618:
40:
335:... until comparatively recent times, Deeside was an isolated and little frequented region and the reason for this is the extensive mountain barrier of the Grampians which begins in a low range on the seacoast immediately south of Aberdeen and rise through various intervening heights such as Cairn-mon-earn (1,245 ft), Kerloch (1,747 ft), Mount Battoch (2,555 ft), Mount Keen (3,007 ft), Lochnagar (3,786 ft), Beinn a' Ghlo (3,671 ft), to Beinn Dearg (3,556 ft)
186:
561:
553:
The speech "acquired a life of its own, independent of the play, and became widely known through public recitations, lessons in speech, school memorizations and the like" during the 18th and 19th centuries. The speech (and thus the reference to the
Grampian Hills) are casually referred to by Jane
369:
in the west almost to the sea just south of
Aberdeen. Many maps and books have given its name as 'the Grampians' but although children have to learn this at school, they do not learn it at home and nowhere is it used in local speech. Some map-makers have confused the issue by printing 'Grampians'
327:
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
550:
My name is Norval; on the
Grampian Hills My father feeds his flocks; a frugal swain, Whose constant cares were to increase his store. And keep his only son, myself, at home.
388:. 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.
137:
There is some ambiguity about the extent of the range, and until the nineteenth century, they were generally considered to be more than one range, which all formed part of the wider
380:
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
458:
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:
223:, 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
764:
Stephenson, D, and Gould, D. 1995. British regional geology: the
Grampian Highlands. Fourth edition. Reprint 2007. Keyworth, Nottingham: British Geological Survey.
870:
345:
This introduction appears to suggest that Wyness defines the
Grampians as being the range of mountains running from immediately south of Aberdeen westward to
831:
153:. 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
890:
885:
158:
880:
820:
875:
895:
597:
395:
from the
Grampians, but the 1911 Encyclopedia Britannica adopted a wider definition, including the highlands as far as
696:
560:
905:
87:(whose peak contains the highest point in the British Isles at 1,345 m or 4,413 ft above sea level) and
602:
567:
20:
346:
31:
146:
142:
127:
123:
52:
672:
354:
76:
24:
587:
311:
is believed to have first been applied to the mountain range in 1520 by the
Scottish historian
216:
88:
814:
508:
439:
8:
447:
174:
68:
301:"Graupius" was incorrectly rendered "Grampius" in the 1476 printed edition of Tacitus's
194:
607:
392:
138:
900:
700:
623:
350:
280:
107:
83:. The range includes many of the highest mountains in the British Isles, including
72:
19:
This article is about the mountains in Scotland. For the hills in New Zealand, see
644:
302:
250:
162:
131:
111:
39:
734:
542:
396:
292:
236:
150:
115:
864:
846:
833:
809:
530:
519:
245:
207:
141:. This view is still held by many today, and they have no single name in the
442:(<2.6 Ma) eroded the region significantly, and glacial deposits, such as
67:, that together occupy about half of Scotland. The other two ranges are the
704:
477:
467:
443:
312:
170:
154:
119:
503:
408:
256:
232:
212:
103:
824:. Vol. 12 (11th ed.). Cambridge University Press. p. 333.
775:
547:, the second act begins with a speech that mentions the Grampian Hills:
498:
462:
366:
358:
190:
99:
91:(whose peak contains second-highest at 1,309 m or 4,295 ft).
80:
813:
582:
514:
487:
432:
95:
84:
699:
Edited extract from Under Another Sky: Journeys in Roman Britain by
94:
A number of rivers and streams rise in the Grampians, including the
592:
494:
361:, specifically excluded the range south of the River Dee, writing:
228:
185:
64:
60:
647:
Map, Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2002
482:
416:
412:
381:
202:
75:. The Grampian range extends northeast to southwest between the
697:
History in the making: a Roman map... and an 18th-century hoax.
472:
428:
424:
420:
385:
260:
224:
283:
and represent a corrupted form, of which the genuine would be
524:
319:. Thus the range may owe its name to a typesetter's mistake.
673:"Philology on Tacitus's Graupian Hill and Trucculan Harbour"
738:. Edinburgh: The Scottish Mountaineering Trust. p. 19.
263:, a name still held by a number of geographical features.
365:
The other main hill group is the long chain running from
719:
Royal Valley : The Story Of The Aberdeenshire Dee
329:
Royal Valley : The Story Of The Aberdeenshire Dee
613:
776:"In search of the Grampian Hills with W. C. Fields"
554:Austen, Charles Dickens, and George Bernard Shaw.
255:believed to be from the mid-9th century. In the
43:Location of the Grampian Mountains within Scotland
391:Wyness and Watson both exclude areas west of the
370:over the Cairngorms and Strath Don hills as well!
862:
30:"Grampians" redirects here. For other uses, see
871:Mountains and hills of Highland (council area)
407:The Grampian Mountains are chiefly made up of
721:, Alex P. Reid & Son, Aberdeen, p. 1
750:Scotland's Mountains Before the Mountaineers
134:. The area is generally sparsely populated.
692:
690:
752:, pp. 62–63. Published 2013, Luath Press.
315:, perhaps an adaptation of the incorrect
891:Mountains and hills of Perth and Kinross
808:
666:
664:
662:
656:Agricola, edited by Ogilvie and Richmond
211:as the site of the defeat of the native
184:
38:
742:
687:
886:Mountains and hills of Angus, Scotland
863:
760:
758:
731:
716:
670:
23:. For the mountains in Australia, see
710:
659:
415:rocks. The mountains are composed of
881:Mountains and hills of Aberdeenshire
570:View of the Grampian Mountains, 1831
755:
598:List of deaths on eight-thousanders
13:
357:, when defining the extent of the
275:in 83 A.D, the origin of the name
14:
917:
802:
219:c. 83 AD. The actual location of
165:(translated into Scots Gaelic as
616:
559:
536:
249:, a mediaeval copy of Tacitus's
774:Prior, Moody E. (Winter 1979).
603:Mountains and hills of Scotland
259:, this locale was known as the
767:
725:
650:
637:
279:is uncertain. The name may be
1:
630:
453:
876:Mountains and hills of Moray
266:
159:former local government area
59:) is one of the three major
7:
896:Mountain ranges of Scotland
575:
446:, are largely those of the
21:The Grampians (New Zealand)
10:
922:
773:
402:
32:Grampians (disambiguation)
29:
18:
16:Mountain range in Scotland
541:In the popular 1756 play
322:
143:Scottish Gaelic language
906:Highland Boundary Fault
821:Encyclopædia Britannica
717:Wyness, Fenton (1968),
671:Andrew, Breeze (2002).
180:
77:Highland Boundary Fault
25:Grampians National Park
815:"Grampians, The"
378:
343:
291:meaning "ridge" (c.f.
217:Gnaeus Julius Agricola
198:
56:
44:
732:Watson, Adam (1975).
440:Quaternary glaciation
363:
333:
188:
42:
780:The American Scholar
588:Buachaille Etive Mòr
201:The Roman historian
843: /
677:Proc Soc Antiq Scot
175:Grampian Television
69:Northwest Highlands
608:Scottish Highlands
393:Pass of Drumochter
271:Recorded first as
199:
139:Scottish Highlands
49:Grampian Mountains
45:
701:Charlotte Higgins
493:The mountains of
167:Roinn a' Mhonaidh
913:
858:
857:
855:
854:
853:
848:
847:56.917°N 4.000°W
844:
841:
840:
839:
836:
825:
817:
796:
795:
793:
791:
771:
765:
762:
753:
748:Ian R Mitchell.
746:
740:
739:
729:
723:
722:
714:
708:
694:
685:
684:
668:
657:
654:
648:
641:
626:
624:mountains portal
621:
620:
619:
563:
376:
351:Forest of Atholl
341:
157:, including the
108:Burn of Muchalls
73:Southern Uplands
921:
920:
916:
915:
914:
912:
911:
910:
861:
860:
851:
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842:
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789:
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772:
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763:
756:
747:
743:
730:
726:
715:
711:
695:
688:
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660:
655:
651:
645:Ordnance Survey
643:United Kingdom
642:
638:
633:
622:
617:
615:
612:
578:
573:
572:
571:
569:
564:
551:
539:
456:
405:
377:
374:
342:
339:
325:
269:
243:comes from the
239:. The spelling
183:
163:Grampian Region
112:Burn of Pheppie
53:Scottish Gaelic
35:
28:
17:
12:
11:
5:
919:
909:
908:
903:
898:
893:
888:
883:
878:
873:
852:56.917; -4.000
827:
826:
812:, ed. (1911).
810:Chisholm, Hugh
804:
803:External links
801:
798:
797:
766:
754:
741:
735:The Cairngorms
724:
709:
707:, 19 July 2013
686:
658:
649:
635:
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632:
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556:
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533:
527:
522:
517:
512:
506:
501:
491:
485:
480:
475:
470:
465:
455:
452:
450:(< 20 Ka).
404:
401:
397:Dunbartonshire
372:
337:
324:
321:
268:
265:
237:Kempstone Hill
227:, possibly at
182:
179:
116:Burn of Elsick
15:
9:
6:
4:
3:
2:
918:
907:
904:
902:
899:
897:
894:
892:
889:
887:
884:
882:
879:
877:
874:
872:
869:
868:
866:
859:
856:
823:
822:
816:
811:
807:
806:
785:
781:
777:
770:
761:
759:
751:
745:
737:
736:
728:
720:
713:
706:
703:published in
702:
698:
693:
691:
682:
678:
674:
667:
665:
663:
653:
646:
640:
636:
625:
614:
609:
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604:
601:
599:
596:
594:
591:
589:
586:
584:
581:
580:
568:
562:
555:
548:
546:
545:
537:In Literature
532:
531:Isle of Arran
528:
526:
523:
521:
520:Arrochar Alps
518:
516:
513:
510:
507:
505:
502:
500:
496:
492:
489:
486:
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481:
479:
476:
474:
471:
469:
466:
464:
461:
460:
459:
451:
449:
445:
441:
436:
434:
430:
426:
422:
418:
414:
410:
400:
399:in the west.
398:
394:
389:
387:
383:
371:
368:
362:
360:
356:
353:. Similarly,
352:
348:
340:Fenton Wyness
336:
332:
330:
320:
318:
317:Mons Grampius
314:
310:
306:
305:
299:
297:
294:
290:
287:, containing
286:
282:
278:
274:
264:
262:
258:
254:
253:
248:
247:
246:Codex Aesinas
242:
238:
234:
230:
226:
222:
221:Mons Graupius
218:
214:
210:
209:
208:Mons Graupius
204:
196:
195:Beinn a' Ghlò
192:
187:
178:
176:
172:
168:
164:
160:
156:
152:
151:Lowland Scots
148:
147:Doric dialect
144:
140:
135:
133:
129:
125:
121:
117:
113:
109:
105:
101:
97:
92:
90:
86:
82:
78:
74:
70:
66:
62:
58:
54:
50:
41:
37:
33:
26:
22:
828:
819:
788:. Retrieved
786:(1): 102–103
783:
779:
769:
749:
744:
733:
727:
718:
712:
705:The Guardian
680:
676:
652:
639:
552:
543:
540:
478:Grey Corries
468:Monadh Liath
457:
448:last Ice Age
437:
406:
390:
379:
364:
344:
334:
328:
326:
316:
313:Hector Boece
308:
303:
300:
295:
288:
284:
276:
272:
270:
251:
244:
240:
220:
206:
200:
171:NHS Grampian
166:
155:Central Belt
136:
120:Cairnie Burn
93:
48:
46:
36:
850: /
509:Breadalbane
504:Black Mount
409:metamorphic
375:Adam Watson
355:Adam Watson
347:Beinn Dearg
307:. The name
257:Middle Ages
233:Megray Hill
213:Caledonians
104:Cowie Water
865:Categories
683:: 305–311.
631:References
499:Glen Etive
463:Cairngorms
454:Sub-ranges
367:Drumochter
359:Cairngorms
191:Cairngorms
89:Ben Macdui
81:Great Glen
63:ranges in
583:Ben Nevis
515:Trossachs
488:Ben Alder
433:quartzite
309:Grampians
281:Brittonic
277:Grampians
267:Etymology
205:recorded
85:Ben Nevis
57:Am Monadh
901:Grampian
593:Glen Coe
576:See also
495:Glen Coe
384:for the
373:—
338:—
304:Agricola
285:*Cripius
273:Graupius
252:Germania
241:Graupius
229:Raedykes
79:and the
71:and the
65:Scotland
61:mountain
835:56°55′N
544:Douglas
483:Mamores
429:schists
417:granite
413:igneous
403:Geology
382:synonym
349:in the
203:Tacitus
145:or the
838:4°00′W
790:8 June
490:Forest
473:Mounth
425:marble
421:gneiss
386:Mounth
323:Extent
261:Mounth
225:massif
173:, and
525:Cowal
511:Hills
444:tills
293:Welsh
289:*crip
193:from
792:2023
529:The
497:and
438:The
431:and
411:and
296:crib
189:The
181:Name
130:and
100:Spey
47:The
681:132
298:).
235:or
215:by
169:),
161:of
149:of
132:Esk
128:Dee
124:Don
96:Tay
867::
818:.
784:48
782:.
778:.
757:^
689:^
679:.
675:.
661:^
435:.
427:,
423:,
419:,
331::
231:,
177:.
126:,
122:,
118:,
114:,
110:,
106:,
102:,
98:,
55::
794:.
197:.
51:(
34:.
27:.
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