River Onny
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River Onny
The River Onny is a river in Shropshire, England. It is a major tributary of the River Teme. Etymology The river's name derives from Welsh and means the river on which ash trees (Welsh: ''onnau'') grew. Course The river has its sources in the Shropshire Hills at White Grit, located in Mid and South-west Shropshire. It has two branches, the East Onny and West Onny, which converge at Eaton, to the east of Lydham. The River Onny then flows in a south-easterly direction, through Craven Arms and Onibury (a village it gives its name to), before it finally has its confluence with the River Teme just upstream of Ludlow at Bromfield. From White Grit to Bromfield, the river flows over a distance of . The River Teme is itself a tributary of the River Severn, confluencing just south of Worcester city centre. The River Severn then flows south-west meeting the sea at Bristol Channel. Geology Geologically, the Onny has the type section just west of Craven Arms of the Caradoc series of th ...
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River Onny - Downstream - Geograph
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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Bromfield, Shropshire
Bromfield is a village and civil parish in Shropshire, England. According to the 2001 census it had a population of 306, which had fallen to 277 at the 2011 census. Location Bromfield is located near the market town of Ludlow, two miles (3 km) northwest of the town centre, on the A49 road. The A4113 road (to Knighton) has its eastern end in Bromfield, at its junction with the A49. The village is situated near the confluence of the River Teme and River Onny. The latter splits the village into two, with the church and many of the older buildings to the west and the recently redeveloped business area to the east (towards Ludlow). A bridge takes the main road over the river. History The manor of Bromfield, and separately Bromfield Priory, are recorded in the Domesday Book of 1086, then still falling within the Saxon hundred of Culvestan, which was abolished in the reign of Henry I; Bromfield then came within Munslow hundred. It was a large and well-populated manor. The p ...
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Onnia (trilobite)
''Onnia'' is a genus of trilobites from the late Ordovician of Africa, Europe, North America, and South America. Fossils have been found in Canada (Quebec), the Czech Republic, France, Morocco, Portugal, Spain, the United Kingdom, and Venezuela.''Onnia''
at .org


References


Further reading

*''Fossils'' (Smithsonian Handbooks) by David Ward


External links


''Onnia''
in the

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Trilobite
Trilobites (; meaning "three lobes") are extinct marine arthropods that form the class Trilobita. Trilobites form one of the earliest-known groups of arthropods. The first appearance of trilobites in the fossil record defines the base of the Atdabanian stage of the Early Cambrian period () and they flourished throughout the lower Paleozoic before slipping into a long decline, when, during the Devonian, all trilobite orders except the Proetida died out. The last extant trilobites finally disappeared in the mass extinction at the end of the Permian about 252 million years ago. Trilobites were among the most successful of all early animals, existing in oceans for almost 270 million years, with over 22,000 species having been described. By the time trilobites first appeared in the fossil record, they were already highly diversified and geographically dispersed. Because trilobites had wide diversity and an easily fossilized exoskeleton, they left an extensive fossil record. The stu ...
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Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Union of Geological Sciences, Intern ...
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Caradoc Series
In geology, Caradoc Series is the name introduced by Roderick Murchison in 1839 for the sandstone series of Caer Caradoc in Shropshire, England. It is the fifth of the six subdivisions (in ascending order) of the Ordovician System, comprising all those rocks deposited worldwide during the Caradocian Age (458 to 448 million years ago). The limits of Murchison's Caradoc series have since been somewhat modified, and through the labours of Charles Lapworth the several members of the series have been precisely defined by means of graptolitic zones. These zones are identical with those found in the rocks of the same age in North Wales, the Bala Series, and the terms Bala or Caradoc series are used interchangeably by geologists when referring to the uppermost substage of the Ordovician System. The Ordovician rocks of the Caradoc district have been subdivided into the following beds, in descending order: the Trinucleus shales, Acton Scott beds, Longville flags, Chatwell and Soudley sands ...
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Bristol Channel
The Bristol Channel ( cy, Môr Hafren, literal translation: "Severn Sea") is a major inlet in the island of Great Britain, separating South Wales from Devon and Somerset in South West England. It extends from the lower estuary of the River Severn ( cy, Afon Hafren) to the North Atlantic Ocean. It takes its name from the English city of Bristol, and is over 30 miles (50 km) wide at its western limit. Long stretches of both sides of the coastline are designated as Heritage Coast. These include Exmoor, Bideford Bay, the Hartland Point peninsula, Lundy Island, Glamorgan, Gower Peninsula, Carmarthenshire, South Pembrokeshire and Caldey Island. Until Tudor times the Bristol Channel was known as the Severn Sea, and it is still known as this in both cy, Môr Hafren and kw, Mor Havren. Geography The International Hydrographic Organization now defines the western limit of the Bristol Channel as "a line joining Hartland Point in Devon () to St. Govan's Head in Pembrokeshire ...
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Worcester, England
Worcester ( ) is a cathedral city in Worcestershire, England, of which it is the county town. It is south-west of Birmingham, north-west of London, north of Gloucester and north-east of Hereford. The population was 103,872 in the 2021 Census. The River Severn flanks the western side of the city centre. It is overlooked by Worcester Cathedral. Worcester is the home of Royal Worcester, Royal Worcester Porcelain, composer Edward Elgar, Lea & Perrins, makers of traditional Worcestershire sauce, the University of Worcester, and ''Berrow's Worcester Journal'', claimed as the world's oldest newspaper. The Battle of Worcester in 1651 was the final battle of the English Civil War, during which Oliver Cromwell's New Model Army defeated Charles II of England, King Charles II's Cavalier, Royalists. History Early history The trade route past Worcester, later part of the Roman roads in Britain, Roman Ryknild Street, dates from Neolithic times. It commanded a ford crossing over the Rive ...
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River Severn
, name_etymology = , image = SevernFromCastleCB.JPG , image_size = 288 , image_caption = The river seen from Shrewsbury Castle , map = RiverSevernMap.jpg , map_size = 288 , map_caption = Tributaries (light blue) and major settlements on and near the Severn (bold blue) , pushpin_map = , pushpin_map_size = 288 , pushpin_map_caption= , subdivision_type1 = Country , subdivision_name1 = England and Wales , subdivision_type2 = , subdivision_name2 = , subdivision_type3 = Region , subdivision_name3 = Mid Wales, West Midlands, South West , subdivision_type4 = Counties , subdivision_name4 = Powys, Shropshire, Worcestershire, Gloucestershire , subdivision_type5 = Cities , subdivision_name5 = Shrewsbury, Worcester, Gloucester, Bristol , length = , width_min = , width_avg = , width_max = , depth_min = , depth_avg = ...
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Ludlow
Ludlow () is a market town in Shropshire, England. The town is significant in the history of the Welsh Marches and in relation to Wales. It is located south of Shrewsbury and north of Hereford, on the A49 road which bypasses the town. The town is near the confluence of the rivers Corve and Teme. The oldest part is the medieval walled town, founded in the late 11th century after the Norman conquest of England. It is centred on a small hill which lies on the eastern bank of a bend of the River Teme. Situated on this hill are Ludlow Castle and the parish church, St Laurence's, the largest in the county. From there the streets slope downward to the rivers Corve and Teme, to the north and south respectively. The town is in a sheltered spot beneath Mortimer Forest and the Clee Hills, which are clearly visible from the town. Ludlow has nearly 500 listed buildings, including examples of medieval and Tudor-style half-timbered buildings. The town was described by Sir John Betjeman ...
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Shropshire
Shropshire (; alternatively Salop; abbreviated in print only as Shrops; demonym Salopian ) is a landlocked historic county in the West Midlands region of England. It is bordered by Wales to the west and the English counties of Cheshire to the north, Staffordshire to the east, Worcestershire to the southeast, and Herefordshire to the south. A unitary authority of the same name was created in 2009, taking over from the previous county council and five district councils, now governed by Shropshire Council. The borough of Telford and Wrekin has been a separate unitary authority since 1998, but remains part of the ceremonial county. The county's population and economy is centred on five towns: the county town of Shrewsbury, which is culturally and historically important and close to the centre of the county; Telford, which was founded as a new town in the east which was constructed around a number of older towns, most notably Wellington, Dawley and Madeley, which is today th ...
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Onibury
Onibury is a village and civil parish on the River Onny in southern Shropshire, about northwest of the market town of Ludlow. The parish includes the hamlets of Walton and Wootton and was extended in 1967 to include parts from Clungunford and Stokesay. It borders the parishes of Clungunford, Stokesay (now part of Craven Arms parish), Bromfield, Culmington and Stanton Lacy. The country houses of Ferney Hall and Stokesay Court are in the parish. History Toponym The toponym "Onibury" is derived from the Old English for "fortified place on the River Onny". "Onny" means "river on whose banks ash trees grew", from the Welsh "on" meaning ashes. Domesday Book Onibury is recorded in the Domesday Book of 1086 as ''Aneberie''. It had 15 households, making it a fairly medium-sized settlement for the time, and a priest. The manor formed part of the Saxon hundred of Culvestan. Hundred Onibury came to be in the lower division of the hundred of Munslow, following the amalgamation of C ...
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