Falkirk

Sister cities

• Quimper

History

An Eaglais Bhreac is a derivative formed from the Scottish Gaelic cognate of the first recorded name Egglesbreth from the Brittonic for "speckled church",), then later amended to the modern English name of Falkirk. The Latin name Varia Capella also has the same meaning. Falkirk Old Parish Church stands on the site of the medieval church, which may have been founded as early as the 7th century. The Antonine Wall, which stretches across the centre of Scotland, passed through the town and remnants of it can be seen at Callendar Park. Similar to Hadrian's Wall but built of turf rather than stone so less of it has survived, it marked the northern frontier of the Roman Empire between the Firth of Forth and Firth of Clyde during the AD 140s. Much of the best evidence of Roman occupation in Scotland has been found in Falkirk, including a large hoard of Roman coins and a cloth of tartan, thought to be the oldest ever recorded. A Roman fort was confirmed to be found by Geoff Bailey in the Pleasance area of Falkirk in 1991. A Roman themed park at Callendar House was awarded lottery funding to help raise awareness of the wall. In the 18th century the area was the cradle of Scotland's Industrial Revolution, becoming the earliest major centre of the iron-casting industry. James Watt cast some of the beams for his early steam engine designs at the Carron Iron Works in 1765. The area was at the forefront of canal construction when the Forth and Clyde Canal opened in 1790. The Union Canal (1822) provided a link to Edinburgh and early railway development followed in the 1830s and 1840s. The canals brought economic wealth to Falkirk and led to the town's growth. Through time, trunk roads and motorways followed the same canal corridors through the Falkirk area, linking the town with the…

Geography

Falkirk is located in an area of undulating topography between the Slamannan Plateau and the upper reaches of the Firth of Forth. The area to the north of Falkirk is part of the floodplain of the River Carron. Two tributaries of the River Carron - the East Burn and the West Burn flow through the town and form part of its natural drainage system. Falkirk sits at between 50 metres (164 ft) and 125 metres (410 ft) above sea level. The underlying geology of the town of Falkirk is characterised by glacial deposits. Elevations above are covered by a mixture of glacial till and boulder clay with low-lying areas covered by sandy soils and loams. }}