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Strone (Inverness)

Hamlets in ScotlandHighland geography stubsPopulated places in Highland (council area)

Strone (Scottish Gaelic: An t-Sròn, translating to "The Nose") is a small hamlet in the administrative county of the Scottish Highland and in the historic county of Inverness-shire. It lies on the foot of the hill, Creag na h-Iolaire in Glen Urquhart in the Great Glen. The nearest town is Drumnadrochit and Urquhart Castle lies nearby.The hamlet is often confused with the village of Strone in Argyll and Bute.

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

Strone (Inverness)
A82,

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N 57.325 ° E -4.4489 °
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A82
IV63 6XL
Scotland, United Kingdom
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Urquhart Castle
Urquhart Castle

Urquhart Castle ( ; Scottish Gaelic: Caisteal na Sròine) is a ruined castle that sits beside Loch Ness in the Highlands of Scotland. The castle is on the A82 road, 21 kilometres (13 mi) south-west of Inverness and 2 kilometres (1.2 mi) east of the village of Drumnadrochit. The present ruins date from the 13th to the 16th centuries, though built on the site of an early medieval fortification. Founded in the 13th century, Urquhart played a role in the Wars of Scottish Independence in the 14th century. It was subsequently held as a royal castle and was raided on several occasions by the MacDonald Earls of Ross. The castle was granted to the Clan Grant in 1509, though conflict with the MacDonalds continued. Despite a series of further raids the castle was strengthened, only to be largely abandoned by the middle of the 17th century. Urquhart was partially destroyed in 1692 to prevent its use by Jacobite forces, and subsequently decayed. In the 20th century, it was placed in state care as a scheduled monument and opened to the public: it is now one of the most-visited castles in Scotland and received 547,518 visitors in 2019.The castle, situated on a headland overlooking Loch Ness, is one of the largest in Scotland in area. It was approached from the west and defended by a ditch and drawbridge. The buildings of the castle were laid out around two main enclosures on the shore. The northern enclosure or Nether Bailey includes most of the more intact structures, including the gatehouse, and the five-story Grant Tower at the north end of the castle. The southern enclosure or Upper Bailey, sited on higher ground, comprises the scant remains of earlier buildings.

Loch Ness
Loch Ness

Loch Ness (; Scottish Gaelic: Loch Nis [l̪ˠɔx ˈniʃ]) is a large freshwater loch in the Scottish Highlands extending for approximately 37 kilometres (23 miles) southwest of Inverness. It takes its name from the River Ness, which flows from the northern end. Loch Ness is best known for claimed sightings of the cryptozoological Loch Ness Monster, also known affectionately as "Nessie" (Scottish Gaelic: Niseag). It is one of a series of interconnected, murky bodies of water in Scotland; its water visibility is exceptionally low due to the high peat content of the surrounding soil. The southern end connects to Loch Oich by the River Oich and a section of the Caledonian Canal. The northern end connects to Loch Dochfour via the River Ness, which then ultimately leads to the North Sea via the Moray Firth. At 56 km2 (22 sq mi), Loch Ness is the second-largest Scottish loch by surface area after Loch Lomond, but due to its great depth it is the largest by volume in Great Britain. Its deepest point is 230 metres (126 fathoms; 755 feet), making it the second deepest loch in Scotland after Loch Morar. It contains more water than all the lakes in England and Wales combined, and is the largest body of water in the Great Glen, which runs from Inverness in the north to Fort William in the south. Its surface is 16 metres (52 feet) above sea level. It contains a single, artificial island named Cherry Island (Scottish Gaelic: Eilean Muireach) at the southwestern end. There are nine villages around the loch, as well as Urquhart Castle; the village of Drumnadrochit contains a "Loch Ness Centre and Exhibition".

Great Glen
Great Glen

The Great Glen (Scottish Gaelic: An Gleann Mòr [an ˈklaun̪ˠ ˈmoːɾ]), also known as Glen Albyn (from the Gaelic Gleann Albainn "Glen of Scotland" [ˈklaun̪ˠ ˈaɫ̪apən]) or Glen More (from the Gaelic Gleann Mòr), is a glen in Scotland running for 62 miles (100 km) from Inverness on the edge of the Moray Firth, in an approximately straight line to Fort William at the head of Loch Linnhe. It follows a geological fault known as the Great Glen Fault, and bisects the Scottish Highlands into the Grampian Mountains to the southeast and the Northwest Highlands to the northwest. The glen is a natural travelling route in the Highlands of Scotland, which is used by both the Caledonian Canal and the A82 road, which link the city of Inverness on the northeast coast with Fort William on the west coast. The Invergarry and Fort Augustus Railway was built in 1896 from the southern end of the glen to the southern end of Loch Ness, but was never extended to Inverness. The railway closed in 1947. In 2002, the Great Glen Way was opened. A long-distance route for cyclists, canoeists, and walkers, it consists of a series of footpaths, forestry tracks, canal paths and occasional stretches of road linking Fort William to Inverness.The glen's strategic importance in controlling the Highland Scottish clans, particularly around the time of the Jacobite risings of the 18th century, is recognised by the presence of the towns of Fort William in the south, Fort Augustus in the middle of the glen, and Fort George, just to the northeast of Inverness. Much of the glen is taken up with a series of lochs, with rivers connecting them. The Caledonian Canal also uses the lochs as part of the route, but the rivers are not navigable. From northeast to southwest, the natural water features along the Great Glen are: River Ness (Abhainn Nis) Loch Dochfour (Loch Dabhach Phuir) Loch Ness (Loch Nis) River Oich (Abhainn Omhaich) Loch Oich (Loch Omhaich) Loch Lochy (Loch Lochaidh) River Lochy (Abhainn Lochaidh) Loch Linnhe (An Linne Dhubh)The watershed lies between Loch Oich and Loch Lochy. Loch Linnhe to the south of Fort William is a sea loch into which both the River Lochy and Caledonian Canal emerge. At the north end, the River Ness empties into the Beauly Firth at the point where it meets the Moray Firth.