Tillicoultry

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.

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.

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

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.

Harviestoun is an estate in Tillicoultry parish, Clackmannanshire, central Scotland. It lies at the base of the Ochil Hills, around 1.5 kilometres (0.93 mi) east of Tillicoultry and 2 kilometres (1.2 mi) west of Dollar.

Fishcross is a small village in Clackmannanshire in central Scotland, situated to the north of Sauchie at a crossroads just south of Tillicoultry. Formerly a mining village, the population is 484 as at 2003.A golf course and equestrian centre are located nearby and at Auchinbaird there is a fine example of a windmill built in the early 18th Century to drain a coal pit and later converted to serve as a dovecote.

Auchinbaird Windmill or New Sauchie Windmill, was originally a late 17th or early 18th century vaulted tower grain windmill built into a low ridge located on the outskirts of the town of Sauchie, Clackmannanshire, Scotland. It was later converted into the Auchinbaird Dovecote or New Sauchie Dovecote, abandoned at an unknown date and later conserved as a landscape feature and visitor attraction.

Sauchie Tower, also known as Devon Tower, is a 15th-century tower house in Clackmannanshire, Scotland. The tower is located by the village of Fishcross, 1 kilometre (0.62 mi) north of Sauchie and 2.5 kilometres (1.6 mi) north of Alloa, close to the River Devon. It is protected as a Scheduled Ancient Monument.

Sauchie railway station served the town of Sauchie, Clackmannanshire, Scotland from 1873 to 1930 on the Devon Valley Railway.

Sauchie Juniors Football Club are a Scottish football club based in the village of Sauchie, Clackmannanshire. Their home ground is Beechwood Park and club colours are red and white. The team plays in the East of Scotland League Premier Division, having moved from the junior leagues in 2018.