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56-564: Framilode is a village on the banks of the River Severn in Gloucestershire , England, in the parish of Fretherne with Saul . It consists of two settlements: the larger, Framilode, is at the mouth of the River Frome . The smaller settlement, Framilode Passage , lies about 0.5 mile downstream. The name, first recorded in the 7th century, means "Frome crossing point", probably signifying

112-619: A broad beam canal, joins the Severn at Hawford , near to the River Salwarpe , and connects to the Droitwich Canal (narrow beam) in the name town, which then forms a link to the Worcester and Birmingham Canal. The two Droitwich canals re-opened in 2010 after major restoration. The Gloucester and Sharpness Canal connects the Severn at Gloucester to the Severn at Sharpness , avoiding a stretch of

168-531: A crossing of the Severn by the mouth of the Frome. However, by the 16th century the ferry was further downstream at Framilode Passage, and the ferry across the Severn here continued in occasional use until the Second World War. In 1126 Gloucester Abbey acquired a mill on the Frome at Framilode, and both corn mills and fulling mills continued to operate in the village until the late 18th century. The opening of

224-490: A radical restructuring of the vowel system. Notes: Through comparative linguistics , it is possible to approximately reconstruct the declension paradigms of Common Brittonic: Notes: Notes: Notes: Brittonic-derived place names are scattered across Great Britain, with many occurring in the West Country ; however, some of these may be pre-Celtic. The best example is perhaps that of each (river) Avon , which comes from

280-858: Is the longest river in Great Britain . It is also the river with the most voluminous flow of water by far in all of England and Wales , with an average flow rate of 107 m /s (3,800 cu ft/s) at Apperley , Gloucestershire. It rises in the Cambrian Mountains in mid Wales , at an altitude of 2,001 feet (610 m), on the Plynlimon massif, which lies close to the Ceredigion / Powys border near Llanidloes . The river then flows through Shropshire , Worcestershire and Gloucestershire . The county towns of Shrewsbury , Worcester and Gloucester lie on its course. The Severn's major tributaries are

336-624: Is thought to derive from a British word * sabrinā , possibly from an older form * samarosina , meaning "land of summertime fallow". During the Roman occupation the Severn was known by the Romano-British Latin name Sabrina . Milton 's 1634 masque Comus makes Sabrina a nymph who had drowned in the river. In Shrewsbury , there is now a statue of Sabrina in the Dingle Gardens at

392-408: Is tidal. Several more villages sit beside the tidal stretch. Amongst these are Elmore , Epney and Framilode on the east bank and Minsterworth , Broadoak and Newnham on Severn on the west bank. The Severn is bridged at many places, and many of these bridges are notable in their own right. The Iron Bridge at Ironbridge was the world's first iron arch bridge. Several other bridges crossing

448-583: The Arkendale H and Wastdale H died in the accident. There have been frequent floods in Shrewsbury , Bewdley and elsewhere. More recently the river flooded during the 2007 United Kingdom floods and the 2019–20 United Kingdom floods . There is a public right of navigation between Pool Quay , near Welshpool , and Stourport. However this stretch of the river has little traffic, other than small boats, canoes and some tour boats in Shrewsbury. Below Stourport, where

504-616: The Clent Hills , near St Kenelm's Church at Romsley . It flows north into the adjacent West Midlands at Halesowen . It then flows westwards through Cradley Heath and Stourbridge , where it leaves the Black Country . It is joined by the Smestow Brook at Prestwood before it winds around southwards to Kinver , and then flows back into Worcestershire. It then passes through Wolverley , Kidderminster and Wilden to its confluence with

560-585: The Firth of Forth . Cumbric disappeared in the 12th century, and in the far south-west, Cornish probably became extinct in the 18th century, though its use has since been revived . O'Rahilly's historical model suggests a Brittonic language in Ireland before the introduction of the Goidelic languages , but this view has not found wide acceptance. Welsh and Breton are the only daughter languages that have survived fully into

616-760: The Gloucester and Sharpness Canal provides a navigable channel south. Between the docks and Lower Parting Llanthony Weir marks the Normal Tidal Limit (NTL) of the East Channel of the river. In the tidal section of the river below Gloucester, the Gloucester Harbour Trustees are the competent harbour authority. The Trustees maintain navigation lights at various points along the river (including on Chapel Rock and Lyde Rock, and leading lights at Slime Road, Sheperdine and Berkeley Pill). There are locks on

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672-534: The Irish Sea through Cheshire causing a large lake to develop across much of Shropshire. It was supposed that this lake, named as Lake Lapworth , overtopped its southern margin and rapidly cut down to form the Ironbridge Gorge providing the Severn with a southerly exit to the sea as remains the case today. An alternative theory which has gained favour in recent years does away with Lake Lapworth, suggesting that

728-520: The Quarry , as well as a metal sculpture erected in 2013. There is a different deity associated with the Severn Estuary: Nodens , represented as mounted on a seahorse , riding on the crest of the Severn bore . The Welsh form of the name is Afon Hafren ( pronounced [ˈavɔn ˈhavrɛn] ) first recorded in the 12th-century Historia Regum Britanniae . The Old Welsh form of

784-626: The River Tern , after flowing south from Market Drayton and being joined by the River Meese and the River Roden , meets the Severn at Attingham Park . The River Worfe joins the Severn's left bank just above Bridgnorth , before the Mor, Borle and Dowles brooks join on the opposite bank over the next few miles, the last-named draining Wyre Forest . The River Stour rises in the north of Worcestershire in

840-726: The Second Severn Crossing road bridge, and carries the South Wales Main Line section of the Great Western Main Line under the channel. The original line built before the Severn Tunnel was the South Wales Railway from Gloucester , that followed the estuary alongside present day stations of Lydney , Chepstow , Caldicot and Severn Tunnel Junction to Newport . Cars could also be transported through

896-467: The Stroudwater Canal in 1779 created water shortages, and by 1786 the mills were used for tinplate manufacture. By 1831 the mills were used as a forge, but were derelict by 1841. The Stroudwater Canal also entered the Severn at Framilode, and a canal basin was built at Framilode in 1794 and 1795. After the Gloucester and Berkeley Canal opened in 1827 use of the stretch between the junction with

952-700: The Usk all flow into the estuarine section of the Severn. The main tributaries are described in sequence below. The first tributary of significance is the Afon Dulas , joining from the south immediately upstream of Llanidloes , with the Afon Clywedog joining in the town. The Afon Cerist , bolstered by the Afon Trannon , and the Afon Carno join as left bank tributaries immediately upstream of Caersws. Mochdre Brook enters on

1008-907: The Vyrnwy , the Tern , the Teme , the Warwickshire Avon , and the Worcestershire Stour . By convention, the River Severn is usually considered to end, and the Severn Estuary to begin, after the Second Severn Crossing , between Severn Beach in South Gloucestershire and Sudbrook, Monmouthshire . The total area of the Estuary's drainage basin is 4,409 square miles (11,419 km ). That figure excludes

1064-546: The 21st century. Cornish fell out of use in the 1700s but has since undergone a revival . Cumbric and Pictish are extinct and today spoken only in the form of loanwords in English, Scots , and Scottish Gaelic . The early Common Brittonic vowel inventory is effectively identical to that of Proto-Celtic. /ɨ/ and /ʉ/ have not developed yet. By late Common Brittonic, the New Quantity System had occurred, leading to

1120-506: The Hatherley and Horsbere brooks, before it reaches Gloucester. The River Leadon enters the tidal West Channel of the Severn at Over, immediately west of Gloucester. The River Frome is the second significant tributary to enter the tidal stretch of the Severn, doing so at Framilode. Bideford Brook drains the easternmost part of the Forest of Dean , entering the Severn estuary east of Blakeney . On

1176-793: The Romanised towns and their descendants, and later from church use. By 500–550 AD, Common Brittonic had diverged into the Neo-Brittonic dialects: Old Welsh primarily in Wales, Old Cornish in Cornwall, Old Breton in what is now Brittany, Cumbric in Northern England and Southern Scotland, and probably Pictish in Northern Scotland. The modern forms of Breton and Welsh are the only direct descendants of Common Brittonic to have survived fully into

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1232-536: The SSW-NNE aligned valley either side of Welshpool is there any obvious relationship to geological structure; the valley follows the lines of the Severn Valley Faults. For much of the rest of its course it runs directly across geological structures. It was first proposed in the 1900s that the former northerly course of the upper Severn was disrupted during the course of the ice age by the blocking of its access to

1288-594: The Severn Estuary from the mid 19th century to the late 1970s by P & A Campbell of Bristol . The vessels, Cardiff Queen , Bristol Queen , Glen Usk , Glen Gower and Britannia all operated on this route in the 1950s and 1960s. Since 1986 Waverley Excursions has operated occasional sailings to Sharpness and Lydney by the MV Balmoral . A number of ferries were also operated on the tidal river, for example at New Passage , Purton and Arlingham . The last ferry

1344-457: The Severn Tunnel. In the 1950s three trains a day made round trips between Severn Tunnel Junction and Pilning . The vehicles were loaded onto open flat bed carriages and pulled by a small pannier tank locomotive , although sometimes they were joined to a scheduled passenger train. The prudent owner paid to cover the vehicle with a sheet, as sparks often flew when the steam locomotive tackled

1400-527: The Severn at Stourport-on-Severn . The Dick Brook , Shrawley Brook and Grimley Brook enter on the right bank before the River Salwarpe , which runs through Droitwich enters on the opposite (east) bank. The River Teme flows eastwards from its source in Mid Wales , straddling the border between Shropshire and Herefordshire ; it is joined by the River Onny , River Corve and River Rea before it finally joins

1456-463: The Severn on the southern edge of Worcester . Bushley Brook joins just upstream of the confluence of the Warwickshire Avon with the Severn at Tewkesbury . One of several Avons, this one flows west through Rugby , Warwick and Stratford-upon-Avon . It is then joined by its tributary the River Arrow , before joining the Severn. The rivers Swilgate and Chelt also join the Severn's left bank, as do

1512-556: The Shropshire Plain, these lower Palaeozoic rocks are replaced by Permian and Triassic age strata though largely unseen beneath a thick cover of Quaternary deposits. Certain stretches also run across Carboniferous strata as at Shrewsbury and for much of the distance between Ironbridge and Bewdley. Permo-Triassic bedrock then continues until the Severn moves intermittently onto the Jurassic outcrop from Tewkesbury southwards. Only in

1568-692: The area of the River Wye and the Bristol Avon , both of which flow into the Severn Estuary. The Estuary discharges into the Bristol Channel , which opens into the Celtic Sea and from there into the Atlantic Ocean. An etymology has been proposed, which signifies that 'Severn' is an anglicized version of a ancient Celtic phrase signifying 'a gap (in the coastline)', referring to the estuary. The name Severn

1624-488: The boats The Pride of the Midlands and The Earl Grosvenor . Common Brittonic It is a form of Insular Celtic , descended from Proto-Celtic , a theorized parent language that, by the first half of the first millennium BC, was diverging into separate dialects or languages. Pictish is linked, likely as a sister language or a descendant branch. Evidence from early and modern Welsh shows that Common Brittonic

1680-605: The club-rush growing along the banks of the River Severn to make wicker baskets. The name history shows evidence of Scandinavian influence: In the Summer of 893 a coalition of all of the Danish armies in England made a determined attempt to annex western Mercia to Danish Mercia. The Anglo-Saxon Chronicle (ASC) recorded an account of the Battle of Buttington , and included this description of

1736-528: The county of Powys . The first town it encounters downstream of its source is Llanidloes where it is joined by the Dulas and the Clywedog. It flows past the villages of Llandinam and Caersws before reaching Newtown . It then runs by Abermule and Cilcewydd before flowing beside Welshpool , the last town on its course in Wales. Entering Shropshire and England, a few villages such as Shrawardine sit back from

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1792-414: The final word has been rendered cuamiinai .) This text is often seen as: 'The affixed – Deuina, Deieda, Andagin [and] Uindiorix – I have bound'; else, at the opposite extreme, taking into account case-marking – -rix 'king' nominative, andagin 'worthless woman' accusative, dewina deieda 'divine Deieda' nominative/vocative – is: 'May I, Windiorix for/at Cuamena defeat [or 'summon to justice']

1848-457: The language differed little from that of Gaul . Comparison with what is known of Gaulish confirms the similarity. Pictish , which became extinct around 1000 years ago, was the spoken language of the Picts in Northern Scotland. Despite significant debate as to whether this language was Celtic, items such as geographical and personal names documented in the region gave evidence that this language

1904-527: The lower Severn to enable seagoing boats to reach as far as Stourport. The most northerly lock is at Lincomb, about 1 mile (1.6 km) downstream from Stourport. The Staffordshire and Worcestershire Canal , the Worcester and Birmingham Canal , (both narrow beam) and the Herefordshire and Gloucestershire Canal join the Severn at Stourport, Worcester and Gloucester respectively. The Droitwich Barge Canal ,

1960-558: The modern day. No documents in the language have been found, but a few inscriptions have been identified. The Bath curse tablets , found in the Roman feeder pool at Bath, Somerset ( Aquae Sulis ), bear about 150 names – about 50% Celtic (but not necessarily Brittonic). An inscription on a metal pendant (discovered there in 1979) seems to contain an ancient Brittonic curse: " Adixoui Deuina Deieda Andagin Uindiorix cuamenai ". (Sometimes

2016-581: The name Habren was recorded c.800. Documented history of the Welsh name: The toponym for Habren might be: The English form of the name (" Severn ") is derived from Old English Sæfern . However the name is also influenced by English dialect seave (" sedge, rush ") hence the origin of the name Seaverne recorded in the 16th–17th century. Common club-rush ( Schoenoplectus lacustris ) prefers to grow in shallow water such as that found in ponds, streams and river margins. The Hwicce people used

2072-654: The name of the Dalvík – Grímsey ferry in Iceland . The River Severn's current form is the result of a multi-million year history and complex underlying geology but is in part the result of glaciation during the last ice age in the Pleistocene epoch of the Quaternary period. Within Wales, the river runs through a landscape formed in Ordovician and Silurian rocks. As it enters

2128-639: The new canal and the Severn declined, and in the 1920s the section was blocked and fell into disuse. The basin was subsequently filled. Framilode became an ecclesiastical parish in 1855, and the parish church of St Peter was built in 1854. The church is a Grade II listed building . The ecclesiastical parish was merged with the parish of Fretherne in 1949, and is now part of the Severnside group of parishes. [REDACTED] Media related to Framilode at Wikimedia Commons River Severn The River Severn ( Welsh : Afon Hafren , pronounced [ˈavɔn ˈhavrɛn] ), at 220 miles (354 km) long,

2184-485: The opposite (southeast) bank the flow of the River Cam is usurped by the Gloucester and Sharpness Canal before reaching the estuary. The Lyd enters the west bank of the estuary at Lydney Harbour , opposite the place where Berkeley Pill carries the waters of the Little Avon River into it. The final tributary before the Severn Bridge is the collection of streams which enter via Oldbury Pill. The River Wye, from its source in Plynlimon in Wales (2 miles (3 km) from

2240-478: The river as it meanders eastwards towards the county town of Shrewsbury . More villages, notably Atcham , Wroxeter and Cressage sit beside the river as it turns southeast and heads for the gorge at Ironbridge before turning south for Bridgnorth . The Shropshire villages of Quatford and Hampton Loade and the Worcestershire village of Upper Arley follow, before the Severn runs through Bewdley and Stourport-on-Severn in quick succession. The river then passes

2296-439: The river is more navigable for larger craft, users must obtain permits from the Canal & River Trust , who are the navigation authority . During spring freshet the river can be closed to navigation. At Upper Parting above Gloucester, the river divides into two, and flows either side of Alney Island to Lower Parting. The West Channel is no longer navigable. The East Channel is navigable as far as Gloucester Docks, from where

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2352-432: The river were designed and built by the engineer Thomas Telford . The two major road bridges of the Severn crossing link south eastern Wales with the southern counties of England. Prior to the construction of the first bridge in 1966, the channel was crossed by the Aust Ferry . Other notable bridges include: The Severn Tunnel , completed in 1886 by John Hawkshaw on behalf of the Great Western Railway , lies near

2408-446: The route taken by the Danes : "... Foron þa up be Temese oþþæt hie gedydon æt Sæferne , þa up be Sæferne . The Seafarer (poem) ..."þæt he a his sæfore sorge næbbe, to hwon hine Dryhten gedon wille." ..."that he never in his seafaring has a worry, as to what his Lord will do to him." — A passage in Old English poem The name Sæfern might be related to: The Old Norse name Sæfari ("Seafarer") lives on as

2464-501: The slope leading to the tunnel exit. A railway coach was provided for passengers and drivers. Reservations could be made and the fee for the car was about thirty shillings (£1.50) in the early 1950s. There have been many disasters on the Severn , which have claimed perhaps 300 lives, depending on sources, especially during the 20th century. The Severn Railway Bridge was badly damaged by the collision of two river barges in 1960, which led to its demolition in 1970. Five crew members of both

2520-420: The source of the Severn), flows generally south east through the Welsh towns of Rhayader and Builth Wells . It enters Herefordshire , flows through Hereford , and is shortly afterwards joined by the River Lugg , before flowing through Ross-on-Wye and Monmouth , and then southwards where it forms part of the border between England ( Forest of Dean ) and Wales . The Wye flows into the Severn estuary south of

2576-536: The tidal river which is dangerous to navigate. The Stroudwater Navigation used to join the tidal Severn at Framilode , but since the 1920s has connected to the Severn only via the Gloucester and Sharpness Canal. The Lydney Canal is a short canal which connects Lydney to the river. The section of the river between Tewkesbury and Worcester forms part of the Avon Ring , a 109-mile (175 km) circular cruising route which includes 129 locks and covers parts of three other waterways. Paddle steamers were operated in

2632-512: The time of 75–100 AD. The term Pritenic is controversial. In 2015, linguist Guto Rhys concluded that most proposals that Pictish diverged from Brittonic before c.  500 AD were incorrect, questionable, or of little importance, and that a lack of evidence to distinguish Brittonic and Pictish rendered the term Pritenic "redundant". Common Brittonic vied with Latin after the Roman conquest of Britain in 43 AD, at least in major settlements. Latin words were widely borrowed by its speakers in

2688-406: The town of Chepstow . The Mounton Brook and Nedern Brooks enter on the Monmouthshire side between the two motorway crossings. The Port of Bristol is on the Severn Estuary , where another River Avon flows into it through the Avon Gorge . The River Usk and the Ebbw River flow into the Severn Estuary at Uskmouth just south of Newport . The river's course within Wales lies wholly within

2744-420: The upper Severn flowed beneath the icesheet in a bedrock hollow known as the Severn Trench eastwards from Melverley to the Ironbridge Gorge. It is possible that the trench and gorge were cut over successive ice ages. Over its length, there are a large number of tributaries, but the three largest feeding the non-tidal river are the Vyrnwy , the Teme and the Warwickshire Avon . The Wye , the Bristol Avon and

2800-405: The villages of Astley Burf and Holt Fleet before entry into the city of Worcester . Several villages sit back from the river before it runs by Upton-upon-Severn and then enters Gloucestershire as it joins with the Warwickshire Avon outside of Tewkesbury . A few more villages intervene, notable amongst which is Maisemore before the river enters the city of Gloucester from which point it

2856-405: The waters of the Banwy , Cain and Tanat , before forming part of the border between England and Wales, and joining the Severn near Melverley , Shropshire. The River Perry joins on the left bank above Shrewsbury , while both the Rad Brook and the Rea Brook , which flows northeast from its source at Marton Pool near the Welsh border, join the Severn within the town. The left bank tributary,

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2912-446: The western edge of Newtown, followed by the Bechan Brook just northeast of the town. The Mule enters at Abermule , and the River Rhiw east of Berriew , followed shortly by the Camlad which rises above Churchstoke and by the Luggy Brook. The left bank Sylfaen Brook enters at Welshpool , and the Bele Brook via the New Cut east of Arddlin . The River Vyrnwy, which begins at Lake Vyrnwy , flows eastwards through Powys , gathering

2968-585: The worthless woman, [oh] divine Deieda.' A tin/lead sheet retains part of nine text lines, damaged, with likely Brittonic names. Local Roman Britain toponyms (place names) are evidentiary, recorded in Latinised forms by Ptolemy 's Geography discussed by Rivet and Smith in their book of that name published in 1979. They show most names he used were from the Brittonic language. Some place names still contain elements derived from it. Tribe names and some Brittonic personal names are also taken down by Greeks and, mainly, Romans. Tacitus 's Agricola says that

3024-481: Was most closely aligned with the Brittonic branch of Celtic languages. The question of the extent to which this language was distinguished, and the date of divergence, from the rest of Brittonic, was historically disputed. Pritenic (also Pretanic and Prittenic ) is a term coined in 1955 by Kenneth H. Jackson to describe a hypothetical Roman-era (1st to 5th centuries) predecessor to the Pictish language. Jackson saw Pritenic as having diverged from Brittonic around

3080-549: Was significantly influenced by Latin during the Roman period , especially in terms related to the church and Christianity . By the sixth century AD, the languages of the Celtic Britons were rapidly diverging into Neo-Brittonic : Welsh , Cumbric , Cornish , Breton , and possibly the Pictish language . Over the next three centuries, Brittonic was replaced by Scottish Gaelic in most of Scotland, and by Old English (from which descend Modern English and Scots ) throughout most of modern England as well as Scotland south of

3136-419: Was the Aust Ferry , which closed in 1966 when the Severn Bridge opened. One of the Aust ferries, Severn Princess , is still in Chepstow although largely derelict. Currently the only passenger boat operating between Shrewsbury & Gloucester is the 'River King' vessel that operates in Stourport. Worcester River Cruises used to run boat trips up and down the river between Tewkesbury and Stourport, operating

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