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The journey to Ben Macdhui is a hard walk which goes along Càrn a' Mhàim's northern ridge with Irvine Butterfield saying: "The ridge linking Carn a' Mhaim to Ben Macdhui is the only one of its kind in the Cairngorms, an exhilarating arête commanding a fine prospect of The Devil's Point and Cairn Toul " .
Coire an t-Sneachda (sometimes misspelled as Coire an t'Sneachda) is a glacial cirque or corrie landform in the Cairngorm or Am Monadh Ruadh mountain range in the Grampian Mountains of the Scottish Highlands. The summits of Cairn Lochan (1215 m) and Stob Coire an t-Sneachda (1176 m) lie above Coire an t-Sneachda's headwall.
Cairn Gorm (Scottish Gaelic: An Càrn Gorm) [4] is a mountain in the Scottish Highlands.It is part of the Cairngorms range and wider Grampian Mountains.With a summit elevation of 1,245 m (4,085 ft) above sea level, Cairn Gorm is classed as a Munro and is the sixth-highest mountain in the British Isles.
It lies within the Cairngorms National Park, close to the villages of Nethy Bridge, Boat of Garten, and Aviemore. The forest is an RSPB reserve, close to Loch Garten Osprey Centre, which is also owned by the RSPB. It is popular with walkers, as there are various trails throughout the reserve. [4]
The Cairngorms became part of Scotland's second national park (the Cairngorms National Park) on 1 September 2003. [2] Although the Cairngorms give their name to, and are at the heart of, the Cairngorms National Park, they only form one part of the national park, alongside other hill ranges such as the Angus Glens and the Monadhliath , and lower ...
Cairngorms National Park (Scottish Gaelic: Pàirc Nàiseanta a' Mhonaidh Ruaidh) is a national park in northeast Scotland, established in 2003. It was the second of two national parks established by the Scottish Parliament , after Loch Lomond and The Trossachs National Park , which was set up in 2002.
Derry Cairngorm is characterised by large granite boulders on its higher slopes which make walking in the summit area difficult, the walker often having to resort to hopping between boulders. This large expanse of boulders is formed by the action of freezing and thawing in a periglacial environment and is known as a blockfield or felsenmeer. [4]
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