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ABERDEENSHIRE , a See also:north-eastern See also:county of See also:Scotland, bounded N. and E. by the North See also:Sea, S. by Kincardine, See also:Forfar and See also:Perth, and W. by See also:Inverness and See also:Banff . It has a See also:coast-See also:line of 65 m., and is the See also:sixth Scottish county in See also:area, occupying 1,261,887 acres or 1971 sq. m . The county is generally hilly, and from the See also:south-See also:west, near the centre of Scotland, the See also:Grampians send out various branches, mostly to the north-See also:east . The See also:shire is popularly divided into five districts . Of these the first is See also:Mar, mostly between the See also:Dee and See also:Don, which nearly covers the See also:southern See also:half of the county and contains the See also:city of See also:Aberdeen . It is mountainous, especially See also:Braemar (q.v.), which contains the greatest See also:mass of elevated See also:land in the See also:British Isles . The See also:soil on the Dee is sandy, and on the Don loamy . The second See also:district, Formartine, between the See also:lower Don and Ythan, has a sandy coast, which is succeeded inland by a clayey, fertile, tilled See also:tract, and then by See also:low hills, See also:moors, mosses and tilled land . See also:Buchan, the third district, lies north of the Ythan, and, comprising the north-east of the county, is next in See also:size to Mar, parts of the coast being bold and rocky, the interior See also:bare, low, See also:flat, undulating and in places peaty . On the coast, 6 m . S. of See also:Peter-See also:head, are the Bullers of Buchan—a See also:basin in which the sea, entering by a natural See also:arch, boils up violently in stormy See also:weather . Buchan Ness is the most easterly point of Scotland .
The See also:fourth
district, Garioch, in the centre of the shire, is a beautiful, undulating, loamy, fertile valley. formerly called the granary of Aberdeen
.
Strathbogie, the fifth district, occupying a consider-able area south of the Deveron, mostly consists of hills, moors and mosses
.
The mountains are the most striking of the See also:physical features of the county
.
See also:Ben Macdhui (4296 ft.), a magnificent mass, the second highest See also:mountain in See also:Great See also:Britain, Braeriach (4248), Cairntoul (4241), Ben-na-bhuaird (3924), Ben See also:Avon (3843), " dark " Lochnagar (3786), the subject of a well-known See also:song by See also:Byron, See also:Cairn Eas (3556), Sgarsoch (3402), Culardoch '(29J3), are the See also:principal heights in the See also:division of Mar
.
Farther north rise the See also:Buck of Cabrach (2368) on the See also:Banffshire border, Tap o' Noth (1830), Bennachie (1698), a beautiful See also:peak which from its central position is a landmark visible from many different parts of the county, and which is celebrated in See also: S.E. of See also:Fraserburgh, is only separated from the sea by a narrow See also:strip of land . There are noted chalybeate springs at See also:Peterhead, Fraserburgh, and Pannanich near Ballater . See also:Geology.—The greater See also:part of the county is composed of crystalline See also:schists belonging to the metamorphic rocks of the Eastern See also:Highlands . In the upper parts of the valleys of the Dee and the Don they See also:form well-marked See also:groups, of which the most characteristic are (1) the See also:black schists and phyllites, with calcflintas, and a thin See also:band of See also:tremolite See also:limestone, (2) the See also:main or See also:Blair See also:Atholl limestone, (3) the See also:quartzite . These divisions are folded on highly inclined or See also:vertical axes trending north-east and south-west, and hence the same zones are repeated over a considerable area . The quartzite is generally regarded as the highest member of the See also:series . Excellent sections showing the component strata occur in Glen Clunie and its tributary valleys above Braemar . Eastwards down the Dee and the Don and northwards across the See also:plain of Buchan towards Rattray Head and Fraserburgh there is a development of See also:biotite See also:gneiss, partly of sedimentary and perhaps partly of igneous origin . A See also:belt of See also:slate which has been quarried for roofing purposes runs along the west border of the county from See also:Turriff by Auchterless and the Foudland Hills towards the Tap o' Noth near Gartly . The metamorphic rocks have been invaded by igneous materials, some before, and by far the larger series after the folding of the strata . The basic types of the former are represented by the sills of See also:epidiorite and See also:hornblende gneiss in Glen Muick and Glen Callater, which have been permeated by See also:granite and See also:pegmatite in See also:veins and lenticles, often foliated . The later granites subsequent to the plication of the schists have a wide See also:distribution on the Ben Macdhui and Ben Avon range, and on Lochnagar; they stretch eastwards from Ballater by Tarland to Aberdeen and north to Bennachie .
Isolated masses appear at Peterhead and at Strichen
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Though consisting mainly of biotite granite, these later intrusions pass by intermediate stages into See also:diorite, as in the area between Balmoral and the head-See also:waters of the Gairn
.
The granites have been extensively quarried at Rubislaw, Peter-head and Kemnay
.
See also:Serpentine and troctolite, the precise See also:age of which is uncertain, occur at the Black See also:Dog See also:rock north of Aberdeen, at Belhelvie and near Old Meldrum
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Where the schists of sedimentary origin have been pierced by these igneous intrusions, they are charged with contact minerals such as See also:sillimanite, cordierite, kyanite and See also:andalusite
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Cordierite-bearing rocks occur near Ellon, at the See also:foot of Bennachie; and on the See also:top of the Buck of Cabrach
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A banded and mottled calc-silicate See also:hornfels occurring with the limestone at Derry Falls, W
.
N.W. of Braemar, has yielded malacolite, See also:wollastonite, See also: The glacial deposits, 'especially in the belt bordering the coast between Aberdeen and Peterhead, furnish important See also:evidence . The See also:ice moved eastwards off the high ground at the head of the Dee and the Don, while the mass spreading outwards from the See also:Moray See also:Firth invaded the low See also:plateau of Buchan; but at a certain See also:stage there was a marked defection northwards parallel with the coast, as proved by the See also:deposit of red See also:clay north of Aberdeen . At a later date the See also:local glaciers laid down materials on top of the red clay . The See also:committee appointed by the British Association (See also:Report for 1897, p . 333) proved that the See also:Greensand, which has yielded a large See also:suite of Cretaceous fossils at Moreseat, in the See also:parish of See also:Cruden, occurs in glacial See also:drift, resting probably on granite . The strata from which the Moreseat fossils were derived are not now found in See also:place in that part of Scotland, but Mr See also:Jukes Brown considers that the See also:horizon of the fossils is that of the lower Greensand of the Isle of See also:Wight or the Aptien stage of See also:France . See also:Chalk flints are widely distributed in the drift between Fyvie and the east coast of Buchan . At Plaidy a patch of clay with Liassic fossils occurs . At several localities between Logie Coldstone and Dinnet a deposit of diatomite (Kieselguhr) occurs beneath the See also:peat . See also:Flora and See also:Fauna.—The tops of the highest mountains have an See also:arctic flora . At the royal See also:lodge on Loch Muick, 1350 ft. above the sea, grow larches, vegetables, currants, laurels, See also:roses, &c . Some ash-trees, four or five feet in girth, are growing at 1300 ft. above the sea . Trees, especially Scotch See also:fir and See also:larch, grow well, and Braemar is See also:rich in natural See also:timber, said to surpass any in the north of See also:Europe . Stumps of Scotch fir and See also:oak found in peat are sometimes far larger than any now growing . The See also:mole is found at 'Soo ft. above the sea, and the See also:squirrel at 1400 . See also:Grouse, partridges and See also:hares are plentiful, and rabbits are often too numerous . Red See also:deer abound in Braemar, the deer See also:forest being the most extensive in Scotland . See also:Climate and See also:Agriculture.—The climate, except in the mountainous districts, is comparatively mild, owing to the proximity of much of the shire to the sea . The mean See also:annual temperature at Braemar is 43.6 F., and at Aberdeen 45.8° . The mean yearly rainfall varies from about.30 to 37 M . The summer climate of the upper Dee and Don valleys is the driest and most bracing in the British Isles, and See also:grain is cultivated up to 1600 ft. above the sea, or 400 to 500 ft. higher than elsewhere in North Britain . Poor, gravelly, clayey and peaty soils prevail, but See also:tile-draining, bones and See also:guano, and the best methods of See also:modern tillage, have greatly increased the produce . Indeed, in no part of Scotland has a more productive soil been made out of such unpromising material . See also:Farm-houses and steadings have much improved, and the best agricultural implements and See also:machines are in See also:general use .
About two-thirds of the See also:population depend entirely on agriculture
.
Farms are small compared with those in the south-eastern counties
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Oats are the predominant See also:crop, See also:wheat has practically gone out of cultivation, but See also:barley has largely increased
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The most distinctive See also:industry is See also:cattle-feeding
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A great number of the See also:home-bred crosses are fattened for the See also:London and local markets, and Irish animals are imported on an extensive See also:scale for the same purpose, while an exceedingly heavy business in dead See also:meat for London and the south is done all over the county
.
See also:Sheep, horses and pigs are also raised in large See also:numbers
.
See also:Fisheries.—A large fishing population in villages along the coast engage in the See also:
The See also:average annual despatch of salmon from Aberdeen-shire is about 400 tons
.
Other See also:Industries.—Manufactures are mainly prosecuted in or near the city of Aberdeen, but throughout the rural districts there is much milling of See also:corn, See also:brick and tile making, See also:
Population and See also:Government.—In 1891 the population numbered 284,036 and in 1901 it was 304,439 (of whom 159,603 were See also:females), or 154 persons to the sq. m
.
In 1901 there were 8 persons who spoke Gaelic only, and 1333 who spoke Gaelic and See also:English
.
The chief towns are Aberdeen (pop. in 1901, 153,503), Bucksburn (2231), Fraserburgh (91o5), I-Iuntly (4136), Inverurie (3624), Peterhead (11,794), Turriff (2273)
.
The Supreme See also:Court of See also:Justiciary sits in Aberdeen to try cases from the counties of Aberdeen, Banff and Kincardine
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The three counties are under a See also:sheriff, and there are two sheriffs-substitute See also:resident in Aberdeen, who sit also at Fraserburgh, Huntly, Peterhead and Turriff
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The sheriff courts are held in Aberdeen and Peterhead
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The county sends two members to See also:parliament -one for East Aberdeenshire and the other for West Aberdeen-shire
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The county See also:town, Aberdeen (q.v.), returns two members
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Peterhead, Inverurie and Kintore belong to the Elgin See also:group of See also:parliamentary burghs, the other constituents being Banff, See also:Cullen and Elgin
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The county is under school-See also:board See also:jurisdiction, and there are also several voluntary See also:schools
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There are higher-class schools in Aberdeen, and secondary schools at Huntly, Peterhead and Fraserburgh, and many of the other schools in the county See also:earn grants for secondary See also:education
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The County Secondary Education Committee dispense a large sum, partly granted by the education See also:department and partly contributed by local authorities from the "See also:residue" See also: The higher branches of education have always been thoroughly taught in the schools throughout the shire, and pupils have long been in the See also:habit of going directly from the schools to the university . The native Scots are long-headed, shrewd, careful, canny, active, persistent, but reserved and See also:blunt, and without See also:demonstrative See also:enthusiasm . They have a See also:physiognomy distinct from the See also:rest of the Scottish See also:people, and have a See also:quick, See also:sharp, rather angry See also:accent . The local Scots See also:dialect is broad, and rich in diminutives, and is noted for the use of e for o or u, f for wh, d for th, &c . So recently as I 83o Gaelic was the fireside See also:language of almost every See also:family in Braemar, but now it is little used . See also:History.—The See also:country now forming the shires of Aberdeen and Banff was originally peopled by See also:northern Picts, whom See also:Ptolemy called Taixali, the territory being named Taixalon . Their town of Devana, once supposed to be the modern Aberdeen, has been identified by Prof . John See also:Stuart with a site in the parish of Peterculter, where there are remains of an See also:ancient See also:camp at Normandykes, and by Dr W . F . See also:Skene with a station on Loch Davan, west of Aboyne . So-called See also:Roman camps have also been discovered on the upper Ythan and Deveron, but evidence of effective Roman occupation is still to seek . Traces of the native inhabitants, however, are much less equivocal .
Weems or See also:earth-houses are fairly See also:common in the west
.
See also:Relics of crannogs or See also:lake-dwellings exist at Loch Ceander, or Kinnord, 5 M. north-east of Ballater, at Loch Goul in the parish of New Machar and elsewhere
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See also:Duns or forts occur on hills at Dunecht, where the dun encloses an area of two acres, See also:Barra near Old Meldrum, Tap o' Noth, Dunnideer near Insch and other places
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Monoliths, See also:standing stones and "Druidical" circles of the See also:pagan See also:period abound, and there are many examples of the sculptured stones of the See also:early See also:Christian See also:epoch
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Efforts to convert the Picts were begun by Ternan in the 5th See also:century, and continued by See also:Columba (who founded a monastery at Old Deer), Drostan, Maluog and Machar, but it was long before they showed lasting results
.
Indeed, dissensions within the See also:Columban See also: (d . 1124) mention is first made of Aberdeen (originally called AberdSn and, in the Norse sagas, Apardion), which received its See also:charter from See also: |