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Trysull
Trysull is a rural village in the county of Staffordshire, England approximately five miles south-west of Wolverhampton. With the adjacent village of Seisdon, it forms the civil parish of Trysull and Seisdon, within the South Staffordshire non-metropolitan district. Until 1974 it formed part of Seisdon Rural District. The 2011 census recorded a usually resident population for the parish of Trysull & Seisdon of 1,150 persons in 455 households. The village has not been greatly affected by over-modern development and still retains many of the old country cottages, houses and a manor house. Toponymy In 1086 the village name appears in the Domesday Book as ''Treslei''. One of the families who subsequently occupied the estate were styled ''de Tressell''. The name appears to mean "the settlement in the clearing", deriving from the Welsh prefix ''tre'' settlement and the suffix ''leah'' a woodland clearing. The next significant placename to the north is Trescott, where the suffix ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trysull And Seisdon
Trysull and Seisdon is a conjoined Civil parishes in England, civil parish in the South Staffordshire non-metropolitan district, in the county of Staffordshire, England. The population of the civil parish taken at the United Kingdom Census 2011, 2011 census was 1,150. It is in the lowest tier of local government below districts of England, districts and metropolitan and non-metropolitan counties of England, counties.F. Youngs, Local Administrative Units: Northern England (London: Royal Historical Society, 1991), p. 426. It is both an Parish (administrative division), administrative parish, and an ecclesiastical parish formed from the two historic villages of Trysull and Seisdon. Background Although a historic entity, the civil parish, in its modern sense, was established afresh in 1894, by the Local Government Act 1894. It was part of Seisdon Rural District until 1974. Governance There is a parish meeting, consisting of all the electors of the parish. Generally a meeting is held ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seisdon
Seisdon is a rural village in the parish of Trysull and Seisdon, Staffordshire approximately six miles west of Wolverhampton and the name of one of the five Hundred (county division), hundreds of Staffordshire. The population recorded at the United Kingdom Census 2011, 2011 census does not distinguish this hamlet from the rest of the parish, which had a population of 1,150. Etymology The name appears to mean "hill of the Saxons", deriving from the Anglo-Saxon words ''Seis'' meaning Saxon and ''Dun'' meaning hill. The first element may alternatively be a personal name.The English Hundred Names, by Olof Anderson, Lund (Sweden), 1934. Page 145 Location and Sites Seisdon is a hamlet within the parish of Trysull and Seisdon (formerly named Trysull, only), lying one mile north-west of the village of Trysull, near the border with Shropshire. There is a narrow bridge of several arches over the river Smestow Brook, Smestow,History, Gazetteer and Directory of Staffordshire by William White ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Smestow Brook
The Smestow Brook, sometimes called the River Smestow, is a small river that plays an important part in the drainage of Wolverhampton, South Staffordshire, and parts of Dudley in the United Kingdom, and has contributed to the industrial development of the Black Country. It is the most important tributary of the River Stour, Worcestershire and part of the River Severn catchment. Etymology and usage The name of the stream may be of Anglo-Saxon origin, although it was not written down before the 14th century in the Middle English forms ''Smetheslall'' and ''Smethestalle''. As late as the 19th century, the name was still generally rendered ''Smestall'' in surveys of the county. It means ″place of the smiths″. The whole of this part of the West Midlands was famed for iron production from the Middle Ages onwards. The nearby Kinver Forest and Wyre Forest supplied charcoal for smelting and working iron before the Industrial Revolution. Both the lower Smestow and the Stour were line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seisdon Rural District
Seisdon was a rural district in Staffordshire, England from 1894 to 1974. It lays west of Wolverhampton and was formed under the Local Government Act 1894 based on the Seisdon rural sanitary district. Villages in the district included Kinver, Wombourne, Codsall, Trysull and Pattingham. In 1933, it was expanded to absorb the northern section of Kingswinford rural district, with the southern, more urban section of the district being absorbed into Brierley Hill. At the same time, a section of Penn was removed from Seisdon to be incorporated into Wolverhampton. A year later, part of the district was absorbed into Tettenhall. In 1966, the village of Gospel End was transferred into Seisdon having previously been part of Sedgley. This reorganisation also involved a section of Brierley Hill being removed from Seisdon and, along with the bulk of Sedgley and Brierley Hill, being placed into an enlarged Dudley borough. It continued in existence until 1 April 1974, when it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Staffordshire (UK Parliament Constituency)
South Staffordshire is a constituency represented in the House of Commons of the UK Parliament since 2010 by Sir Gavin Williamson, a Conservative. Boundaries 1832–1868: The Hundreds of South Offlow, Seisdon and Cuttleston. 1983–1997: The District of South Staffordshire. 1997–2010: The District of South Staffordshire wards of Bilbrook, Brewood and Coven, Cheslyn Hay, Codsall North, Codsall South, Essington, Featherstone, Great Wyrley Landywood, Great Wyrley Town, Kinver, Lower Penn, Pattingham and Patshull, Perton Central, Perton Dippons, Shareshill, Swindon, Trysull and Seisdon, Wombourne North, Wombourne South East, and Wombourne South West. 2010–present: The District of South Staffordshire wards of Bilbrook, Brewood and Coven, Cheslyn Hay North and Saredon, Cheslyn Hay South, Codsall North, Codsall South, Essington, Featherstone and Shareshill, Great Wyrley Landywood, Great Wyrley Town, Himley and Swindon, Huntington and Hatherton, Kinver, Pattingham and Patshul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wolverhampton
Wolverhampton () is a city, metropolitan borough and administrative centre in the West Midlands, England. The population size has increased by 5.7%, from around 249,500 in 2011 to 263,700 in 2021. People from the city are called "Wulfrunians". Historically part of Staffordshire, the city grew initially as a market town specialising in the wool trade. In the Industrial Revolution, it became a major centre for coal mining, steel production, lock making, and the manufacture of cars and motorcycles. The economy of the city is still based on engineering, including a large aerospace industry, as well as the service sector. Toponym The city is named after Wulfrun, who founded the town in 985, from the Anglo-Saxon ''Wulfrūnehēantūn'' ("Wulfrūn's high or principal enclosure or farm"). Before the Norman Conquest, the area's name appears only as variants of ''Heantune'' or ''Hamtun'', the prefix ''Wulfrun'' or similar appearing in 1070 and thereafter. Alternatively, the city ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flood Plain
A floodplain or flood plain or bottomlands is an area of land adjacent to a river which stretches from the banks of its channel to the base of the enclosing valley walls, and which experiences flooding during periods of high discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because the regular flooding of floodplains can deposit nutrients and water, floodplains frequently have high soil fertility; some important agricultural regions, such as the Mississippi river basin and the Nile, rely heavily on the flood plains. Agricultural regions as well as urban areas have developed near or on floodplains to take advantage of the rich soil and fresh water. However, the risk of flooding has led to increasing efforts to control flooding. Formation Most floodplains are formed by deposition on the inside of river meanders and by overbank flow. Whereve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunter (geology)
Bunter Pebble Beds is the name formerly given to a set of sandstone deposits within the New Red Sandstone containing rounded pebbles. They are thought to be alluvial deposits and, judging from the rounding of the mainly quartzite pebbles, to have resulted from prolonged transportation in a large and turbulent river, resulting in powerful abrasion. Etymology The name "Bunter" derives from the German term "Buntsandstein", "bunt" meaning "variegated" or "colourful", referring to the colour of the sandstone deposit, which varies from reddish to greenish. Utility The pebbles, also called cobbles, which can be used as gravel, as ballast or as cobblestones, are mainly milky-white quartzite but can vary in colour and composition, including some that are hard, reddish-coloured sandstone. The sandstone in which these pebbles are deposited can be used for building or as an aggregate for cement or concrete. The sandstone can be hard enough for building, yet easy enough to "work", result ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roman Britain
Roman Britain was the period in classical antiquity when large parts of the island of Great Britain were under occupation by the Roman Empire. The occupation lasted from AD 43 to AD 410. During that time, the territory conquered was raised to the status of a Roman province. Julius Caesar invaded Britain in 55 and 54 BC as part of his Gallic Wars. According to Caesar, the Britons had been overrun or culturally assimilated by other Celtic tribes during the British Iron Age and had been aiding Caesar's enemies. He received tribute, installed the friendly king Mandubracius over the Trinovantes, and returned to Gaul. Planned invasions under Augustus were called off in 34, 27, and 25 BC. In 40 AD, Caligula assembled 200,000 men at the Channel on the continent, only to have them gather seashells ('' musculi'') according to Suetonius, perhaps as a symbolic gesture to proclaim Caligula's victory over the sea. Three years later, Claudius directed four legi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greensforge
Greensforge is a scattered hamlet on the boundary of Kinver and Swindon parishes, in South Staffordshire, England. It is noted for its Roman associations and its industrial heritage. Etymology The hamlet takes its name from a finery forge established there in the early 17th century: Mr Green's Forge. This was typical of early industrial development all along the Smestow Brook, in which bloomeries, foundries and forges used local water supplies and charcoal. History The hamlet was not the earliest settlement in the area. The name Greensforge is also used for a group of Romans forts lying on the west of the brook, partly in Ashwood. The remains of one fort, extending to 2.3 hectares, are visible as a low banked enclosure on either side of Mile Flat, just east of the canal locks and wharf. This dates from period 60-80 AD. It was identified at least as early as the 18th century and numerous finds of pottery and other objects were made before it was excavated in 1929. The other, ea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Road To Church - Geograph
A road is a linear way for the conveyance of traffic that mostly has an improved surface for use by vehicles (motorized and non-motorized) and pedestrians. Unlike streets, the main function of roads is transportation. There are many types of roads, including parkways, avenues, controlled-access highways (freeways, motorways, and expressways), tollways, interstates, highways, thoroughfares, and local roads. The primary features of roads include lanes, sidewalks (pavement), roadways (carriageways), medians, shoulders, verges, bike paths (cycle paths), and shared-use paths. Definitions Historically many roads were simply recognizable routes without any formal construction or some maintenance. The Organization for Economic Co-operation and Development (OECD) defines a road as "a line of communication (travelled way) using a stabilized base other than rails or air strips open to public traffic, primarily for the use of road motor vehicles running on their own wheels", which in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
