A cairn is a man-made pile of stones raised for a purpose, usually as a marker or as a burial mound. The word cairn comes from the Scottish Gaelic: càrn[ˈkʰaːrˠn̪ˠ].
Berwickshire is a historic county, registration county and lieutenancy area in southeastern Scotland, on the English border. It takes its name from Berwick-upon-Tweed, which was part of the Kingdom of Northumbria at the time of the county's formation, but became part of England in 1482 after several centuries of swapping back and forth between the two kingdoms
Biggar is a town and former burgh in South Lanarkshire, Scotland, in the Southern Uplands near the River Clyde on the A702. The closest towns are Lanark and Peebles.
The Grampian Mountains are one of the three major mountain ranges in Scotland, occupying a considerable portion of the Scottish Highlands in northern Scotland. The other major mountain ranges in Scotland are the Northwest Highlands and the Southern Uplands. The Grampian range extends southwest to northeast between the Highland Boundary Fault and the Great Glen, occupying almost half of the land area of Scotland and including the Cairngorms and the Lochaber hills. The range includes many of the highest mountains in the British Isles, including Ben Nevis and Ben Macdui.
Holyrood Park is a royal park in central Edinburgh, Scotland about 1 mile to the east of Edinburgh Castle. It is open to the public. It has an array of hills, lochs, glens, ridges, basalt cliffs, and patches of gorse, providing a wild piece of highland landscape within its 650-acre (260 ha) area. The park is associated with the royal palace of Holyroodhouse and was formerly a 12th-century royal hunting estate. The park was created in 1541 when James V had the ground "circulit about Arthurs Sett, Salisborie and Duddingston craggis" enclosed by a stone wall.
Beinn Eighe is a complex mountain massif in the Torridon area of Wester Ross in the Highlands of Scotland. Lying to the south of Loch Maree, it forms a long ridge with many spurs and summits, two of which are classified as Munros. The name Beinn Eighe comes from the Scottish Gaelic meaning file mountain. Unlike most other hills in the area it has a cap of Cambrian basal quartzite which gives the peaks of Beinn Eighe a distinctive light colour. Its complex topography has made it popular with both hillwalkers and climbers and the national nature reserve on its northern side makes it an accessible mountain for all visitors.
Ben Lawers is the highest mountain in the southern part of the Scottish Highlands. It lies to the north of Loch Tay, and is the highest point of a long ridge that includes seven Munros. It is the highest peak in Perthshire, and is the tenth highest Munro in Scotland. Ben Lawers was long thought to be over 4,000 feet (1,219.2 m) in height; accurate measurement in the 1870s showed it to be some 17 feet (5.2 m) short of this figure.
Braeriach is the third-highest mountain in the British Isles, surpassed only by Ben Nevis and Ben Macdui. It is the highest point in the western massif of the Cairngorms, separated from the central section by the pass of the Lairig Ghru. The summit has a crescent shape, with several corries. The lingering snows of Braeriach are amongst the most persistent snow patches in Scotland and - by extension - the entire British Isles. The north-facing corrie of Garbh Coire Mor has been snow-free just seven times in the last one hundred years: 1933, 1959, 1996, 2003, 2006, 2017 and 2021, although the rate and occurrence of melting appears to be increasing.
Kilmartin Glen is an area in Argyll north of Knapdale. It has the most important concentration of Neolithic and Bronze Age remains in mainland Scotland. The glen is located between Oban and Lochgilphead, surrounding the village of Kilmartin. In the village, Kilmartin Museum explains the stories of this ancient landscape and the people who dwelt there. There are more than 800 ancient monuments within a six-mile (ten-kilometre) radius of the village, with 150 monuments being prehistoric. Monuments include standing stones, a henge monument, numerous cists, and a "linear cemetery" comprising five burial cairns. Several of these, as well as many natural rocks, are decorated with cup and ring marks.
Scotland is the most mountainous country in the United Kingdom. Scotland's mountain ranges can be divided in a roughly north to south direction into: the Scottish Highlands, the Central Belt and the Southern Uplands, the latter two primarily belonging to the Scottish Lowlands. The highlands eponymously contains the country's main mountain ranges, but many hills and mountains are to be found south of these as well. The below lists are not exhaustive; there are countless subranges throughout the country.
Derry Cairngorm is a Scottish mountain in the Cairngorms range, 14 kilometres (8.7 mi) north west of Braemar in the county of Aberdeenshire.
A moot hill or mons placiti is a hill or mound historically used as an assembly or meeting place, as a moot hall is a meeting or assembly building, also traditionally to decide local issues. In early medieval Britain, such hills were used for "moots", meetings of local people to settle local business. Among other things, proclamations might be read; decisions might be taken; court cases might be settled at a moot. Although some moot hills were naturally occurring features or had been created long before as burial mounds, others were purpose-built.
Carlin Stone or Carline Stane is the name given to a number of prehistoric standing stones and natural stone or landscape features in Scotland. The significance of the name is unclear, other than its association with old hags, witches, and the legends of the Cailleach.
Symington is a small village in South Lanarkshire, Scotland, 3 miles (5 km) southwest of Biggar, 10 miles (16 km) east of Douglas and 13 miles (21 km) southeast of Carluke. Geographical features near Symington include Tinto Hill, the Coulter Hills and the River Clyde. A map by Pont in 1596 showed two St John's Kirks in a small settlement, and another map by Roy in 1754 showed a mill to the east.
The Kilpatrick Hills are a range of hills in central Scotland, stretching from Dumbarton in the west to Strathblane in the east. Strathblane divides the Kilpatricks from the Campsie Fells to the east, while to the north is part of the Loch Lomond and the Trossachs National Park. To west and south the hills are fringed by the settlements of Balloch, Dumbarton, Milton, Bowling, Old Kilpatrick, Clydebank, Bearsden and Milngavie. The majority of the range is within West Dunbartonshire, although it extends into the East Dunbartonshire and Stirling areas.
Lewis and Harris, or Lewis with Harris, is a single Scottish island in the Outer Hebrides, divided by mountains. It is the largest island in Scotland and the third largest in the British Isles, after Great Britain and the island of Ireland, with an area of 841 square miles (2,178 km2), which is approximately 1% of the area of Great Britain. The northern two-thirds is called [the Isle of] Lewis and the southern third [the Isle of] Harris; each is frequently referred to as if it were a separate island.
Inch is a civil parish in Dumfries and Galloway, southwest Scotland. It lies on the shore of Loch Ryan, in the traditional county of Wigtownshire.
The Rhinns of Kells are a range of hills in the Galloway Hills range, part of the Southern Uplands of Scotland. The most easterly of three parallel ridges, they are neighboured to the west by the Range of the Awful Hand and the Dungeon Hills. The eastern portion of the Minnigaff Hills range lies immediately southwest of the range. In total, these four ranges are part of the Galloway Forest Park. The ridge is located entirely within Dumfries and Galloway, with the base of the western flanks being a northwestern boundary of the county.
Loanhead of Daviot stone circle is a recumbent stone circle in Aberdeenshire in lowland northeast Scotland. The circle consists of the recumbent stone with its flankers and a complete set of eight orthostats about 21 metres (69 ft) in diameter surrounding a low kerbed ring cairn which has an open court. However, the present appearance has in part been produced by substantial restoration after archaeological excavation in 1934, and in 1989 by the removal of the stones covering the central court.
