River Clyde topographic map

Average elevation: 107 m

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Average elevation: 278 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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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).

Average elevation: 283 m

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Average elevation: 61 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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In the 1846 book A Topographical Dictionary of Scotland, Samuel Lewis writes.

Average elevation: 167 m

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Average elevation: 63 m

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: 229 m

Lerwick has an oceanic climate (Cfb) closely bordering on a subpolar oceanic climate (Cfc) with cool to cold temperatures all year long. The lack of trees reflects the latter type. This is particularly pronounced by virtue of Lerwick being on the coast of an island, so even extreme temperature records are…

Average elevation: 39 m

The earliest-known evidence of occupation in the area dates as far back as the late Neolithic and Early Bronze Age, as archaeological investigation has demonstrated that burial cairns in the district began as ceremonial or ritual sites of burial during the Neolithic, with the use of cup-marked, and other…

Average elevation: 174 m

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Average elevation: 25 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

It lies in a strath 5 miles (8 km) west of Dingwall, with the elevation ranging from 60 to 120 m (200 to 400 ft) above sea level. Sheltered on the west and north, it has a comparatively dry and warm climate.

Average elevation: 127 m

Average elevation: 117 m

Average elevation: 61 m

Average elevation: 50 m