Bodesbeck Law

The Southern Uplands (Scottish Gaelic: Na Monaidhean a Deas) are the southernmost and least populous of mainland Scotland's three major geographic areas (the others being the Central Lowlands and the Highlands). The term is used both to describe the geographical region and to collectively denote the various ranges of hills and mountains within this region. An overwhelmingly rural and agricultural region, the Southern Uplands are partly forested and contain many areas of open moorland - the hill names in the area are congruent with these characteristics.

White Coomb is a hill in the Moffat Hills range, part of the Southern Uplands of Scotland. Its broad summit is the highest point in the range and the registration county of Dumfriesshire, as well as being the fourth highest point in southern Scotland, however, despite this, it is largely concealed by other hills on all sides except its east and south east, making this the only direction from which its full scale can be seen. White Coomb is most easily climbed from the National Trust for Scotland car park underneath the Grey Mare's Tail waterfall, on the A708 from Moffat to Selkirk, at NT 186146. The most direct route heads directly west up a steep ridge, but a more comfortable route follows a well built footpath above the north side of the waterfall. Above the waterfall, the fast flowing Tail Burn must be crossed to avoid a long detour; although there are plenty of natural stepping stones, spate or icy conditions may make their use dangerous. From across the stream, the best route through the peat and heather follows the course of a wall leading to the summit of Upper Tarnberry. From there, the east ridge, which is steep and craggy in places, leads to the broad summit. An alternative ascent, described by the Daily Telegraph as one of "Britain's finest half-day and day walks", follows the Tail Burn to the outlet of Loch Skeen before ascending the ridge to Mid Craig, and passing Donald's Cleuch Head to reach the summit. The descent suggested is via Rough Craig and south to join the road and walk back to the start point.

Grey Mare's Tail is a 60-metre (200 ft) hanging valley waterfall near to Moffat in southern Scotland. The fall is produced by the Tail Burn flowing from Loch Skeen cascading into the Moffat Water in the lower valley below. The surrounding area forms the Grey Mare's Tail Nature Reserve, owned by the National Trust for Scotland. The footpath from the valley floor up to Loch Skeen is one of the more popular walks in the area. Parking is also provided. Grey Mare's Tail Nature Reserve is situated along the Moffat Water Valley in the heart of the Southern Uplands. This National Trust for Scotland property extends over 922 hectares and is characterised by a dramatic waterfall (the 5th highest in the UK), an upland loch Loch Skeen and White Coomb which rises to 821m and is one of the highest hills in Southern Scotland. The post-glacial landscape is an open mosaic of heather and rough grazing that includes 8 habitats of European importance and many plant species of international, national and regional significance. The reserve is botanically diverse, containing the richest assemblage of rare upland plants in Southern Scotland. Recognised as a Special Area of Conservation, Grey Mare's Tail Nature Reserve is popular with hill walkers, botanists and wildlife enthusiasts. There is also historical evidence of Iron Age settlers and the Covenanters who sought sanctuary here in the 17th century. Notable animal species: peregrine falcon, ring ouzel, raven, vendace and wild goats. Rare plants: many, including oblong woodsia, montane willows, and alpine saw-wort.

Croft Head is a hill in the Ettrick Hills range, part of the Southern Uplands of Scotland. It offers unobstructed views to the Solway Firth, the fells and mountains of Cumbria and the Pennines to the south and east. To the north, the major Moffat Hills are close by and to the west, Queensberry, the Lowthers and many of the Galloway Hills can be seen. Its summit is easily reached from Moffat by taking the Southern Upland Way path east from the Moffat water bridge near Craigbeck. A quite dramatic ridge loop is possible by climbing north on the forestry fire road shortly after Craigbeck Hope cottage via Gateshaw Rig to Croft Head's summit and descending via Cat Shoulder to the junction of the SUW and the Selcoth burn pass.

Loch Skeen or Loch Skene is a loch in Dumfries and Galloway in the south of Scotland. It is located about 10 miles to the north-east of Moffat and feeds the 60-metre (200 ft) high Grey Mare's Tail waterfall. The area around Loch Skeen is popular with hikers, and the Daily Telegraph included Loch Skeen in a list of Britain's finest one-day and half-day walks. It is the highest loch in the Southern Uplands at approximately 510m.

Andrewhinney Hill is a hill in the Ettrick Hills range, part of the Southern Uplands of Scotland. It is the highest summit of a ridge that runs parallel to the A708 road on its southern side, with the Grey Mare's Tail in the Moffat Hills directly opposite. The northwestern slopes are designated as part of the 'Moffat Hills' SSSI and SAC.

Ettrick Pen is a hill in the Ettrick Hills range, part of the Southern Uplands of Scotland. A remote peak, It lies southwest of the village of Ettrick, on the border of the Scottish Borders and Dumfries and Galloway. The highest of the Ettrick Hills, it is crossed by the Southern Upland Way and is a prominent landmark from many directions. Its summit is topped by an ancient cairn.

Dob's Linn is a small steep valley in Dumfries and Galloway, just north of the A708 road between Moffat and Selkirk, in Scotland. It is part of the Grey Mare's Tail Nature Reserve which is owned by the National Trust for Scotland. According to tradition, Dob's Linn is named for a covenanter, Halbert Dobson, who took refuge there from Government troops during The Killing Time in the late 17th century.Dob's Linn is important in geology as the location of the Global Boundary Stratotype Section and Point (GSSP) which marks the boundary between the Ordovician and Silurian periods, and marks the base of the Llandovery epoch, on the geologic time scale. Dob's Linn was ratified as the GSSP by the International Union of Geological Sciences in 1984.The boundary is defined as the first appearance of graptolites Parakidograptus acuminatus and Akidograptus ascensu 1.6 m above the base of the Birkhill Shale Formation. The shale section also contains chitinozoa and conodonts, but neither are well preserved. Dob's Linn has been criticized for the difficulty in relating its graptolite biostratigraphic sequence with shallow water sequences elsewhere, although the stratotype also appears to correspond with a carbon-13 isotope excursion in the latest Ordovician which can be identified worldwide.The area was first studied by Charles Lapworth in the late 19th century. His work established fossil graptolites as a method of understanding stratigraphic sequences. A more recent description of the area, enumerating the zones established by Lapworth, is given in the British Regional Geology Monograph. Before Lapworth's work, it was thought that the Silurian rocks of the Southern Uplands formed a single sequence, that would have to be about 6000m in thickness. By his identification of particular graptolite species in different zones of the Dob's Linn exposure, Lapworth was able to demonstrate that the Uplands consist of a much thinner layer, consistent with Silurian deposits elsewhere, that had been repeatedly folded and faulted, with multiple repetitions of the same strata, often upside down. The understanding that sequences of sedimentary rocks could be inverted played an important part in the later resolution of the Highlands Controversy in which Lapworth was also involved.

The Moffat Hills are a range of hills in the Southern Uplands of Scotland. They form a roughly triangular shape with a west facing side, a north facing side, and a south-east facing side. It is 17 kilometres from east to west across this triangle and some 16 kilometres north to south. The highest point is White Coomb at 821 m (2694 ft). The town of Moffat lies just south of the Moffat hills and along with Tweedsmuir, at the northern extremity, is the only centre of population around these hills. In some older maps, the northern part of the Moffat Hills is called the Tweedsmuir Hills, but can also be known by the title Manor Hills.

Hart Fell is a hill in the Moffat Hills range, part of the Southern Uplands of Scotland. It lies north of the town of Moffat on the border with the Scottish Borders and Dumfries and Galloway. A broad, rolling hill, it is visible from the M74 motorway in the west, parts of Dumfries and ranges to the east. Hart Fell is gently sloping on three sides of the hill, however the east ridge is steep and craggy and features a deep corrie known as Blackhope. The normal route is from the southern ridge, passing over Swatte Fell and can be extended to include a full loop of Blackhope, finishing on Saddle Yoke, known as the Hart Fell Horseshoe.

Cornal Tower is the ruins of a tower house located near Moffat, Dumfries-shire, Scotland. Alternative names are Polcornare, Cornal Burn, or Logan. The ruins are located on a plateau and the grounds consisted of five farms.The place was said to be a hunting lodge for Scottish kings. In the 15th century the land was given to the Carruthers family of Mousewald. Then it was given to Johnstone of Coreheard. It was also later owned by the Duke of Queensberry.Only a portion of the north wall currently remains.

Talla Water is a river in the Scottish Borders area of Scotland, near Tweedsmuir. It feeds the Talla Reservoir, and is a tributary of the River Tweed. Above the reservoir are a series of waterfalls known as the Talla Linns.The Talla Railway was constructed to facilitate the building work, especially the Tweed Viaduct.