Source (river) in the context of "River Avon, Bristol"

Play Trivia Questions online!

or

Skip to study material about Source (river) in the context of "River Avon, Bristol"

Ad spacer

⭐ Core Definition: Source (river)

The headwater of a river or stream is the geographical point of its beginning, specifically where surface runoff water begins to accumulate into a flowing channel of water. A river or stream into which one or many tributary rivers or streams flow has many headwaters, these being all of the individual headwaters of its tributaries. Each headwater is one of the river or stream's sources, as it is the place where surface runoffs from rainwater, meltwater, or spring water begin accumulating into a more substantial and consistent flow that becomes a first-order tributary of that river or stream. The tributary with the longest channel of all the tributaries to a river or stream, such length measured from that tributary's headwater to its mouth where it discharges into the river or stream, is the main stem of the river or stream in question.

↓ Menu

>>>PUT SHARE BUTTONS HERE<<<
In this Dossier

Source (river) in the context of River Cole, West Midlands

The River Cole is a 25-mile-long (40-kilometre) river in the English Midlands. It rises on the lower slopes of Forhill, one of the south-western ramparts of the Birmingham Plateau, at Red Hill and flows south before flowing largely north-east across the plateau to enter the River Blythe below Coleshill, near Ladywalk, shortly before the Blythe meets the Tame. This then joins the Trent, whose waters reach the North Sea via the Humber Estuary. Its source is very near the main watershed of Midland England: tributaries are few and very short except in the lower reaches, so the Cole is only a small stream. The stretch between Shard End and Tyseley formed part of the historic border between Warwickshire and Worcestershire.

↑ Return to Menu

Source (river) in the context of Bristol Avon

The River Avon (/ˈvən/ AY-vən) is a river in the southwest of England. To distinguish it from a number of other rivers of the same name, it is often called the Bristol Avon. The name 'Avon' is loaned from an ancestor of the Welsh word afon, meaning 'river'.

The Avon rises just north of the village of Acton Turville in South Gloucestershire, before flowing through Wiltshire into Somerset. In its lower reaches from Bath (where it meets the Kennet and Avon Canal) to the Severn Estuary at Avonmouth near Bristol, the river is navigable and is known as the Avon Navigation.

↑ Return to Menu

Source (river) in the context of River Axe (Bristol Channel)

The River Axe is a river in South West England. The river is formed by water entering swallets in the limestone and rises from the ground at Wookey Hole Caves in the Mendip Hills in Somerset, and runs through a V-shaped valley. The geology of the area is limestone and the water reaches Wookey Hole in a series of underground channels that have eroded through the soluble limestone. The river mouth is in Weston Bay on the Bristol Channel.

The river was navigable from the Middle Ages until 1915, during early centuries of which seeing some European trade.

↑ Return to Menu

Source (river) in the context of River Welland

The River Welland is a lowland river in the east of England, some 65 miles (105 km) long. It drains part of the Midlands eastwards to The Wash. The river rises in the Hothorpe Hills, at Sibbertoft in Northamptonshire, then flows generally northeast to Market Harborough, Stamford and Spalding, to reach The Wash near Fosdyke. It is a major waterway across the part of the Fens called South Holland, and is one of the Fenland rivers that were laid out with washlands. There are two channels between widely spaced embankments with the intention that flood waters would have space in which to spread while the tide in the estuary prevented free egress. However, after the floods of 1947, new works such as the Coronation Channel were constructed to control flooding in Spalding, and the washlands are no longer used solely as pasture, but may be used for arable farming.

Significant improvements were made to the river in the 1660s, when a new cut with 10 locks was constructed between Stamford and Market Deeping, and two locks were built on the river section below Market Deeping. The canal section was known as the Stamford Canal, and was the longest canal with locks in Britain when it was built. The river provided the final outlet to the sea for land drainage schemes implemented in the seventeenth century, although they were not completely successful until a steam-powered pumping station was built at Pode Hole in 1827. Navigation on the upper river, including the Stamford Canal, had ceased by 1863, but Spalding remained an active port until the end of the Second World War.

↑ Return to Menu

Source (river) in the context of River Dee, Aberdeenshire

The River Dee (Scottish Gaelic: Uisge Dhè) is a river in Aberdeenshire, Scotland. It rises in the Cairngorms and flows through southern Aberdeenshire to reach the North Sea at Aberdeen. The area it passes through is known as Deeside, or Royal Deeside in the region between Braemar and Banchory because Queen Victoria came for a visit there in 1848 and greatly enjoyed herself. She and her husband, Prince Albert, built Balmoral Castle there which replaced an older castle.

Deeside is a popular area for tourists, due to the combination of its scenery and historic royal associations. It is part of the Cairngorms National Park, and the Deeside and Lochnagar National Scenic Area. The Dee is popular with anglers and is one of the most famous salmon fishing rivers in the world.

↑ Return to Menu

Source (river) in the context of River Tyne, Scotland

The River Tyne is a river in Scotland. It rises in the Moorfoot Hills in Midlothian near Tynehead to thesouth of Edinburgh, at the junction of the B6458 and the B6367. It continues approximately 30 miles (50 kilometres) northeast, and empties into the North Sea near Belhaven.

↑ Return to Menu