- published: 24 Jul 2009
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The Firth of Forth (Scottish Gaelic: Linne Foirthe) is the estuary or firth of Scotland's River Forth, where it flows into the North Sea, between Fife to the north, and West Lothian, the City of Edinburgh and East Lothian to the south. It was known as Bodotria in Roman times.
Geologically, the Firth of Forth is a fjord, formed by the Forth Glacier in the last glacial period.
The river is tidal as far inland as Stirling, but generally it is considered that the inland extent of the firth ends at the Kincardine Bridge.[citation needed]
There are a number of towns which line the shores, as well as the petrochemical complexes at Grangemouth, the commercial docks at Leith, former 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[clarification needed], Burntisland, Kirkcaldy, Bo'ness and Leven.
The Kincardine Bridge and the famous Forth Road Bridge and Forth Bridge carry traffic across the Firth. A fourth crossing, located next to the Kincardine Bridge, opened in 2008. On 1 October 2008 it was announced that the new bridge would be called the "Clackmannanshire Bridge". Another new road bridge is currently under construction alongside the Forth Road Bridge and is expected to be open in 2016.
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