The Cairngorms are a mountain range in the eastern Highlands of Scotland closely associated with the mountain Cairn Gorm. The Cairngorms became part of Scotland's second national park on 1 September 2003. Although the Cairngorms give their name to, and are at the heart of, the Cairngorms National Park, they only form one part of the national park, alongside other hill ranges such as the Angus Glens and the Monadhliath, and lower areas like Strathspey.
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 Palace of Holyroodhouse and was formerly a 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.
Cairn Gorm is a mountain in the Scottish Highlands. It is part of the Cairngorms range and wider Grampian Mountains. With a summit elevation of 1,244.8 m (4,084 ft) above sea level, Cairn Gorm is classed as a Munro and is the sixth-highest mountain in the British Isles. The high, broad domed summit overlooking Strathspey is one of the most readily identifiable mountains from the nearby town and regional centre of Aviemore. Although it shares its name with the Cairngorm mountains, Ben Macdui is the highest mountain in the range.
Braeriach or Brae Riach is the third-highest mountain in Scotland and all of the British Isles, after Ben Nevis and Ben Macdui, rising 1,296 metres (4,252 ft) above sea level. It is in the Scottish Highlands and is the highest point in the western massif of the Cairngorms, separated from the central section by the Lairig Ghru pass. The summit is a crescent-shaped plateau, overlooking several corries.
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.
The Southern Upland Way is a 344-kilometre (214 mi) coast-to-coast long-distance footpath in southern Scotland. The route links Portpatrick in the west and Cockburnspath in the east via the hills of the Southern Uplands. The Way is designated as one of Scotland's Great Trails by NatureScot and is the longest of the 29 Great Trails. The Southern Upland Way meets with seven of the other Great Trails: the Annandale Way, the Berwickshire Coastal Path, the Borders Abbeys Way, the Cross Borders Drove Road, the Mull of Galloway Trail, the Romans and Reivers Route and St Cuthbert's Way.
Scotland is the 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 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.
The Callanish IV stone circle is one of many megalithic structures around the better-known Calanais I on the west coast of the Isle of Lewis, in the Outer Hebrides, Scotland. It is a scheduled monument and its official name is Sron a'Chail. The site was first surveyed and recorded by RCAHMS in 1914 and again in 2009, with another survey in the 1970s by other archaeologists, but no known archaeological excavations have taken place at the stones.
Derry Cairngorm is a Scottish mountain in the Cairngorms range, 14 kilometres (8.7 mi) north west of Braemar in the county of Aberdeenshire.
West Linga is an uninhabited island located between Mainland and Whalsay in Shetland, Scotland.
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.
Broad Cairn is a mountain in the Grampians of Scotland, located about 16 mi (26 km) south of the River Dee near Balmoral.
Tomnaverie stone circle is a recumbent stone circle set on the top of a small hill in lowland northeast Scotland. Construction started from about 2500 BC, in the Bronze Age, to produce a monument of thirteen granite stones including a massive 6.5-ton recumbent stone lying on its side along the southwest of the circle's perimeter. Within the 17-metre (56 ft) circle are kerb stones encircling a low 15-metre (49 ft) ring cairn but the cairn itself no longer exists.
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.
