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Osse Stream
The Osse Stream or Osse Ditch, otherwise known as the Appleton Brook, is a small stream in the Vale of White Horse in historic Berkshire, since 1974 in Oxfordshire. The stream is a tributary of the River Ock, with its confluence near Marcham Mill. The stream rises at a pond in Cumnor, flowing past Besselsleigh, Appleton, Fyfield, Frilford and Marcham. Name The hydronym ''Osse'' appears to be derived from the Old English word ''Wase'', meaning 'mud'. See also * Tributaries of the River Ock *List of rivers of England This is a list of rivers of England, organised geographically and taken anti-clockwise around the English coast where the various rivers discharge into the surrounding seas, from the Solway Firth on the Scottish border to the Welsh Dee on the Wel ... References Vale of White Horse Rivers of Oxfordshire Thames drainage basin {{England-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Osse Stream Near Besselsleigh
The Compton Gamma Ray Observatory (CGRO) was a space observatory detecting photons with energies from 20 k eV to 30 GeV, in Earth orbit from 1991 to 2000. The observatory featured four main telescopes in one spacecraft, covering X-rays and gamma rays, including various specialized sub-instruments and detectors. Following 14 years of effort, the observatory was launched from Space Shuttle ''Atlantis'' during STS-37 on April 5, 1991, and operated until its deorbit on June 4, 2000. It was deployed in low Earth orbit at to avoid the Van Allen radiation belt. It was the heaviest astrophysical payload ever flown at that time at . Costing $617 million, the CGRO was part of NASA's "Great Observatories" series, along with the Hubble Space Telescope, the Chandra X-ray Observatory, and the Spitzer Space Telescope. It was the second of the series to be launched into space, following the Hubble Space Telescope. The CGRO was named after Arthur Compton, an American physicist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vale Of White Horse
The Vale of White Horse is a local government district of Oxfordshire in England. It was historically a north-west projection of Berkshire. The area is commonly referred to as the 'Vale of ''the'' White Horse'. It is crossed by the Ridgeway National Trail in its far south, across the North Wessex Downs AONB at the junction of four counties. The northern boundary is defined by the River Thames. The name refers to Uffington White Horse, a prehistoric hill figure. History The area has been long settled as a productive fertile chalklands above well-drained clay valleys and well-farmed with many small woodlands and hills between the Berkshire Downs and the River Thames on its north and east sides. It is named after the prominent and large Bronze Age-founded Uffington White Horse hill figure. The name "Vale of the White Horse" predates the present-day local authority district, having been described, for example, in the 1870-72 ''Imperial Gazetteer of England and Wales''. The distri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Ock
The River Ock is a small English river which is a tributary of the River Thames. It has as its catchment area the Vale of White Horse, a low-lying and wide valley in south Oxfordshire, and flows into the River Thames, at Abingdon on the reach above Culham Lock. Course The River Ock rises near the village of Little Coxwell. It collects tributaries from each village along the base of the White Horse Hills, where springs emanating from the chalk hills allowed settlements to flourish in former times. Among these tributaries is the Osse Stream, rising in Cumnor. From Little Coxwell, the Ock runs around Longcot and flows past Stanford in the Vale, where it is about wide. The name of Stanford comes from ''stony ford'', possibly alluding to the Ock crossing at Stanford Mill. Thence it runs past Charney Bassett, Lyford, Garford and Marcham Mill, before losing its identity and its waters to the Thames at Abingdon by the old Hygienic Laundry building. An iron bridge crosses at the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Besselsleigh
Besselsleigh or Bessels Leigh is an English village and civil parish about southwest of Oxford. Besselsleigh was part of Berkshire until the 1974 boundary changes transferred it to Oxfordshire. The village is just off the A420 road between Oxford and Swindon. Manor Domesday Book Besselsleigh is almost certainly the "Lea" or "Leigh" owned by a Saxon named Earmund in the 7th century. At the time of the Domesday Book in 1086 it was recorded (as "Leie") as having been held before the Norman Conquest by Northmann of Mereworth of Abingdon Abbey and to have passed under the same overall ownership to the minor feudal lord William the Chamberlain. Bessels The manor of Leigh was acquired by the family of Bessels (or Besils, Bessiles, etc.) in the mid-14th century, possibly by Thomas Bessels, and by the next century had become known as "Bessels Leigh" to distinguish it from the many other places in England called "Leigh". According to the antiquary John Leland, the Bessels family had ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Appleton, Oxfordshire
Appleton is a village in the civil parish of Appleton-with-Eaton, about northwest of Abingdon. Historically in Berkshire, the 1974 boundary changes transferred it to Oxfordshire for administrative purposes. The 2011 Census recorded Appleton-with-Eaton's parish population as 915. Manor In the 9th century Abingdon Abbey held the manor of Appleton. In 871 the Danes sacked the abbey and thereby obtained Appleton, but it is assumed that Appleton was recovered by Alfred the Great. Appleton's toponym means simply "an orchard". In the 10th century it was ''Æppeltune'' or ''Appeltun'', from then until the 17th century it evolved as ''Apletone'', ''Apletune'' and ''Appelton'', and in 1316 it was recorded as ''Aspelton''. In the 10th century the village had the alternative name of ''Earmundeslæh'', ''Earmundesleah'', ''Earmundeslee'' or ''Earmundeslei'', referring to King Edmund I, who in 942 granted it to Athelstan, one of his thegns, who may have restored it to Abingdon Abbey. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fyfield, Oxfordshire
Fyfield is a village in Fyfield and Tubney civil parish, about west of Abingdon. It was part of Berkshire until the 1974 boundary changes transferred it to Oxfordshire. The village used to be on the main A420 road between Oxford and Faringdon, but a bypass now carries the main road just south of the village. Toponym Fyfield's toponym is derived from the Old English ''Fif Hide'' (10th century). It was spelt ''Fifhide'' from the 10th to the 16th century, but also ''Fivehide'' in the 11th century, ''Fifide'' from the 13th to the 15th century, ''Fifhede'' in the 15th century and ''Fighfield'' or ''Fyfylde'' in the 16th century. Manor There has been a manor of Fyfield since at least the 10th century. The Chronicle of Abingdon claims that in 956 King Eadwig granted his thegn Æthelnoth 13 manses of land there. In 968 King Edgar confirmed these 11 hides of land plus another 12 hides to the Benedictine Abingdon Abbey. After the Norman Conquest the manor was granted to Henry ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frilford
Frilford is a hamlet and civil parish about west of Abingdon, at the junction of the A415 and A338 roads. It lies in the traditional county of Berkshire, but since 1974 has been administered as part of Oxfordshire. Archaeology The parish of Frilford has two significant archaeological sites: a Roman villa, and a cemetery on Frilford Heath that appears to include both Roman and Saxon burials. A further complex of remains, including a Roman shrine and amphitheatre, is often referred to as being in Frilford but lies to the south of the village, just inside the boundary of Marcham parish. Churches Frilford is part of the Church of England parish of Marcham. It has no Church of England parish church of its own, but a Congregational chapel was built at Frilford in 1841. Amenities Frilford Heath Golf Club is to the east of the village. Abingdon Preparatory School at Frilford, formerly Joscas, is a preparatory school. Transport Three Stagecoach in Oxfordshire bus routes serve Fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marcham
Marcham is a village and civil parish about west of Abingdon, Oxfordshire. The 2011 Census recorded the parish's population as 1,905. The parish includes the hamlets of Cothill east-northeast of the village, and Gozzard's Ford northeast of the village. Frilford and Garford used to be townships of Marcham parish, but are now separate civil parishes. All these parishes were part of Berkshire until the 1974 boundary changes transferred them to Oxfordshire. Marcham parish extends about north–south and up to east–west. It is bounded to the south by the River Ock and to the east largely by Sandford Brook, a tributary of the Ock. To the west it is bounded largely by field boundaries. To the north the parish tapers almost to a point, bounded to the west by the A338 road, to the north by the A420 road and to the east by field boundaries. The land is low-lying, rising from about above sea level by the Ock in the south to at Upwood Park in the north. Marcham village is on t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hydronym
A hydronym (from el, ὕδρω, , "water" and , , "name") is a type of toponym that designates a proper name of a body of water. Hydronyms include the proper names of rivers and streams, lakes and ponds, swamps and marshes, seas and oceans. As a subset of toponymy, a distinctive discipline of ''hydronymy'' (or ''hydronomastics'') studies the proper names of all bodies of water, the origins and meanings of those names, and their development and transmission through history. Classification by water types Within the onomastic classification, main types of hydronyms are (in alphabetical order): * helonyms: proper names of swamps, marshes and bogs, * limnonyms: proper names of lakes and ponds, * oceanonyms: proper names of oceans, * pelagonyms: proper names of seas and maritime bays, * potamonyms: proper names of rivers and streams. Linguistic phenomena Often a given body of water will have several entirely different names given to it by different peoples living along its shor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old English Language
Old English (, ), or Anglo-Saxon, is the earliest recorded form of the English language, spoken in England and southern and eastern Scotland in the early Middle Ages. It was brought to Great Britain by Anglo-Saxon settlers in the mid-5th century, and the first Old English literary works date from the mid-7th century. After the Norman conquest of 1066, English was replaced, for a time, by Anglo-Norman (a relative of French) as the language of the upper classes. This is regarded as marking the end of the Old English era, since during this period the English language was heavily influenced by Anglo-Norman, developing into a phase known now as Middle English in England and Early Scots in Scotland. Old English developed from a set of Anglo-Frisian or Ingvaeonic dialects originally spoken by Germanic tribes traditionally known as the Angles, Saxons and Jutes. As the Germanic settlers became dominant in England, their language replaced the languages of Roman Britain: Common Br ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributaries Of The River Ock
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & Scott ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Rivers Of England
This is a list of rivers of England, organised geographically and taken anti-clockwise around the English coast where the various rivers discharge into the surrounding seas, from the Solway Firth on the Scottish border to the Welsh Dee on the Welsh border, and again from the Wye on the Welsh border anti-clockwise to the Tweed on the Scottish border. Tributaries are listed down the page in an upstream direction, i.e. the first tributary listed is closest to the sea, and tributaries of tributaries are treated similarly. Thus, in the first catchment below, the River Sark is the lowermost tributary of the Border Esk and the Hether Burn is the lowermost tributary of the River Lyne. The main stem (or principal) river of a catchment is labelled as (MS), left-bank tributaries are indicated by (L), right-bank tributaries by (R). Note that in general usage, the 'left (or right) bank of a river' refers to the left (or right) hand bank, as seen when looking downstream. Where a named river ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
