Scottish Borders topographic map

Some have called Edinburgh the Athens of the North for a variety of reasons. The earliest comparison between the two cities showed that they had a similar topography, with the Castle Rock of Edinburgh performing a similar role to the Athenian Acropolis. Both of them had flatter, fertile agricultural land…

Average elevation: 104 m

Glasgow itself was reputed to have been founded by the Christian missionary Saint Mungo in the 6th century. He established a church on the Molendinar Burn, where the present Glasgow Cathedral stands, and in the following years Glasgow became a religious centre. Glasgow grew over the following centuries. The…

Average elevation: 128 m

The Scottish Highlands are renowned for their rugged, mountainous terrain that dominates much of the region. Stretching across the northern and central parts of Scotland, the landscape is shaped by ancient geological forces, including the Caledonian Orogeny, which caused significant tectonic collisions…

Average elevation: 907 m

Average elevation: 275 m

Average elevation: 80 m

Ben Nevis has a highland (alpine) maritime (oceanic) polar climate (ET climate in the Köppen classification). Ben Nevis's elevation, maritime location and topography frequently lead to cool and cloudy weather conditions, which can pose a danger to ill-equipped walkers. According to the observations carried…

Average elevation: 912 m

Average elevation: 161 m

The source of the river is Blairdenon Hill in the Ochils at an altitude of 1,800 feet (550 m). Upper areas have been dammed, creating Upper Glendevon, Lower Glendevon and Castlehill reservoirs. The Devon then flows east and southeast through Glendevon, turning southwest at Crook of Devon and then continuing…

Average elevation: 96 m

Glasgow itself was reputed to have been founded by the Christian missionary Saint Mungo in the 6th century. He established a church on the Molendinar Burn, where the present Glasgow Cathedral stands, and in the following years Glasgow became a religious centre. Glasgow grew over the following centuries as part…

Average elevation: 128 m

The entire region was covered by ice sheets during the Pleistocene ice ages, save perhaps for a few nunataks. The complex geomorphology includes incised valleys and lochs carved by the action of mountain streams and ice, and a topography of irregularly distributed mountains whose summits have similar heights…

Average elevation: 907 m

According to the 1846 A Topographical Dictionary of Scotland, "This parish, formerly called Skirdustan, signifying, in the Gaelic tongue, 'the division of Dustan', its tutelary saint, derived its present name from its situation at the mouth of a noisy burn, which discharges itself into the river Spey."

Average elevation: 160 m

Average elevation: 99 m

Towards the end of the 16th century, a detailed assessment on the size of the townscape was carried out. The first estimate of the parish population in 1639 was between 3,000 and 3,200 and around 3,400 by 1691. At the beginning of the 18th century, the population declined. A census by Webster's Topographical…

Average elevation: 50 m

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In a small glen above Ailsa Castle, a small freshwater body known as the Garry Loch is located at an altitude of 247 m (810 ft), with a depth of at least 17 feet.

Average elevation: 14 m

Average elevation: 9 m

Average elevation: 236 m

Average elevation: 222 m

Ailsa Craig and the County Antrim coast of Ulster and Rathlin Island are all clearly visible from the Mull. On clearer days it is also possible to make out Malin Head in Inishowen in County Donegal in the west of Ulster, and the Ayrshire coast on the other side of Ailsa Craig. Other islands in the Firth of…

Average elevation: 84 m

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Average elevation: 6 m

Two weather stations collect climate data for the area, Aberdeen/Dyce Airport, and Craibstone. Both are about 4 1⁄2 miles (7 km) to the north west of the city centre, and given that they are in close proximity to each other, exhibit very similar climatic regimes. Dyce tends to have marginally warmer daytime…

Average elevation: 52 m

Dundee sits on the north bank of the Firth of Tay on the eastern, North Sea Coast of Scotland. The city lies 36.1 miles (58 km) NNE of Edinburgh and 360.6 miles (580 km) NNW of London. The built-up area occupies a roughly rectangular shape 8.3 miles (13 km) long by 2.5 miles (4 km) wide, aligned in an east to…

Average elevation: 82 m

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Average elevation: 268 m

In the 1846 book A Topographical Dictionary of Scotland, Samuel Lewis writes.

Average elevation: 167 m

Average elevation: 304 m

Average elevation: 25 m

Cumbernauld's name probably comes from the Gaelic comar nan allt, meaning "meeting of the burns or streams". There are differing views as to the etymology of this. One theory is that from its high point in the Central Belt, its streams flow both west to the River Clyde and east to the Firth of Forth so…

Average elevation: 111 m

Average elevation: 110 m

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Average elevation: 140 m

Wigtown Castle was in existence by 1291, on flat land down by the River Bladnoch, (outlines clearly seen on an aerial view), whilst the town and church were on a hill, "an inversion of the usual arrangements". Nothing remains of the castle, although a strong natural site and indication of a large enclosed and…

Average elevation: 18 m

Average elevation: 69 m

Falkirk is located in an area of undulating topography between the Slamannan Plateau and the upper reaches of the Firth of Forth. The area to the north of Falkirk is part of the floodplain of the River Carron. Two tributaries of the River Carron - the East Burn and the West Burn flow through the town and form…

Average elevation: 69 m

Average elevation: 70 m

Average elevation: 55 m

Average elevation: 151 m