place

Raploch

Geography of Stirling (council area)Housing estates in ScotlandStirling (city)

Raploch, known locally as The Raploch or The Raptap, is a district of the city of Stirling, which lies to the south of the River Forth in central Scotland. The first houses were built in the late 17th century, after the land had been sold by the Earl of Mar to the patrons of Cowane's Hospital in Stirling. Economic conditions led to stagnation but housing began again in earnest at the start of the 19th century. The real expansion came in the middle of the 20th century, when council housing replaced decrepit housing in the old town. Perhaps one of the most notable people to have come from the district is football legend Billy Bremner, who also attended the local St. Mary's Roman Catholic primary school. A more recent football star from Raploch is David Goodwillie.The Raploch was the subject of a 2002 BBC Scotland documentary entitled Raploch Stories, and in a 2017 sequel Raploch Stories Revisited. Since 2004, the Raploch area has undergone a great deal of physical regeneration.In 2008 the area became the home of the UK's first El Sistema children's orchestra, called Big Noise Raploch. A children's orchestra with over 100 members, who performed with Gustavo Dudamel and the Simón Bolívar Symphony Orchestra of Venezuela on 21 June 2012 and on a BBC Scotland Christmas Eve (2012) Special in Stirling's Holy Rude Church.

Excerpt from the Wikipedia article Raploch (License: CC BY-SA 3.0, Authors).

Raploch
Drip Road, Stirling Raploch

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: RaplochContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 56.1297 ° E -3.9471 °
placeShow on map

Address

Drip Road

Drip Road
FK8 1RD Stirling, Raploch
Scotland, United Kingdom
mapOpen on Google Maps

Share experience

Nearby Places

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 penetrates the coal measures, often in bedding planes between the various strata. In places, it rises through fractures in the strata to a new level, forming features that, at the surface, would be called dikes. At its outcrop on the west, the sill generally lies towards the base of the Carboniferous sequence, and just above the calciferous sandstone deposits and lavas, as can be seen in the upper part of the valley of the Bannock Burn. However, to the consternation of miners, it occupies a higher position amongst the useful strata towards the east, and in places has destroyed the coal, while in others the effect of the sill has been to convert the coal to more valuable anthracite. The slope of the Abbey Craig, or the Stirling Castle rock, gives a general idea of the angle of dip of the coal measures at the extremity or the coalfield, and the thickness of the sill can also be seen, which is approximately 100 metres.Geologists have had various theories about the formation of anthracite, as the coal has been most effectively baked near the Ochil Fault, however the theories are not necessarily incompatible.The source of the sill, where the molten rock rose from below, is not known; however it is known that there are risers in the Ochil Fault, although these are inconsistent with the overall structure. The main origin of the sill may be in the region of the eruptive centre that formed the Ochil Hills in a much earlier period, which geologists postulate is somewhere to the east of Stirling, possibly in the region of Kincardine. This ties in with subsidence following the first round of eruptive activity that lead to the formation of the coal basins, with a much later outbreak of intrusive activity from the same magma feeders, however the truth will remain unknown because it would take very many deep bores in hard rock to probe the depths and find the necessary evidence.The western extremities of the sill can be seen at the Abbey Craig, Stirling Castle, Kings Park, Gillies Hill, Sauchieburn and various points to the south. The quartz-dolerite was once quarried at several places including Cambusbarron and Murrayshall, but is quarried today at Northfield, primarily for roadstone.