River Kelvin in the context of Forth and Clyde Canal


River Kelvin in the context of Forth and Clyde Canal

⭐ Core Definition: River Kelvin

The River Kelvin (Scottish Gaelic: Abhainn Cheilbhinn) is a tributary of the River Clyde in northern and northeastern Glasgow, Scotland. It rises on the moor south east of the village of Banton, east of Kilsyth. At almost 22 miles (35 km) long, it initially flows south to Dullatur Bog where it falls into a man made trench and takes a ninety degree turn flowing west through Strathkelvin and along the northern boundary of the bog parallel with the Forth and Clyde Canal.

The University of Glasgow is situated by the river, in Gilmorehill. In 1892, the title of Baron Kelvin was created for physicist and engineer William Thomson, a professor at the university. The name "kelvin" for the unit of temperature, chosen in honour of Lord Kelvin, thus traces its origins to the river.

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River Kelvin in the context of River Clyde

The River Clyde (Scottish Gaelic: Abhainn Chluaidh, pronounced [ˈavɪɲ ˈxl̪ˠuəj]) is a major river of western Scotland and the third-longest in the country at about 170 kilometres (110 mi) in length. Its river network extends to 4,244 km and drains a basin of 1,903 km, expanding to 3,854 km when the Clyde estuary system with the Kelvin, White Cart, Black Cart and Leven is included. Around 1.79 million people, 33.8% of Scotland's population, live within this catchment. The river rises in the Lowther Hills and flows north-west through South Lanarkshire and Glasgow before entering the Firth of Clyde.

From the late 18th century the upper estuary and river through Glasgow were systematically engineered using groynes, longitudinal training walls and continuous dredging, and by removing rocky obstructions such as a large part of the Elderslie Rock. This was done to enable ocean-going access and support Glasgow's rise as a world centre of shipbuilding and marine engineering in the 19th and 20th centuries.

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River Kelvin in the context of Govan

Govan (/ˈɡʌvən/ GUV-ən; Cumbric: Gwovan; Scots: Gouan; Scottish Gaelic: Baile a' Ghobhainn) is a district, parish, and former burgh now part of southwest Glasgow, Scotland. It is situated 2+12 miles (4 kilometres) west of Glasgow city centre, on the south bank of the River Clyde, opposite the mouth of the River Kelvin and the district of Partick. Historically it was part of the County of Lanark.

In the early medieval period, the site of the present Govan Old churchyard was established as a Christian centre for the Brittonic Kingdom of Alt Clut (Dumbarton Rock) and its successor realm, the Kingdom of Strathclyde. This latter kingdom, established in the aftermath of the Viking siege and capture of Alt Clut by Vikings from Dublin in 870, created the stone sculptures known today as the Govan Stones.

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River Kelvin in the context of Strathkelvin

55°55′41″N 4°08′02″W / 55.928°N 4.134°W / 55.928; -4.134

Strathkelvin (Scottish Gaelic: Srath Chealbhainn) is the strath (valley) of the River Kelvin in west central Scotland, lying north-east of Glasgow. The name Strathkelvin was used between 1975 and 1996 for one of nineteen local government districts in the Strathclyde region.

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