Grampian Mountains

The Grampian Mountains ("Am Monadh" in Gaelic) are one of the three major mountain ranges in Scotland, occupying a considerable portion of the Scottish Highlands in northern Scotland. The other major mountain ranges in Scotland are the Northwest Highlands and the Southern Uplands. The Grampian 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 (the highest point in the British Isles at above sea level) and Ben Macdui (the second-highest at ).
A number of rivers and streams rise in the Grampians, including the Tay, Spey, Cowie Water, Burn of Muchalls, Burn of Pheppie, Burn of Elsick, Cairnie Burn, Don, Dee and Esk. The area is generally sparsely populated.
There is some ambiguity about the extent of the range, and until the 19th century, they were generally considered to be more than one range, which all formed part of the wider Scottish Highlands. This view is still held by many today, and they have no single name in the Scottish Gaelic language or the Doric dialect of Lowland Scots. In both languages, a number of names are used. The name "Grampian" has been used in the titles of organisations covering parts of Scotland north of the Central Belt, including the former local government area of Grampian Region (translated into Scots Gaelic as "Roinn a' Mhonaidh"), NHS Grampian, and Grampian Television.
Name.
The Roman historian Cornelius Tacitus recorded "Mons Graupius" as the site of the defeat of the native Caledonians by Gnaeus Julius Agricola c. 83 AD. The actual location of "Mons Graupius", literally 'Mount Graupius' (the element 'Graupius' is of unknown meaning), is a matter of dispute among historians, though most favour a location within the Grampian massif, possibly at Raedykes, Megray Hill or Kempstone Hill. The spelling "Graupius" comes from the Codex Aesinas, a mediaeval copy of Tacitus's Germania believed to be from the mid-9th century. "Graupius" was incorrectly rendered "Grampius" only in the 1476 printed edition of Tacitus's biography of Agricola. The name "Grampians" is believed to have first been applied to the mountain range in 1520 by the Scottish historian Hector Boece, an adaptation of the incorrect "Mons Grampius". Thus the range owes its name to this day to a typesetter's mistake. In the Middle Ages, this locale was known as the Mounths, a name still held by a number of geographical features.
Etymology.
Recorded first as "Graupius" in 83 A.D, the genesis of the name "Grampians" is uncertain. The name may be Brittonic and represent a corrupted form, "*Cripius", containing "*crip" meaning "ridge" (c.f. Welsh "crib").
Extent.
There is some ambiguity about the extent of the range. Fenton Wyness, writing about Deeside, puts the northern edge of the Grampians at the River Dee in the introduction to his 1968 book "Royal Valley : The Story Of The Aberdeenshire Dee":
This introduction appears to suggest that Wyness defines the Grampians as being the range of mountains running from immediately south of Aberdeen westward to Beinn Dearg in the Forest of Atholl. Similarly, Adam Watson, when defining the extent of the Cairngorms, specifically excluded the range south of the River Dee, writing:
Both Wyness and Watson appear to exclude the Cairngorms from the Grampians, regarding them as a separate range. In effect, Wyness' and Watson's definition of the Grampians is as a synonym for the Mounth. However Robert Gordon, writing in the 1650s, used the term Grampians to refer to hills on either side of the River Dee, and thus explicitly included the Cairngorms within the range.
Geology.
The mountains are composed of granite, gneiss, marble, schists and quartzite.
Sub-ranges.
The following ranges of hills and mountains fall within the generally recognised definition of the Grampians, i.e lying between the Highland and Great Glen fault lines: