest of the English canal system at several junctions. It was owned and operated by the Birmingham Canal Navigation Company from 1767 to 1948. At its working peak, the BCN contained about 160 miles (257 km) of canals; today just over 100 miles (160 km) are navigable, and the majority of traffic is from tourist and residential narrowboats. History The earliest mention of the Birmingham Canal Navigation appears in ''Aris's Birmingham Gazette'' on 11 April 1768. Here it was reported that on 25 March 1768, the first general assembly of the Company of Proprietors of the Birmingham Canal Navigation was held at the Swann Inn, Birmingham, to raise funds to submit for an act of Parliament. The first canal to be built in the area was the Birmingham Canal, authorized by the (8 Geo. 3. c. 38) and built from 17 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Copyhold
Copyhold was a form of customary land ownership common from the Late Middle Ages into modern times in England. The name for this type of land tenure is derived from the act of giving a copy of the relevant title deed that is recorded in the manorial court roll to the tenant, rather than the actual land deed itself. The legal owner of the manor land remained the mesne lord, who was legally the ''copyholder'', according to the titles and customs written down in the manorial roll. In return for being given land, a copyhold tenant was required to carry out specific manorial duties or services. The specific rights and duties of copyhold tenants varied greatly from one manor to another and many were established by custom. By the 19th century, many customary duties had been replaced with the payment of rent. Copyhold was directly descended from the feudal system of villeinage which involved giving service and produce to the local lord in return for land. Although feudalism in Eng ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Castle
A castle is a type of fortification, fortified structure built during the Middle Ages predominantly by the nobility or royalty and by Military order (monastic society), military orders. Scholars usually consider a ''castle'' to be the private fortified house, fortified residence of a lord or noble. This is distinct from a mansion, palace, and villa, whose main purpose was exclusively for ''pleasance'' and are not primarily fortresses but may be fortified. Use of the term has varied over time and, sometimes, has also been applied to structures such as hill forts and 19th- and 20th-century homes built to resemble castles. Over the Middle Ages, when genuine castles were built, they took on a great many forms with many different features, although some, such as curtain wall (fortification), curtain walls, arrowslits, and portcullises, were commonplace. European-style castles originated in the 9th and 10th centuries after the fall of the Carolingian Empire, which resulted ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saxon
The Saxons, sometimes called the Old Saxons or Continental Saxons, were a Germanic people of early medieval "Old" Saxony () which became a Carolingian " stem duchy" in 804, in what is now northern Germany. Many of their neighbours were, like them, speakers of West Germanic dialects, including the inland Franks and Thuringians to the south, and the coastal Frisians and Angles to the north who were among the peoples who were originally referred to as "Saxons" in the context of early raiding and settlements in Roman Britain and Gaul. To their east were Obotrites and other Slavic-speaking peoples. The political history of these continental Saxons is unclear until the 8th century and the conflict between their semi-legendary hero Widukind and the Frankish emperor Charlemagne. They do not appear to have been politically united until the generations leading up to that conflict, and before then they were reportedly ruled by regional "satraps". Previous Frankish rulers of Austrasia, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subsidence
Subsidence is a general term for downward vertical movement of the Earth's surface, which can be caused by both natural processes and human activities. Subsidence involves little or no horizontal movement, which distinguishes it from slope movement. Processes that lead to subsidence include dissolution of underlying carbonate rock by groundwater; gradual compaction of sediments; withdrawal of fluid lava from beneath a solidified crust of rock; mining; pumping of subsurface fluids, such as groundwater or petroleum; or warping of the Earth's crust by tectonic forces. Subsidence resulting from tectonic deformation of the crust is known as tectonic subsidence and can create accommodation for sediments to accumulate and eventually lithify into sedimentary rock. Ground subsidence is of global concern to geologists, geotechnical engineers, surveyors, engineers, urban planners, landowners, and the public in general.National Research Council, 1991. ''Mitigating losses from land ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous Period
The Carboniferous ( ) is a geologic period and system of the Paleozoic era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the Permian Period, Ma. It is the fifth and penultimate period of the Paleozoic era and the fifth period of the Phanerozoic eon. In North America, the Carboniferous is often treated as two separate geological periods, the earlier Mississippian and the later Pennsylvanian. The name ''Carboniferous'' means "coal-bearing", from the Latin ("coal") and ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern "system" names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. Carboniferous is the period during which both terrestrial animal and land plant life was well established. Stegocephalia (four-limbed vertebrates including true tetrapods), whose forerunners (tetrapodomo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Staffordshire Coalfield
The South Staffordshire coalfield is one of several coalfields in the English Midlands. It stretches for 25 miles / 40 km from the Lickey Hills in the south to Rugeley in the north. The coalfield is around wide; its eastern and western margins are fault (geology), fault-bounded. Coal measures Numerous coal seams are recognised within the coalfield - the following coal seams are recognised within the Cannock section of the coalfield - an area sometimes separately referred to as the Cannock coalfield or Cannock Chase Coalfield, Cannock Chase coalfield: *Middle Coal Measures ** Top Robins ** Bottom Robins ** Charles ** Brooch ** Benches ** Eight Feet ** Park ** Upper/Top Heathen ** Lower/Bottom Heathen *Lower Coal Measures ** Yard ** Bass ** Cinder ** Shallow ** Deep ** Mealy Greys Within the southern part of the coalfield, fewer seams are recognised due to the 'Benches', 'Eight Feet' and 'Park' seams combining as the 'Thick' whilst the two 'Heathen' seams combine, the 'Yar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tame, West Midlands
The River Tame is a river in the West Midlands of England, and one of the principal tributaries of the River Trent. The Tame is about long from the source at Oldbury to its confluence with the Trent near Alrewas, but the main river length of the entire catchment, i.e. the Tame and its main tributaries, is about . It forms part of the Severn-Trent flyway, a route used by migratory birds to cross Great Britain. Etymology The name derives from the Celtic language, although it may have even earlier roots. It is usually thought to mean "dark", by analogy with the Sanskrit word ''tamas'' meaning darkness. Other possibilities are "slow-moving" or "flowing", although the precise meaning is uncertain. The name is shared with the River Tame, Greater Manchester, and it is likely that the River Thame, the River Thames, the River Teme, the River Team, and the River Tamar all share the derivation. Historic significance Birmingham and the parishes in the centre and north of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tame Flows Peacefully - Geograph
A river is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape aro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
