Inverclyde topographic map

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

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

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

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: 115 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

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

Average elevation: 163 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: 9 m

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Average elevation: 141 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

Average elevation: 36 m

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Average elevation: 77 m

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Average elevation: 683 m

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Average elevation: 91 m

Average elevation: 0 m

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: 26 m

Average elevation: 191 m

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Average elevation: 469 m

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Average elevation: 118 m

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Average elevation: 585 m

Average elevation: 124 m

Average elevation: 355 m

Average elevation: 101 m

Average elevation: 32 m

Brimmond Hill is a hill in Aberdeen, Scotland. The summit is the highest point within the Aberdeen City council area, at an elevation of 266 m (873 ft).

Average elevation: 165 m

Average elevation: 210 m

Average elevation: 42 m

Average elevation: 3 m

Average elevation: 24 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: 183 m

Average elevation: 24 m

Average elevation: 15 m

Average elevation: 63 m

Average elevation: 0 m

Average elevation: 6 m

Average elevation: 217 m

Average elevation: 55 m

Average elevation: 71 m

Average elevation: 80 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: 25 m

Average elevation: 25 m

Average elevation: 99 m

Average elevation: 29 m

Average elevation: 34 m

Average elevation: 11 m

Average elevation: 206 m

Average elevation: 216 m

Average elevation: 95 m

Average elevation: 40 m

Average elevation: 86 m

Average elevation: 135 m

Average elevation: 138 m

Average elevation: 131 m

Average elevation: 129 m

Average elevation: 29 m

Average elevation: 461 m

Average elevation: 40 m

Average elevation: 64 m

Average elevation: 223 m

The village is on fairly level terrain at an elevation of 100m, an elevation which proved challenging for the design of the old Formartine and Buchan Railway running to the Village. There are a number of springs and burns around the village notably Pinkie Burn to the SE and the longer Burn of Straloch to the…

Average elevation: 107 m

Average elevation: 166 m