Caithness 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 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

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

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

Average elevation: 167 m

Newtonmore is located within the Cairngorms National Park, approximately 3 miles (5 km) southwest of Kingussie and 15 miles (24 km) southwest of Aviemore. It is on the northeastern bank of the River Spey, between the River Calder and the Allt Lairaidh, at an altitude of approximately 250 metres (820 ft).

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Historically part of Stirlingshire, Kilsyth is at an elevation of 200 feet (60 metres) above sea level and occupies a narrow strip of land between the Kilsyth Hills to the north and the River Kelvin to the south. To the east and west it is bordered by marshland and bogs. The centre of the town is close to the…

Average elevation: 161 m

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Average elevation: 117 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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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

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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

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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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The topography of Coatbridge was an important feature in the town's development during the industrial revolution. Coatbridge rests 60 metres below the "Slamannan plateau" and neighbouring Airdrie sits on its edge. The low-lying flat ground of Coatbridge was a vital factor in the siting of the town's blast…

Average elevation: 100 m

Average elevation: 25 m

Elgin is first documented in the Cartulary of Moray in 1190 AD. It was created a royal burgh in the 12th century by King David I of Scotland, and by that time had a castle on top of the present-day Lady Hill to the west of the town. The origin of the name Elgin is likely to be Celtic. It may derive from…

Average elevation: 26 m

Average elevation: 98 m

Fort William has an oceanic climate (Cfb) with moderate, but generally cool, temperatures and abundant precipitation. In the towns immediate vicinity, there are significant variations in elevation, which leads to some uninhabited areas near the town having a subpolar oceanic climate (Cfc), or, at the absolute…

Average elevation: 122 m

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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

Average elevation: 114 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

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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

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Average elevation: 57 m

Ballater (/ˈbælətər/, Scottish Gaelic: Bealadair) is a village in Aberdeenshire, Scotland, on the River Dee, immediately east of the Cairngorm Mountains. Situated at an elevation of 213 metres (699 feet), Ballater is a centre for hikers and known for its spring water, once said to cure scrofula. It is home…

Average elevation: 360 m

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