Stranraer, also known as The Toon, is a town in Dumfries and Galloway, Scotland, on Loch Ryan and the northern side of the isthmus joining the Rhins of Galloway to the mainland. Stranraer is Dumfries and Galloway's second-largest town, with a population of 10,593.
Kirkcudbrightshire, or the County of Kirkcudbright or the Stewartry of Kirkcudbright is one of the historic counties of Scotland, covering an area in the south-west of the country. Until 1975, Kirkcudbrightshire was an administrative county used for local government. Since 1975, the area has formed part of Dumfries and Galloway for local government purposes. Kirkcudbrightshire continues to be used as a registration county for land registration. A lower-tier district called Stewartry covered the majority of the historic county from 1975 to 1996. The area of Stewartry district is still used as a lieutenancy area. Dumfries and Galloway Council also has a Stewartry area committee.
Galloway is a region in southwestern Scotland comprising the historic counties of Wigtownshire and Kirkcudbrightshire. It is administered as part of the council area of Dumfries and Galloway.
Wigtownshire or the County of Wigtown is one of the historic counties of Scotland, covering an area in the south-west of the country. Until 1975, Wigtownshire was an administrative county used for local government. Since 1975 the area has formed part of Dumfries and Galloway for local government purposes. Wigtownshire continues to be used as a territory for land registration, being a registration county. The historic county is all within the slightly larger Wigtown Area, which is one of the lieutenancy areas of Scotland and was used in local government as the Wigtown District from 1975 to 1996.
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 Machars is a peninsula in the historical county of Wigtownshire in Galloway in the south-west of Scotland. Its name is derived from the Gaelic word Machair meaning low-lying or level land, known as "links" on the east coast of Scotland. Although there are no high peaks in The Machars, it is not flat and would best be described as undulating or rolling. The North Atlantic Drift or Gulf Stream creates a mild climate, and dolphins and basking sharks are frequently seen in the seas.
New Luce is a civil parish in Dumfries and Galloway, south-west Scotland. It lies in the traditional county of Wigtownshire, and is about 10 miles (16 km) in length and 5 miles (8.0 km) in breath, being the upper part of the original Glenluce Parish. New Luce is shown as a civil parish on John Ainslie's county map of 1782.
Clan MacDowall or MacDouall is a Lowlands Scottish clan.
Glasserton is a civil parish in Dumfries and Galloway, south-west Scotland. It is on the Machars peninsula, in the traditional county of Wigtownshire. The parish is about 8 miles (13 km) in length, varying in breadth from 1 to 3 miles, and contains 13,477 acres (54.54 km2).
Stoneykirk is an area and a village in the heart of the Rhins of Galloway, Wigtownshire, in the administrative council area of Dumfries and Galloway, Scotland nearly 10 miles (16 km) in length and 3+1⁄2 miles (5.6 km) in breadth, bounded on the east by the bay of Luce, and on the west by the Irish Channel, 5 miles (8 km) south of Stranraer.
Cargenbridge is a village located in Dumfries and Galloway, United Kingdom, southwest of Dumfries. It is in Troqueer parish, in the historic county of Kirkcudbrightshire.
Leswalt is a village and civil parish in Dumfries and Galloway, south-west Scotland. It lies between Portpatrick and Stranraer in the Rhins of Galloway, part of the traditional county of Wigtownshire. The parish covers around 8 square miles (21 km2).
Kirkcolm is a village and civil parish on the northern tip of the Rhinns of Galloway peninsula, south-west Scotland. It is in Dumfries and Galloway, and is part of the former county of Wigtownshire. The parish is bounded on the north and west by the sea, on the east by the bay of Loch Ryan and on the south by Leswalt parish.
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.
Old Luce is a civil parish in Dumfries and Galloway, Scotland. It lies in the Machars peninsula, in the traditional county of Wigtownshire. The parish is around 10 miles (16 km) long and 8 miles (13 km) broad, and contains 40,350 acres (16,330 ha).
The Wren's Egg is the name given to a set of late Neolithic or Bronze Age stone monuments in the parish of Glasserton, Wigtownshire, Dumfries and Galloway. The site comprises two pairs of standing stones to the north and south of a large glacial erratic, the Wren's Egg itself. It was one of the first monuments taken into state care after the Ancient Monuments Act passed in 1882.
Droughdool Mote is a Neolithic round mound in the parish of Old Luce, Wigtownshire, Dumfries and Galloway. The mound is oval in plan, measuring 60m by 50m at its base and rises to 10m in height. It is located 400m south of the late neolithic palisaded enclosure at Dunragit. It has been suggested that the mound may have been used as a viewing platform for activities at Dunragit complex of monuments. The most well known parallel the site has is Silbury Hill in Wiltshire, but is closer in size to the less well known sites at Conquer Barrow, Willy Howe and Wold Newton. The mound was originally built with stepped sides on top of a sand dune. Excavation between 1999-2002 revealed a round cairn at the top of the mound, similar to the nearby Mid Gleniron A.
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.
Mid Gleniron is a prehistoric site in Dumfries and Galloway used in the Neolithic and Bronze Age. The site is a scheduled ancient monument that comprises a group of six burial cairns. Two of the cairns, Mid Gleniron I and Mid Gleniron II are chambered cairns of the Clyde tradition. These are of historic importance because of their multi-stage construction which provides evidence for the development of Clyde cairns at the beginning of the Neolithic period.
The High Banks cup and ring markings are a series of Neolithic or Bronze Age carvings on an outcrop of rock near High Banks farm, 3 km SE of Kirkcudbright, Dumfries and Galloway. They are one of the best collections of cup and ring markings in Galloway.
