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Mentioned the river Devon flows into to the Forth at Cambus, and changed Queensferry in a link to the wiki page.
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The '''River Forth''' (''Uisge For'' and ''Abhainn Dhubh'' (meaning "black river") in Gaelic), 47 km (29 miles) long, is the major [[river]] draining the eastern part of the central belt of [[Scotland]].
The '''River Forth''' (''Uisge For'' and ''Abhainn Dhubh'' (meaning "black river") in Gaelic), 47 km (29 miles) long, is the major [[river]] draining the eastern part of the central belt of [[Scotland]].


The Forth rises in [[Loch Ard]] in [[The Trossachs]], a [[mountain]] range some 30 km (19 miles) west of [[Stirling]]. It flows roughly eastward, through [[Aberfoyle]], joining with the [[Duchray Water]] and [[Kelty Water]], and out over the flat expanse of the [[Flanders Moss]]. It is then joined by the [[River Teith]] (which itself drains [[Loch Venachar]], [[Loch Lubnaig]], [[Loch Katrine]], and [[Loch Voil]]) and the [[Allan Water|River Allan]], before meandering through the ancient city of Stirling. At Stirling the river widens and becomes [[tide|tidal]], and it is here that the last (seasonal) [[ford (river)|ford]] of the river exists. From Stirling, the Forth flows east over the [[Carse]] of Stirling and past the towns of [[Alloa]] and [[Airth]]. Upon reaching [[Kincardine on Forth|Kincardine]] the river begins to widen into an [[estuary]], the [[Firth of Forth]].
The Forth rises in [[Loch Ard]] in [[The Trossachs]], a [[mountain]] range some 30 km (19 miles) west of [[Stirling]]. It flows roughly eastward, through [[Aberfoyle]], joining with the [[Duchray Water]] and [[Kelty Water]], and out over the flat expanse of the [[Flanders Moss]]. It is then joined by the [[River Teith]] (which itself drains [[Loch Venachar]], [[Loch Lubnaig]], [[Loch Katrine]], and [[Loch Voil]]) and the [[Allan Water|River Allan]], before meandering through the ancient city of Stirling. At Stirling the river widens and becomes [[tide|tidal]], and it is here that the last (seasonal) [[ford (river)|ford]] of the river exists. From Stirling, the Forth flows east over the [[Carse]] of Stirling and past the towns of Cambus (where it is joined by the river [[River_Devon%2C_Clackmannanshire|Devon]]), [[Alloa]] and [[Airth]]. Upon reaching [[Kincardine on Forth|Kincardine]] the river begins to widen into an [[estuary]], the [[Firth of Forth]].


[[image:Meander1.jpg|thumb|right|300px|[[Meander|Meandering]] viewed from the [[Wallace Monument]]. The river flows from right to left, and the former limit of navigation was in the left distance.]]
[[image:Meander1.jpg|thumb|right|300px|[[Meander|Meandering]] viewed from the [[Wallace Monument]]. The river flows from right to left, and the former limit of navigation was in the left distance.]]
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== Bridges over the Forth ==
== Bridges over the Forth ==


Upstream of Stirling, the river is rather small and is crossed in numerous places (although prior to modern drainage works, the ground was often treacherously marshy near the riverbank). After its [[Confluence (geography)|confluence]] with the Teith and Allan, the river is sufficiently wide that a significant bridge is required. A [[bridge]] has existed at Stirling since at least the [[13th Century]], and until the opening of the road crossing at Kincardine in [[1936]], Stirling remained the easternmost road crossing. Much further downstream (at Queensferry) the famous [[Forth Bridge (railway)|rail bridge]] opened in [[1890]] and a modern [[Forth Road Bridge|road bridge]] in [[1964]]. A swinging railway bridge between [[Alloa]] on the north shore and [[Throsk]] on the south opened in [[1885]] and was closed (and largely demolished) in [[1970]].
Upstream of Stirling, the river is rather small and is crossed in numerous places (although prior to modern drainage works, the ground was often treacherously marshy near the riverbank). After its [[Confluence (geography)|confluence]] with the Teith and Allan, the river is sufficiently wide that a significant bridge is required. A [[bridge]] has existed at Stirling since at least the [[13th Century]], and until the opening of the road crossing at Kincardine in [[1936]], Stirling remained the easternmost road crossing. Much further downstream at [[South_Queensferry|Queensferry]] the famous [[Forth Bridge (railway)|rail bridge]] opened in [[1890]] and a modern [[Forth Road Bridge|road bridge]] in [[1964]]. A swinging railway bridge between [[Alloa]] on the north shore and [[Throsk]] on the south opened in [[1885]] and was closed (and largely demolished) in [[1970]].


Plans to construct a new road bridge slightly to the West of the existing Forth road Bridge have been announced by the Scottish Executive. It is planned to open in 2016.
Plans to construct a new road bridge slightly to the West of the existing Forth road Bridge have been announced by the Scottish Executive. It is planned to open in 2016.

Revision as of 19:36, 27 March 2008

The River Forth meanders over fertile farmlands near Stirling

The River Forth (Uisge For and Abhainn Dhubh (meaning "black river") in Gaelic), 47 km (29 miles) long, is the major river draining the eastern part of the central belt of Scotland.

The Forth rises in Loch Ard in The Trossachs, a mountain range some 30 km (19 miles) west of Stirling. It flows roughly eastward, through Aberfoyle, joining with the Duchray Water and Kelty Water, and out over the flat expanse of the Flanders Moss. It is then joined by the River Teith (which itself drains Loch Venachar, Loch Lubnaig, Loch Katrine, and Loch Voil) and the River Allan, before meandering through the ancient city of Stirling. At Stirling the river widens and becomes tidal, and it is here that the last (seasonal) ford of the river exists. From Stirling, the Forth flows east over the Carse of Stirling and past the towns of Cambus (where it is joined by the river Devon), Alloa and Airth. Upon reaching Kincardine the river begins to widen into an estuary, the Firth of Forth.

Meandering viewed from the Wallace Monument. The river flows from right to left, and the former limit of navigation was in the left distance.

Settlements on the Forth

There are a number of towns which line the shores, as well as the petrochemical complexes at Grangemouth, the commercial docks at Leith, oilrig construction yards at Methil, the ship-breaking facility at Inverkeithing and the naval dockyard at Rosyth, with numerous other industrial areas including the Forth Bridgehead area, Burntisland, Kirkcaldy, Bo'ness and Leven.

Navigation on the Forth

In medieval times the Forth was navigable at least as far as Stirling, but silting and the increase in ship sizes now mean that traffic upstream of Kincardine is rare.

Bridges over the Forth

Upstream of Stirling, the river is rather small and is crossed in numerous places (although prior to modern drainage works, the ground was often treacherously marshy near the riverbank). After its confluence with the Teith and Allan, the river is sufficiently wide that a significant bridge is required. A bridge has existed at Stirling since at least the 13th Century, and until the opening of the road crossing at Kincardine in 1936, Stirling remained the easternmost road crossing. Much further downstream at Queensferry the famous rail bridge opened in 1890 and a modern road bridge in 1964. A swinging railway bridge between Alloa on the north shore and Throsk on the south opened in 1885 and was closed (and largely demolished) in 1970.

Plans to construct a new road bridge slightly to the West of the existing Forth road Bridge have been announced by the Scottish Executive. It is planned to open in 2016.

See also