Dundee City 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

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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

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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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

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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

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

Average elevation: 149 m

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

Average elevation: 167 m

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Schiehallion lies between Loch Tay, Loch Rannoch and Loch Tummel, about 10 miles (16 kilometres) to the west-north-west of Aberfeldy in Perthshire. The mountain, with an elevation of 1,083 metres (3,553 ft), is isolated from other peaks and has an almost perfectly conical shape from the west. The view of the…

Average elevation: 652 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."

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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

Average elevation: 276 m

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Average elevation: 218 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

Average elevation: 228 m

Average elevation: 100 m

Average elevation: 37 m

To the northeast of the town a hill fort, possibly of Pictish date or earlier, stands atop Barry (or 'barrow') Hill. It is considered to be one of the best preserved examples of an enclosed hilltop settlement in Scotland. The remains consist of massive collapsed stone ramparts that take advantage of the…

Average elevation: 125 m

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Average elevation: 181 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

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Average elevation: 163 m

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Average elevation: 127 m

Average elevation: 121 m

To the northeast of the town a hill fort, possibly of Pictish date or earlier, stands atop Barry (or 'barrow') Hill. It is considered to be one of the best preserved examples of an enclosed hilltop settlement in Scotland. The remains consist of massive collapsed stone ramparts that take advantage of the…

Average elevation: 125 m

Average elevation: 557 m

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Average elevation: 463 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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These findings have found further support through ongoing research indicating that many East Kilbride Cairns first noticed by the Reverend David Ure in his History of Rutherglen and East Kilbride (1793), are embedded, alongside other monuments, into a ritual landscape related to ancestor cults and…

Average elevation: 174 m

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Tomintoul has an oceanic climate (Cfb), bordering on subpolar oceanic (Cfc). Since March 2025, Tomintoul has an official MetOffice weather station. Manual readings are sent to the Met-Office on a daily basis. The temperature values below are simulated and not taken from this weather station. Due to the…

Average elevation: 374 m

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Average elevation: 151 m

These findings have found further support through ongoing research indicating that many East Kilbride Cairns first noticed by the Reverend David Ure in his History of Rutherglen and East Kilbride (1793), are embedded, alongside other monuments, into a ritual landscape related to ancestor cults and…

Average elevation: 174 m

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