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Trysull And Seisdon Inclosure Act 1773
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 suffi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Road To Church - Geograph
A road is a thoroughfare used primarily for movement of traffic. Roads differ from streets, whose primary use is local access. They also differ from stroads, which combine the features of streets and roads. Most modern roads are Road surface, paved. The words "road" and "street" are commonly considered to be interchangeable, but the distinction is important in urban design. There are road hierarchy, many types of roads, including parkways, avenue (landscape), avenues, controlled-access highways (freeways, motorways, and expressways), tollways, interstates, highways, and local roads. The primary features of roads include lanes, sidewalks (pavement), roadways (carriageways), median strip, medians, shoulder (road), shoulders, road verge, 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 Organisation for Economic Co-operation and Development, Organi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and Rock (geology), 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 are those 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 language, French , which in turn is derived from the Savoyard dialect, Savoyard Italian ('mound of e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anglo-Saxon England
Anglo-Saxon England or early medieval England covers the period from the end of Roman Empire, Roman imperial rule in Roman Britain, Britain in the 5th century until the Norman Conquest in 1066. Compared to modern England, the territory of the Anglo-Saxons stretched north to present day Lothian in southeastern Scotland, whereas it did not initially include western areas of England such as Cornwall, Herefordshire, Shropshire, Cheshire, Lancashire, and Cumbria. The 5th and 6th centuries involved the collapse of economic networks and political structures and also saw a radical change to a new Anglo-Saxon language and culture. This change was driven by movements of peoples as well as changes which were happening in both northern Gaul and the North Sea coast of what is now Germany and the Netherlands. The Anglo-Saxon language, also known as Old English, was a close relative of languages spoken in the latter regions, and genetic studies have confirmed that there was significant migrat ... [...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, Sweden, Finland, Norway, 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), ''härad'' or ''hundare'' (Swedish), ''Harde'' (German), ''hiird'' (North Frisian language, North Frisian), ''kihlakunta'' (Finnish), and ''cantref'' (Welsh). In Ireland, a similar subdivision of counties is referred to as a Barony (Ireland), barony, and a hundred is a subdivision of a particularly large townland (most townlands are not divided into hundreds). Etymology The origin of the division of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anglo-Saxon
The Anglo-Saxons, in some contexts simply called Saxons or the English, were a Cultural identity, cultural group who spoke Old English and inhabited much of what is now England and south-eastern Scotland in the Early Middle Ages. They traced their origins to Germanic peoples, Germanic settlers who became one of the most important cultural groups in Britain by the 5th century. The Anglo-Saxon period in Britain is considered to have started by about 450 and ended in 1066, with the Norman conquest of England, Norman Conquest. Although the details of Anglo-Saxon settlement of Britain, their early settlement and History of Anglo-Saxon England, political development are not clear, by the 8th century an Anglo-Saxon cultural identity which was generally called had developed out of the interaction of these settlers with the existing Romano-British culture. By 1066, most of the people of what is now England spoke Old English, and were considered English. Viking and Norman invasions chang ... [...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 The West Midlands conurbation is the large conurbation in the West Midlands region of England. The area consists of two cities and numerous towns: to the east, the city of Birmingham, along with adjacent towns of Solihull and Sutton Coldfield; a ... and the Metropolitan Borough of Dudley. Population details for the United Kingdom Census 2011, 2011 census can be found under Kinver. There are a small number of predominantly older scattered houses in it, as well as a 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. History Ashwood was formerly an area of medieval woodland and later heathland, bounded by th ... [...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, e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roman Britain
Roman Britain was the territory that became the Roman province of ''Britannia'' after the Roman conquest of Britain, consisting of a large part of the island of Great Britain. The occupation lasted from AD 43 to AD 410. 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 the Belgae during the British Iron Age and had been aiding Caesar's enemies. The Belgae were the only Celtic tribe to cross the sea into Britain, for to all other Celtic tribes this land was unknown. 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 () according to Suetonius, perhaps as a symbolic gesture to proclaim Caligula's victory over th ... [...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", r ... [...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. Floodplains stretch from the banks of a river channel to the base of the enclosing valley, and experience flooding during periods of high Discharge (hydrology), 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 of regular flooding, floodplains frequently have high soil fertility since nutrients are deposited with the flood waters. This can encourage farming; some important agricultural regions, such as the Nile and Mississippi Basin, Mississippi Drainage basin, river basins, heavily exploit floodplains. Agricultural and urban regions have developed near or on floodplains to take advantage of the rich soil and freshwater. However, the Flood risk, risk of inundation has led to increasing efforts to Flood control, control flooding. Formation Most floodplai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, 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 dike (geology), 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 diagram, 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) conta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pebble
A pebble is a clastic rocks, clast of rock (geology), rock with a grain size, particle size of based on the Particle size (grain size), Udden-Wentworth scale of sedimentology. Pebbles are generally considered larger than Granule (geology), granules ( in diameter) and smaller than Cobble (geology), cobbles ( in diameter). A rock made predominantly of pebbles is termed a conglomerate (geology), conglomerate. oldowan, 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 armor (hydrology), 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. Pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
