River Devon, Clackmannanshire

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River Devon
River Devon.jpg
The Devon at dusk, near Tillicoultry
Native nameDuibhe (Scottish Gaelic)
Location
Country United Kingdom
Constituent country Scotland
Physical characteristics
Mouth River Forth
  coordinates
56°07′14″N3°51′11″W / 56.12067°N 3.85312°W / 56.12067; -3.85312

The River Devon (formerly Dovan, [1] Scottish Gaelic : Duibhe) is a tributary of the River Forth in Clackmannanshire and Perth & Kinross, Scotland.

Contents

Geography and hydrology

Creation of Castlehill Reservoir, Glendevon c.1971 Creation of Castlehill Reservoir, Glendevon.png
Creation of Castlehill Reservoir, Glendevon c.1971
Castlehill Reservoir in Glen Devon Glen Devon Reservoir.jpg
Castlehill Reservoir in Glen Devon

The source of the river is Blairdenon Hill in the Ochils at an altitude of 1,800 feet (550 m). Upper areas have been dammed, creating Upper Glendevon, Lower Glendevon and Castlehill reservoirs. [2] The Devon then flows east and southeast through Glendevon, turning southwest at Crook of Devon and then continuing westwards, meandering across its flood plain along the foot of the Ochil Hills. It reaches the River Forth to the west of Alloa at the small village of Cambus.

The UK Centre for Ecology & Hydrology, (part of UK's Natural Environment Research Council, NERC) describes the catchment area thus: [3] "Headwaters are steep; lower valley is broad and very flat. Bedrock extrusive igneous rocks, 50% overlain by superficial deposits. Land use arable in the valley; grassland in headwaters, some forest." The catchment covers an area of 181 km2.

Glen Devon

18th century Bridge at Glendevon Bridge at Glendevon - geograph.org.uk - 656967.jpg
18th century Bridge at Glendevon

Glen Devon stretches from the junction of the river Devon with the dramatic Glen Eagles (a perfect U-valley) southwards to the Yetts of Muckhart where the landscape then opens into a wide flood plain. The natural landscape was greatly altered by the construction of the Castlehill Reservoir which was built around 1975.

The central village, Glendevon, lies north of the reservoir, and has for 70 years been a holiday destination for holiday cabins. Glen Devon Castle was largely destroyed by fire c.1970. Its arched entranceway still exists at the north end of the reservoir. The village contains the old coach hostelry, The Tormaukin, which still survives as a restaurant. The church and manse lie north of the main village. An 18th century bridge crosses the Devon to the south of the church.

The high level reservoirs are named Glenquey, Glensherup, after the Devon's high level tributaries, and upper and lower Frandy reservoir. All were built by German PoWs in the Second World War and are used for trout fishing. [4]

History and culture

During the Scottish Reformation, William Kirkcaldy destroyed the bridge at Tullibody in attempt to prevent French troops retreating to the Siege of Leith at the end of January 1560. However, the French took down the roof of Tullibody Kirk to bridge the Devon. [5]

The Devon was surveyed by James Watt in 1766, who claimed that by deepening the river bed it might be navigable as far as Dollar. The estimated cost of such a project was £2000.

Two songs The Banks of the Devon and Fairest Maid on Devon Banks were written in 1787 by Robert Burns, which recall Charlotte Hamilton of Mauchline whom he had met at nearby Harviestoun estate. [2]

The Devon Valley Railway was built along the strath.

Flooding

Flooded House in Tillicoultry, 26 January 2008 Tillicoultry flood - geograph.org.uk - 1562619.jpg
Flooded House in Tillicoultry, 26 January 2008

Clackmannanshire Council has recognised the threat of flooding along the Devon and has worked to address the issue on its own account and in partnership with others, including WWF-Scotland. Works undertaken on the Devon catchment include willow walling, riverside woodland and the blocking of wetland drains. [6]

River Devon in flood near Menstrie, 20 November 2009 Flooding near Menstrie Nov 2009.jpg
River Devon in flood near Menstrie, 20 November 2009

In January 2008 the Devon catchment area was 'Very Wet'. Land became saturated and rainfall resulted in run-off into rivers, reaching the river system very quickly. River flows in the region were 'Exceptionally High'. Upstream, all the Ochil reservoirs were full with Castlehill reservoir overflowing for all of that month. The flood at the upstream gauge at Castlehill was the second highest recorded. Further downstream, the water level recorded at Glenochil was the highest since records began in 1956.

Over the period of 25–26 January 2008, residential and commercial properties in part of Tillicoultry were inundated. [7] The extent of flooding was greater than had been experienced in the past and the Council appointed specialist hydrological consultants to investigate the contributory factors and advise on measures available to minimise or eliminate any future occurrence. [8]

In November 2008 and again in November 2009 extensive flooding occurred in the Hillfoots making several road bridges across the river impassable. No houses were damaged on those two occasions.

River level data at Glenochil gauging station (hourly, automatic) are now available from SEPA on-line. [9]

Related Research Articles

<span class="mw-page-title-main">Perthshire</span> Historic administrative division in Scotland

Perthshire, officially the County of Perth, is a historic county and registration county in central Scotland. Geographically it extends from Strathmore in the east, to the Pass of Drumochter in the north, Rannoch Moor and Ben Lui in the west, and Aberfoyle in the south; it borders the counties of Inverness-shire and Aberdeenshire to the north, Angus to the east, Fife, Kinross-shire, Clackmannanshire, Stirlingshire and Dunbartonshire to the south and Argyllshire to the west. It was a local government county from 1890 to 1930.

<span class="mw-page-title-main">Clackmannanshire</span> Historic county and council area of Scotland

Clackmannanshire, or the County of Clackmannan, is a historic county, council area, registration county and lieutenancy area in Scotland, bordering the council areas of Stirling, Fife, and Perth and Kinross. In terms of historic counties it borders Perthshire, Stirlingshire and Fife.

<span class="mw-page-title-main">River Forth</span> River in central Scotland

The River Forth is a major river in central Scotland, 47 km (29 mi) long, which drains into the North Sea on the east coast of the country. Its drainage basin covers much of Stirlingshire in Scotland's Central Belt. The Gaelic name for the upper reach of the river, above Stirling, is Abhainn Dubh, meaning "black river". The name for the river below the tidal reach is Uisge For.

<span class="mw-page-title-main">Alloa</span> Town in Clackmannanshire, Scotland

Alloa is a town in Clackmannanshire in the Central Lowlands of Scotland. It is on the north bank of the Forth at the spot where some say it ceases to be the River Forth and becomes the Firth of Forth. Alloa is south of the Ochil Hills, 5.5 miles (8.9 km) east of Stirling and 7.9 miles (12.7 km) north of Falkirk; by water Alloa is 25 miles (40 km) from Granton.

<span class="mw-page-title-main">Tillicoultry</span> Town in Clackmannanshire, Scotland

Tillicoultry is a town in Clackmannanshire, Scotland. Tillicoultry is usually referred to as Tilly by the locals.

<span class="mw-page-title-main">Ochil Hills</span> Range of hills in Scotland, UK

The Ochil Hills (; Scottish Gaelic: Monadh Ochail is a range of hills in Scotland north of the Forth valley bordered by the towns of Stirling, Alloa, Kinross, Auchterarder and Perth. The only major roads crossing the hills pass through Glen Devon/Glen Eagles and Glenfarg, the latter now largely replaced except for local traffic by the M90 Edinburgh-Perth motorway cutting through the eastern foothills. The hills are part of a Devonian lava extrusion whose appearance today is largely due to the Ochil Fault which results in the southern face of the hills forming an escarpment. The plateau is undulating with no prominent peak, the highest point being Ben Cleuch at 721 m. The south-flowing burns have cut deep ravines including Dollar Glen, Silver Glen and Alva Glen, often only passable with the aid of wooden walkways.

<span class="mw-page-title-main">Ochil and South Perthshire (UK Parliament constituency)</span> Parliamentary constituency in the United Kingdom, 2005 onwards

Ochil and South Perthshire is a county constituency of the House of Commons of the Parliament of the United Kingdom. It elects one Member of Parliament (MP) by the first-past-the-post system of election.

<span class="mw-page-title-main">Menstrie</span> Human settlement in Scotland

Menstrie is a village in the county of Clackmannanshire in Scotland. It is about five miles east-northeast of Stirling and is one of a string of towns that, because of their location at the foothill base of the Ochil Hills, are collectively referred to as the Hillfoots Villages or simply The Hillfoots.

<span class="mw-page-title-main">Alva, Clackmannanshire</span> Human settlement in Scotland

Alva is a small town in Clackmannanshire, set in the Central Lowlands of Scotland. It is one of a number of towns situated immediately to the south of the Ochil Hills, collectively referred to as the Hillfoots Villages or simply The Hillfoots. It is located between Tillicoultry and Menstrie. Alva had a resident population of 5,181 at the 2001 census but this has since been revised to 4,600 in 2016. It boasts many features such as a park with an event hall and a newly opened outdoor gym, and is the home of Alva Academy.

<span class="mw-page-title-main">Harviestoun</span>

Harviestoun is an estate in Tillicoultry parish, Clackmannanshire, central Scotland. It lies at the base of the Ochil Hills, around 1.5 kilometres (0.93 mi) east of Tillicoultry and 2 kilometres (1.2 mi) west of Dollar.

<span class="mw-page-title-main">Tullibody</span> Town in Clackmannanshire, Central Lowlands, Scotland

Tullibody is a town set in the Central Lowlands of Scotland. It lies north of the River Forth near to the foot of the Ochil Hills within the Forth Valley. The town is 1.8 miles (2.9 km) south-west of Alva, 1.8 miles (2.9 km) north-west of Alloa and 4.0 miles (6.4 km) east-northeast of Stirling. The town is part of the Clackmannanshire council area.

<span class="mw-page-title-main">Stirling and Dunfermline Railway</span> Former railway in Scotland

The Stirling and Dunfermline Railway was a railway in Scotland connecting Stirling and Dunfermline. It was planned by the Edinburgh and Glasgow Railway to get access to the mineral deposits on the line of route, but also as a tactical measure to keep the rival Caledonian Railway out of Fife.

The Alloa Waggonway, also known as the Alloa Railway was an early tramway. It was 2+12 miles (4 km) miles long and connected coal pits above Alloa with the harbour and a bottle manufacturer at Alloa in Clackmannanshire, Scotland. The track was wooden with an iron running surface, and wagons were drawn by horses.

Strathdevon is the strath of the River Devon in Clackmannanshire, Scotland. Strathdevon is associated with the parish of Muckhart and was up until 1971 the southernmost tip of Perthshire.

<span class="mw-page-title-main">Black Devon</span>

The Black Devon is a river in Scotland. It rises in the Cleish Hills, specifically the area known as Outh Muir, 1.5 kilometres (0.93 mi) north of Knockhill Racing Circuit, around 9 kilometres (5.6 mi) north-west of Dunfermline, Fife, with the gathering of three small streams in branch formation. The river flows westwards through Balgonar, north of Saline, and then merges with the Saline Burn. The Black Devon flows into Clackmannanshire, through the hamlet of Forestmill and past the town of Clackmannan. The Black Devon enters the River Forth south of Alloa, 1 kilometre (0.62 mi) north of Dunmore Pier.

<span class="mw-page-title-main">Tullibody Old Bridge</span> Historic site in Tullibody, Clackmannanshire

Tullibody Old Bridge, over the River Devon near Tullibody, Clackmannanshire, Scotland, dates from the early 16th century. Disused after 1915, it was restored for use by walkers and cyclists in 2003.

<span class="mw-page-title-main">Devon Valley Railway</span> Former railway line in Scotland

The Devon Valley Railway linked Alloa and Kinross in central Scotland, along a route following the valley of the River Devon. Its construction took 20 years from the first section opening in 1851, to the final section in 1871. Three railway companies were involved, and it encountered a great many problems both with finance and engineering.

<span class="mw-page-title-main">Devon Way</span>

Devon Way is a pathway in Clackmannanshire, Central Scotland. It lies on the southern section of the former Devon Valley Railway from Dollar to Tillicoultry a distance of 3+14 miles (5.2 km). It is used by for walkers, cyclists and horse riders and forms part of Route 767 on the National Cycle Network.

Crauford Tait WS was a 17th/18th century Scottish lawyer, improver and landowner and also a contemporary and friend of Robert Burns.

References

  1. Glendovan entry, Genuki.org.uk
  2. 1 2 "Devon, River". Gazetteer for Scotland. Retrieved 24 August 2014.
  3. "SEPA Gauging station 18002 - Devon at Glenochil".
  4. "Glendevon Visitor Guide, Hotels, Cottages, Things to do in Scotland".
  5. Knox, John, History of the Reformation, Book 3, e.g., Lennox, Cuthbert, ed., (1905), 191.
  6. Comment by Councillor Eddie Carrick on the Ochils Landscape Partnership and Sustainability: http://www.clacksweb.org.uk/document/2321.pdf
  7. BBC News report of flooding in Tillicoultry http://news.bbc.co.uk/1/hi/scotland/7242586.stm
  8. Clackmannanshire Council, "Report to Council of 5th June 2008: Flooding in Tillicoultry": http://www.clacksweb.org.uk/document/meeting/1/258/2533.doc
  9. "River level data for Devon @ Glenochil (NGR : NS 85815 96073)".