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Grampian Highlands : ウィキペディア英語版
Grampian Mountains

The Grampian Mountains or Grampians (''Am Monadh'' in Gaelic) are one of the three major mountain ranges in Scotland, occupying a considerable portion of the Scottish Highlands in northeast Scotland. The range extends southwest to northeast between the Highland Boundary Fault and the Great Glen, occupying almost half of the land-area of Scotland and including the Cairngorms and the Lochaber hills. The range includes many of the highest mountains in the British Isles, including Ben Nevis and Ben Macdui the two highest.
==Extent==
There is some ambiguity about the extent of the range. In the introduction of Wyness (1969) the author, writing about Deeside, puts the northern-edge of the Grampians at the River Dee when he writes:
Clearly, then, Wyness defines the Cairngorm as being the range of mountains running from immediately south of Aberdeen’ westward to Beinn Dearg in the Forest of Atholl.
In Watson (1975) the author – while defining the extent of the Cairngorms – specifically excludes the range south of the River Dee, writing:
Both Wyness and Watson roughly agree where the eastern, northern, and western limits of The Cairngorms lie.
The Grampians extend southwest to northeast between the Highland Boundary Fault and the Great Glen, occupying almost half of the land-area of Scotland. This includes the Cairngorms and the Lochaber hills. The range includes Ben Nevis (the highest point in the British Isles at 1,344 metres above sea level) and Ben Macdui (the second highest at 1,309 metres).
The mountains are composed of granite, gneiss, marble, schists and quartzite. The other major mountain ranges in Scotland are the Northwest Highlands and the Southern Uplands.
A number of rivers and streams rise in the Grampians: the Tay, Spey, Cowie Water, Burn of Muchalls, Burn of Pheppie, Burn of Elsick, Cairnie Burn, Don, Dee and Esk.〔United Kingdom Ordnance Survey Map, Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2002〕 The area is generally sparsely populated.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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