There are also three other hills over 600m with a drop of 15-20 metres: Hills over 600m. The extent of the Ochils is not well-defined but by some definitions continues to include the hills of north Fife.[3]. Since 1846 small shocks have been observed at Comrie on a regular, if infrequent, basis. Oblique aerial photograph of the line of the Ochil Fault, Ochil Hills, Stirlingshire. Immediately to the north is the campus of Stirling University and Airthrey Loch. The Ochil Fault is the geological feature which defines the southern edge of the Ochil Hills escarpment in Scotland. [10] The windfarm is owned and run by EDF Renewables, who support the work of the Ochils Mountain Rescue Team through the Burnfoot Hill Community Fund with an annual donation of £5,000 guaranteed till 2039. The geology of the Stirling district. Includes geology, climate, natural history, human history, placenames and walks in Alva Glen, Menstrie Glen, and Dollar to Glens Quey/Devon. Abstract The Ochil Hills, running northeastwards from the Forth at Stirling, to Tentsmuir on the North Sea coast, are the most Impressive and most extensive of the several uplands which diversify the Central Lowlands of Scotland (Fig. The plateau is undulating with no prominent peak, the highest point being Ben Cleuch at 721 m (2,365 ft). both from the geological setting and microchemical signature of the gold. 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 km east of the town of Alva, and almost certainly exceeded 5 km vertically. The Ochil Fault is the geological feature which defines the southern edge of the Ochil Hills escarpment in Scotland. Path of Condie and the Ochil Hills The andesitic lavas continue in a broad arc around Perth, and agate bearing localities are found to the south-west around the Path of Condie and along the southern face of the Ochil Hills. [6] Parts of the lower slopes on the northern side around Blackford and Auchterarder are formed from a volcanic conglomerate. The purpose of the trip on the hottest weekend of the year was to look at the Lower Devonian Ochil Volcanic Formation Lavas and volcanic conglomerates, and the … Heavy Metal Mines in the Ochil Hills: Chronology and Context By John G Harrison INTRODUCTION In recent decades the mines of the Ochil Hills, in east central Scotland, have attracted the interest of speleologists, mineralogists, ceramists, and botanists1. Glenfarg, Ochil Hills, Perth and Kinross, Scotland, UK : SUPPORT US. "[9], An 18-turbine development, approved in June 2006, has been constructed at Green Knowes, south of Auchterarder, north of Glendevon about 400 m (1,300 ft) north of the Ben Thrush summit. The highest point is Ben Cleuchin Clackmannanshireat 2,365 feet. Intrusions of both mafic and felsic character are also found. Blairdenon Hill was the site of one of the Beacons of Dissent during the G8 protests in July 2005. The hills are part of a Devonian lava extrusion whose appearance today is largely due to the Ochil Fault which results in the southern face of the hills forming an escarpment. Castle Craig, a ruined ancient fort above the village of Mill Glen destroyed by industrial quarrying, was mentioned by local historian William Gibson in 1883 as being "a round Pictish fortress, the traces of which can still be distinctly seen. They also acted as a boundary with Fife. The Ochil Fault, one of the most prominent tectonic features in the Midland Valley of Scotland, juxtaposes Lower Devonian volcanic rocks against late Westphalian strata, implying a possible vertical displacement of … [5], Coordinates: .mw-parser-output .geo-default,.mw-parser-output .geo-dms,.mw-parser-output .geo-dec{display:inline}.mw-parser-output .geo-nondefault,.mw-parser-output .geo-multi-punct{display:none}.mw-parser-output .longitude,.mw-parser-output .latitude{white-space:nowrap}56°09′36″N 3°44′46″W / 56.160°N 3.746°W / 56.160; -3.746, Learn how and when to remove this template message, "The Ochil Fault and the Kincardine basin: key structures in the tectonic evolution of the Midland Valley of Scotland", "Geology of Scotland | NCAP - National Collection of Aerial Photography", "Geocaching - The Official Global GPS Cache Hunt Site", https://en.wikipedia.org/w/index.php?title=Ochil_Fault&oldid=996880058, Short description is different from Wikidata, Articles needing additional references from October 2011, All articles needing additional references, Creative Commons Attribution-ShareAlike License, This page was last edited on 29 December 2020, at 01:25. The hills are part of a Devonian lava extrusion whose appearance today is largely due to the Ochil Fault which results in the southern face of the hills forming an escarpment. Sheriffmuir, the site of the 1715 battle of the Jacobite rising, is on the northern slopes of the hills. A band of this formation runs from Gargunnock to the Clyde ; and 1 believe there are quarries in it near Gargunnock, but have not seen them myself. Alluvial gold is wide-spread and locally abundant in the central Ochil Hills, but the bedrock sources have not been identified. A notional boundary for the Ochil Hills is shown in Map 2, bounded by roads, and stretching from Dunblane in the west to Glen Farg in the east. Illustrated with many diagrams and drawings and some photographs. Stay safe in the Ochils and always take a map and compass. Ochil Volcanic Formation and the Quaternary of Glen Devon August 9th 2003. To the west and NW, there are commanding views of the Carse west of Stirling, the Menteith Hills (Lower Devonian conglomerates) and the Grampian mountains. The Ochil Hills . The hills are part of a Devonian lava extrusion whose appearance today is largely due to the Ochil Faultwhich … The Path of Condie is a very old established collecting site. "[8]Old lore also told that some of the stones from the fort of Castle Craig were used in the construction of Stirling Castle, 7 3⁄4 miles (12.5 kilometres) to the west. 1. Following approval in early 2007, the construction of a wind farm consisting of thirteen 102 m (335 ft) turbines on Burnfoot Hill, which lies north of Tillicoultry and Ben Cleuch and to the south of the Upper Glendevon Reservoir has been completed. Always take a map and compass Devonian period is exactly what you can see up. Stirling, the Campsie Fells outside Glasgow, and the Quaternary of Glen Devon 9th! 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