Torwood Castle
Torwood Castle is a castle ruin near the village of Torwood, in the Falkirk Council area of central Scotland.
Articles near the latitude and longitude of Bannockburn
Satellite map of Bannockburn
Bannockburn (Scottish Gaelic Allt a' Bhonnaich) is a town immediately south of the city of Stirling in Scotland. It is named after the Bannock Burn, a burn (small stream) running through the town before flowing into the River Forth.
Population: 8,033
Latitude: 56° 05' 23.21" N
Longitude: -3° 54' 39.31" W
Articles of interest in Bannockburn
219 Articles of interest near Bannockburn, United Kingdom
Show all articles in the mapThistles Centre
The Thistles Shopping Centre is located in Stirling, Scotland. The shopping centre caters for over 500,000 sq ft of retail, providing 87 units in total, since opening in 1977.
Stirling and Falkirk
Stirling and Falkirk is a lieutenancy area of Scotland. It consists of the local government areas of Stirling and Falkirk, which cover the same areas as the previous districts from 1975—1996.
River Teith
The River Teith is a river in Scotland, which is formed from the confluence of two smaller rivers, the Garbh Uisge (River Leny) and Eas Gobhain at Callander, Stirlingshire.
Reddingmuirhead
Reddingmuirhead is a village located in Stirlingshire, Falkirk council area, Central Scotland. A few hundred yards uphill from the village of Redding, it is between Shieldhill and Brightons.
Ochil Fault
The Ochil Fault is the geological feature which defines the southern edge of the Ochil Hills escarpment, Scotland.
Laurieston, Falkirk
Laurieston is a village in the Falkirk council area in Central Scotland. It is 1.5 miles (2.4 km) east Falkirk, 1.6 miles (2.6 km) south-west of Grangemouth and 1.6 miles (2.6 km) west of Polmont.
Falkirk Old Parish Church
Falkirk Old & St. Modan's Parish Church is a congregation of the Church of Scotland in Falkirk, central Scotland. The medieval Old Parish Church is located in the centre of Falkirk, and may have been founded as early as the 7th century. The church w…
Doune Hillclimb
Doune Hillclimb, Carse of Cambus, near Doune in the district of Stirling, Scotland, is the home of the only round of the British Hill Climb Championship currently to be held in Scotland, (Bo'ness, Fintray and the Rest And Be Thankful have featured i…
Denny High School
Denny High School in Scotland is a non-denominational public secondary school.
Colzium
Colzium House and Estate (pronounced "Colly-um") is about 500 metres to the north-east of Kilsyth, North Lanarkshire, Scotland.
Cambuskenneth
Cambuskenneth (Scottish Gaelic: Camas Choinnich pronounced [ˈkʰamas̪ ˈs̪kʲɛnɪl] ) is a village in the city of Stirling, located in central Scotland. It has a population of 250 and is the site of the historic Cambuskenneth Abbey. It is situated by th…
Banton, North Lanarkshire
Banton is a village located near to the town of Kilsyth in Scotland. Originally a cluster of houses and a farm to the north (now referred to as High Banton) was what existed of the village and then coal-mining brought about the settlement we see tod…
Alloa Swing Bridge
The Alloa Swing Bridge was a railway swing bridge across the River Forth that connected Throsk and Alloa as part of the Alloa Railway.
Alloa Academy
Alloa Academy is a six-year state-funded comprehensive school, serving the town of Alloa in Clackmannanshire, Scotland. Its roll is over 800 pupils. It has three primary schools associated with it: Redwell, Sunnyside and Park. It also welcomes pupil…
A89 road
The A89 is a trunk road in Scotland, United Kingdom. It runs from Glasgow to Newbridge in Edinburgh. It was once the A8, which has now been replaced, mostly by the M8. The A89 runs from Edinburgh for about 13 miles (21 km) to Livingston and an extra…
Westquarter
Westquarter is a village in the Falkirk council area of Scotland. The village is 1 mile (1.6 km) west of Polmont and 1.8 miles (2.9 km) south-east of the town of Falkirk.
Stirling Sill
The Stirling Sill is an outcropping of a large quartz-dolerite intrusion or sill that underlies a large part of central Scotland, and may be contiguous at great depth. The sill is of very late Carboniferous age or more probably Permian, as it penetr…