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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] |
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] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Provenà ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anglo-Saxon England
Anglo-Saxon England or Early Medieval England, existing from the 5th to the 11th centuries from the end of Roman Britain until the Norman conquest in 1066, consisted of various Anglo-Saxon kingdoms until 927, when it was united as the Kingdom of England by King Æthelstan (r. 927–939). It became part of the short-lived North Sea Empire of Cnut the Great, a personal union between England, Denmark and Norway in the 11th century. The Anglo-Saxons migrated to England from mainland northwestern Europe after the Roman Empire abandoned Britain at the beginning of the fifth century. Anglo-Saxon history thus begins during the period of sub-Roman Britain following the end of Roman control, and traces the establishment of Anglo-Saxon kingdoms in the 5th and 6th centuries (conventionally identified as seven main kingdoms: Northumbria, Mercia, East Anglia, Essex, Kent, Sussex, and Wessex); their Christianisation during the 7th century; the threat of Viking invasions and Danish settle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hundred (county Subdivision)
A hundred is an administrative division that is geographically part of a larger region. It was formerly used in England, Wales, some parts of the United States, Denmark, Southern Schleswig, Sweden, Finland, Norway, the Bishopric of Ösel–Wiek, Curonia, the Ukrainian state of the Cossack Hetmanate and in Cumberland County, New South Wales, Cumberland County in the British Colony of New South Wales. It is still used in other places, including in Australia (in South Australia and the Northern Territory). Other terms for the hundred in English and other languages include ''#wapentake, wapentake'', ''herred'' (Danish and Bokmål, Bokmål Norwegian), ''herad'' (Nynorsk, Nynorsk Norwegian), ''hérað'' (Icelandic), ''härad'' or ''hundare'' (Swedish), ''Harde'' (German), ''hiird'' (North Frisian language, North Frisian), ''satakunta'' or ''kihlakunta'' (Finnish), ''kihelkond'' (Estonian), ''kiligunda'' (Livonian), ''cantref'' (Welsh) and ''sotnia'' (Slavic). In Ireland, a similar subdi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anglo-Saxon
The Anglo-Saxons were a Cultural identity, cultural group who inhabited England in the Early Middle Ages. They traced their origins to settlers who came to Britain from mainland Europe in the 5th century. However, the ethnogenesis of the Anglo-Saxons happened within Britain, and the identity was not merely imported. Anglo-Saxon identity arose from interaction between incoming groups from several Germanic peoples, Germanic tribes, both amongst themselves, and with Celtic Britons, indigenous Britons. Many of the natives, over time, adopted Anglo-Saxon culture and language and were assimilated. The Anglo-Saxons established the concept, and the Kingdom of England, Kingdom, of England, and though the modern English language owes somewhat less than 26% of its words to their language, this includes the vast majority of words used in everyday speech. Historically, the Anglo-Saxon period denotes the period in Britain between about 450 and 1066, after Anglo-Saxon settlement of Britain, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashwood, Staffordshire
Ashwood is a small area of Staffordshire, England. It is situated in the South Staffordshire district, approximately two miles west of the West Midlands conurbation and the Metropolitan Borough of Dudley. Population details for the 2011 census can be found under Kinver. There are a small number of predominantly older scattered houses in it, as well as marina off the Staffordshire and Worcestershire Canal. There is no nucleated village. More built-up nearby areas include Kingswinford, Stourbridge, Kinver and Wolverhampton. The nearest public amenities are approximately one mile away in Wall Heath village. Wooded Pool near Ashwood, Staffordshire History Ashwood was formerly an area of medieval woodland and later heathland, bounded by the Smestow Brook, the River Stour, and cultivated lands in Kingswinford. It was one of the medieval hays (enclosures) of Kinver Forest. It was managed by a bailiff, who had a small farm at Prestwood by the service of keeping the hay. The ... [...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] |
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] |
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] |
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] |
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] |
Pebble
A pebble is a clast of rock with a particle size of based on the Udden-Wentworth scale of sedimentology. Pebbles are generally considered larger than granules ( in diameter) and smaller than cobbles ( in diameter). A rock made predominantly of pebbles is termed a conglomerate. Pebble tools are among the earliest known man-made artifacts, dating from the Palaeolithic period of human history. A beach composed chiefly of surface pebbles is commonly termed a shingle beach. This type of beach has armoring characteristics with respect to wave erosion, as well as ecological niches that provide habitat for animals and plants. Inshore banks of shingle (large quantities of pebbles) exist in some locations, such as the entrance to the River Ore, England, where the moving banks of shingle give notable navigational challenges. Pebbles come in various colors and textures and can have streaks, known as veins, of quartz or other minerals. Pebbles are mostly smooth but, dependent on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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