Harviestoun

Tillicoultry railway station served the town of Tillicoultry, Clackmannanshire, Scotland from 1851 to 1964 on the Devon Valley Railway and the Stirling and Dunfermline Railway.

Tillicoultry ( TIL-ee-KOO-tree; Scottish Gaelic: Tulach Cultraidh, perhaps from older Gaelic Tullich-cul-tir, or "the mount/hill at the back of the country") is a town in Clackmannanshire, Scotland. Tillicoultry is usually referred to as Tilly by the locals. One of the Hillfoots Villages on the A91, which runs from Stirling to St. Andrews, Tillicoultry is situated at the southern base of the Ochil Hills, which provide a spectacular backdrop. The River Devon lies to the south. The river also runs through neighbouring villages Dollar and Alva to the east and west respectively. The former mining village of Coalsnaughton lies just south, whilst Alloa lies 4 miles (6 kilometres) southwest. The "hill" referred to in the first etymology is likely to be Kirkhill, at the east of the town. The alternative Latin etymology, Tellus culta, the cultivated land, suggested by Rev. William Osborne, minister of the parish from 1773 to 1794, is also possible. However, as both etymologies could equally be applied to a hundred places in Scotland, both are suspect, as neither define the town in a unique manner.

The Ochil Fault is the geological feature which defines the southern edge of the Ochil Hills escarpment in Scotland. North of the fault, Devonian lava flows and pyroclastic deposits slope gently down, thinning towards the north. These are in part overlain by Old Red Sandstone rocks formed later in the Devonian period. Because the deposits thin towards the north, and there are few signs of volcanic necks within the Ochil Hills themselves, it is thought that the eruptive centres were south of the fault, however these are buried deep beneath the Carboniferous rocks including coal measures which are found beneath the low-lying carse lands to the south.To put this in perspective, the prominent hill Dumyat which defines the western extremity of the Ochil Hills has a height of 418 metres (1,371 ft). The nearest colliery, Manor Powis, approximately 2 kilometres (1.2 mi) south of the fault, was approximately the same depth, in carse land that is scarcely above sea level, and was mining coal from Carboniferous strata at least many hundreds of metres above the top of the Devonian deposits. The Ochil Fault was active from the earliest part of the Carboniferous period, allowing the marine swamps in which the coal-producing vegetation flourished to be periodically overlain by layers of sand, forming sandstone, or silt, forming shale, in a number of cyclic subsidences. These occurred in the form of basins, and the pattern of movements was complex, however it is known that the greatest vertical movement was centred about 1 kilometre (0.62 mi) east of the town of Alva, and almost certainly exceeded 5 kilometres (3.1 mi) vertically. The deepest deposits of coal measures are obviously found in this region, but this has not been mined to its full extent, probably due to the great depth involved. The point of maximum downwards movement south of the fault lies just south of the Silver Glen, which happens to be the part of the Ochil Hills where the greatest extent of mineralisation has been discovered. The minerals, including ores of silver and cobalt, were probably emplaced by hydrothermal solutions percolating upwards through various minor faults and fractures, in the Tertiary period. The Ochil Fault remained active throughout geological time, and some later movements allowed intrusive eruptions of diorite or quartz-dolerite to rise at various places along its length. Modern movements of the fault are very minor but occasionally give rise to discernible earthquakes, particularly in the village of Menstrie, and the town of Tillicoultry. However the latter may be easily confused with the collapse of old room and pillar coal mine workings which undoubtedly underlie the southern part of the town. The Ochil Fault is one of Britain's finest examples of a fault line scarp, and can be best appreciated from vantage points such as the Wallace Monument near Stirling.

Coalsnaughton or Calibar (Scottish Gaelic: Caolas Neachdainn) is a village in Clackmannanshire, Scotland. It is just south of Tillicoultry of which it also lies in its parish. The miners' row was built by Robert Bald.

Clackmannanshire ( ; Scots: Clackmannanshire; Scottish Gaelic: Siorrachd Chlach Mhanann), 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. The name consists of elements from three languages. The first element is from Scottish Gaelic: Clach meaning "Stone". Mannan is a derivative of the Brythonic name of the Manaw, the Iron Age tribe who inhabited the area. The final element is the English word shire. As Britain's smallest historic county, it is often nicknamed "The Wee County". When written, Clackmannanshire is commonly abbreviated to Clacks.

Gartmorn Dam is an artificial freshwater loch north-east of Alloa, Clackmannanshire, Scotland, UK, built in 1711-12 as a reservoir to supply water to hydraulic machines used in Alloa's mining industry. It was commissioned by John Erskine, 23rd and 6th Earl of Mar, to designs by George Sorocold, and is one of the earliest constructed reservoirs in Scotland.

Glenfoot railway station was a temporary terminus that served the town of Tillicoultry, Clackmannanshire, Scotland in 1851 on the Devon Valley Railway.

Dollar (Scottish Gaelic: Dolair) is a small town with a population of 2,800 people in Clackmannanshire, Scotland. It is 12 miles (19 kilometres) east of Stirling.

The Battle of Dollar was fought in 875 at Dollar, Scotland, between Viking invaders under Halfdan Ragnarsson and the defenders led by King Constantine I. The Vikings had previously been part of the Great Heathen Army which had been assaulting the Anglo-Saxon kingdoms of England before moving to a base by the river Tyne to raid the lands of the Picts and Strathclyde Britons. The battle ended in victory for the Vikings who occupied the east-central lowlands of Scotland for a year before settling in Northumbria. Constantine was forced back to the highlands of Atholl and would later die in a further battle with the Vikings in 876. The Picts disappear from the record after the devastation of 875–878.

Castle Campbell is a medieval castle situated above the town of Dollar, Clackmannanshire, in central Scotland. It was the lowland seat of the earls and dukes of Argyll, chiefs of Clan Campbell, from the 15th to the 19th century, and was visited by Mary, Queen of Scots, in the 16th century. Mary was impressed by this and said "this reminds me of home".

Dollar railway station served the village of Dollar, Clackmannanshire, Scotland from 1869 to 1964 on the Devon Valley Railway.

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+1⁄4 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.