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Mote Hill

Hills of the Scottish Midland ValleyMountains and hills of Stirling (council area)Source attribution
Cannons on Mote Hill (geograph 5950838)
Cannons on Mote Hill (geograph 5950838)

Mote Hill is the northern tip of the Gowanhills, Stirling, the northern half of the Royal Park that extends around Stirling Castle. The wider park includes the King's Knott and sections of a 2-metre-high deer wall, first established in the 12th century, though Gowan Hill only became park of the Royal Park around 1500. Ten thousand years ago, Mote Hill was a promontory projecting into a lost prehistoric sea. On the opposite bank of the River Forth lies Abbey Craig, upon which sits the National Wallace Monument. These two rocky outcrops were, for thousands of years, the lowest crossing point of the Forth. Mote Hill is also known as Heiding Hill or Murdoch's Knowe or Hurlie Haw and is the location of the Beheading Stone, the traditional execution block of medieval Stirling. The stone itself is now on a concrete mount and under an iron cage, but you can still see the axe marks from the executions. Mote Hill is also the site of a vitrified fort, destroyed by fire in the first half of the first millennium AD. This date was confirmed by excavation by Murray Cook, Stirling Council's archaeologist.

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

Mote Hill
Back Walk, Stirling Raploch

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Latitude Longitude
N 56.1277 ° E -3.9428 °
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Back Walk

Back Walk
FK8 1SH Stirling, Raploch
Scotland, United Kingdom
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Cannons on Mote Hill (geograph 5950838)
Cannons on Mote Hill (geograph 5950838)
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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.