68-412: Aberdeen North may refer to: Aberdeen North (UK Parliament constituency) Aberdeen North (Scottish Parliament constituency) Topics referred to by the same term [REDACTED] This disambiguation page lists articles associated with the title Aberdeen North . If an internal link led you here, you may wish to change the link to point directly to
136-665: A hanse (trading league). The Diocese of Aberdeen was in existence by the 1150s. Like much of Scotland, the influence of clans led by powerful families was significant. Many such clans in Aberdeenshire came to prominence in the 12th and 13th centuries, including the clans of Mar , Leslie , Bissett , Comyn and Cheyne . During the English invasion of 1296 , the English army under Edward I took control of Aberdeen Castle . The following year, William Wallace surprised
204-639: A registration county . The area of the historic county excluding the Aberdeen City council area is also a lieutenancy area . The area is generally hilly. The south-west of the county includes part of the Grampian Mountains . The historic county borders Kincardineshire , Angus and Perthshire to the south, Inverness-shire and Banffshire to the west, and the North Sea to the north and east. The area which would become Aberdeenshire
272-437: A sheriff ) are obscure. There is some evidence that it was a shire from the time of David I (reigned 1124–1153), but the earliest documented Sheriff of Aberdeen was in the 13th century. The sheriff's jurisdiction covered the older provinces of Buchan , Formartine , Garioch , and Marr (or Mar). Over time, Scotland's shires became more significant than the old provinces, with more administrative functions being given to
340-505: A hundred years after Bruce's death in 1329, there was intermittent conflict in the shire. The English burned Aberdeen itself in 1336. The dispossession and re-settlement of the districts of Buchan and Strathbogie caused numerous disputes. Moreover, the crown had embroiled itself with some of the Highland chieftains, whose independence it sought to abolish. This policy culminated in the invasion of Aberdeenshire by Donald of Islay, Lord of
408-470: A more productive soil developed out of such unpromising material. Farm-houses and steadings have much improved, and the best agricultural implements and machines get widespread use. About two-thirds of the population depend entirely on agriculture. Farms are small compared with those in the south-eastern counties. Oats form the predominant crop, wheat has practically gone out of cultivation, but barley has largely increased. The most distinctive industry in 1911
476-542: A new list of wards. The new wards were Mastrick, Northfield, St Clement's, St Machar, St Nicholas, and Woodside. February 1974 boundaries were used also for the October 1974 general election . In 1975, throughout Scotland, under the Local Government (Scotland) Act 1973 , counties were abolished, and the enlarged City of Aberdeen district was formed by including areas formerly within the county of Aberdeen and
544-480: A very important part of the North East economy. Farm sizes are perhaps still relatively smaller than UK but there are some significant agribusinesses in Aberdeenshire. Few farmers raise horses, though horses are more common, kept by private owners & specialists, than in any other area of Scotland. In 1911 a large fishing population in villages along the coast engage in the white and herring fishery, fostering
612-415: Is Banff and Buchan which, like West Aberdeenshire and Kincardine, is entirely within the Aberdeenshire council area. Fifth Review changes include the transfer of Bridge of Don , Dyce and Danestone areas from Aberdeen North to Gordon, and the new Aberdeen North has boundaries which are very different from those of the earlier constituency. The northern boundary of the earlier constituency coincided with
680-449: Is only separated from the sea by a narrow strip of land. There are noted chalybeate springs at Peterhead, Fraserburgh, and Pannanich near Ballater . Other lochs of note are Loch Kinord , Loch Davan , Dubh Loch , Lochnagar , Loch Callater , Loch nan Eun and the Loch of Skene . The greater part of the county is composed of crystalline schists belonging to the metamorphic rocks of
748-700: The 1886 general election , the 1892 general election , the 1895 general election , the 1900 general election , the 1906 general election , the January 1910 general election and the December 1910 general election . In 1918 constituency boundaries were redefined by the Representation of the People Act 1918 . By then the county of city of Aberdeen had been created and, together with Aberdeen North, Aberdeen South became one of two constituencies covering
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#1732780139328816-489: The 1945 general election . For the 1950 general election boundaries were redefined again, by the House of Commons (Redistribution of Seats) Act 1949 . A new list of wards defined Aberdeen North - Glimonston, Greyfriars, St Clement, St Machar, St Nicholas and Woodside - but the county of city of Aberdeen remained a two-constituency city, divided between Aberdeen South and Aberdeen North, with both constituencies entirely within
884-474: The 2023 Periodic Review of Westminster constituencies the newly redrawn Aberdeen North to be fought at the 2024 United Kingdom general election consists of the following electoral wards: [REDACTED] From 1832 to 1885 there was a single Aberdeen constituency. Prior to 1832, the burgh of Aberdeen had been represented as a component of the Aberdeen Burghs constituency. When Aberdeen North
952-545: The Aberdeenshire council area . To the south of Aberdeen North there is Aberdeen South , which is also entirely within the Aberdeen City council area. To the west there is West Aberdeenshire and Kincardine , which is entirely within the Aberdeenshire council area, and to the north there is Gordon , which covers part of the Aberdeen City council area and part of the Aberdeenshire council area. Further north there
1020-569: The Cairngorms provide the most striking of the physical features of the county. Munros (peaks over 3000 feet) in the county include: Farther north rise the Buck of Cabrach, 722 m (2,369 ft) on the Banffshire border, Tap o' Noth , 558 m (1,831 ft), Bennachie , 518 m (1,699 ft), which from its central position is a landmark visible from many different parts of
1088-635: The Civil Wars . On 6 September 1715 John Erskine, Earl of Mar initiated the Jacobite rising of 1715 at Braemar in support of the claim of James Francis Edward Stuart to the throne. Stuart arrived in Scotland from his exile in France, landing at Peterhead on 22 December 1715. The rising was unsuccessful and by February 1716 Stuart was back in France. The collapse of the 1715 rising ruined many of
1156-518: The County of Aberdeen ( Scots : Coontie o Aiberdeen , Scottish Gaelic : Siorrachd Obar Dheathain ) is a historic county in Scotland . The county gives its name to the modern Aberdeenshire council area , which covers a larger area than the historic county. The historic county ceased to be used for local government purposes in 1975, but its boundaries are still used for certain functions, being
1224-608: The House of Commons of the Parliament of the United Kingdom and it elects one Member of Parliament (MP) by the first past the post system of election. It was first used in the 1885 general election , but has undergone various boundary changes since that date. The seat has been held by Kirsty Blackman of the Scottish National Party since 2015. At the 2019 general election, the constituency had
1292-507: The Local Government (Scotland) Act 1973 reorganised local government in Scotland into a two-tier system of regions and districts. The administrative counties of Aberdeenshire, the City of Aberdeen, Banffshire, Kincardineshire and most of Moray were merged to form Grampian Region , with the pre-1975 area of Aberdeenshire being divided between the districts of City of Aberdeen , Banff and Buchan , Gordon and Kincardine and Deeside . In 1996
1360-620: The River Gairn . The granites have been extensively quarried at Rubislaw , Peterhead and Kemnay . Serpentinite and troctolite , the precise age of which is uncertain, occur at the Black Dog Rock north of Aberdeen, at Belhelvie and near Oldmeldrum . Where the schists of sedimentary origin have been pierced by these igneous intrusions, they are charged with contact minerals such as sillimanite , cordierite , kyanite and andalusite . Cordierite-bearing rocks occur near Ellon, at
1428-548: The city (which was one of four counties of cities in Scotland) and entirely within the city. The new boundaries were first used in the 1918 general election , and Aberdeen North then consisted of the wards of Greyfriars, St Andrew, St Clement, St Machar, Torry and Woodside. The county of Aberdeen was covered by Aberdeen and Kincardine East , Central Aberdeenshire and Kincardine and West Aberdeenshire . Aberdeen and Kincardine East and Central Aberdeenshire were entirely within
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#17327801393281496-544: The county of Kincardine . The City of Aberdeen district became a district within the Grampian region . The enlarged district included areas covered by the constituencies of West Aberdeenshire and North Angus and Mearns . North Angus and Mearns had been created in 1950 to cover the county of Kincardine and part of the county of Angus . The 1979 general election was held before a review of constituency boundaries took account of new local government boundaries. In this period
1564-629: The Catholics to the influence of James Stewart, 1st Earl of Moray , who was regent during the reign of James VI , but was defeated and killed at the Battle of Corrichie on the Hill of Fare in 1562. As years passed it became apparent that Presbyterianism gained less support in Aberdeenshire than Episcopacy , of which system Aberdeenshire remained for generations the stronghold in Scotland. Another crisis in ecclesiastical affairs arose in 1638, when
1632-582: The Eastern Highlands. In the upper parts of the valleys of the Dee and the Don they form well-marked groups, of which the most characteristic are: These divisions are folded on highly inclined or 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 series. Excellent sections showing
1700-646: The English garrison in Aberdeen, but failed to capture the castle. In 1303 Edward again visited the county, halting at Kildrummy Castle , then in the possession of Robert the Bruce , who shortly afterwards became the acknowledged leader of the Scots and made Aberdeen his headquarters for several months. In 1308, he defeated John Comyn, Earl of Buchan , an opponent of his claim to the Scottish throne, at Inverurie . For
1768-457: The Isles , who was defeated at the Battle of Harlaw in 1411 by the Scottish army under Alexander Stewart, Earl of Mar . In the 15th century two further leading county families emerged: Sir Alexander Forbes becoming Lord Forbes about 1442, and Sir Alexander Seton , Lord Gordon in 1437 and Earl of Huntly in 1445. Bitter feuds raged between these families for a long period. The Gordons reached
1836-478: The Moreseat fossils were derived are not now found in place in that part of Scotland . 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 peat . The tops of the highest mountains have an Arctic flora. At
1904-671: The Picts to Christianity began with Teman in the 5th century, and continued with Columba , Machar (after whom St Machar's Cathedral in Aberdeen is named), and Drostan , who founded a monastery at Old Deer . The Vikings and Danes periodically raided the coast. Macbeth, King of Scotland , was killed at the Battle of Lumphanan in 1057. Aberdeen itself was made a royal burgh by David I (reigned 1124–1153). Its earliest surviving charter dates from 1179, by which date its burgesses had already combined with those of Banff , Elgin , Inverness and other trans-Grampian communities to form
1972-464: The Scottish crown is said to be from the Ythan. Loch Muick , the largest of the few lakes in the county, 399 m (1,309 ft) above the sea, 2 + 1 ⁄ 2 miles (4.0 km) long and 1 ⁄ 3 to 1 ⁄ 2 mile (540 to 800 m) broad, lies some 8 + 1 ⁄ 2 miles (13.7 km) southwest of Ballater . Loch Strathbeg , 6 miles (9.7 km) southeast of Fraserburgh,
2040-537: The Scottish local government system was reorganised again, this time into single-tier council areas . One of the council areas is called Aberdeenshire , covering the combined area of the pre-1996 districts of Banff and Buchan, Gordon, and Kincardine and Deeside. The council area therefore has significantly different boundaries to the pre-1975 county, also including most of the historic county of Kincardineshire and eastern parts of Banffshire (including its county town of Banff ), but excluding Aberdeen City. The boundaries of
2108-415: The area is still famed for cattle, more commonly continental breeds, with most slaughtered in Scotland, and in particular a good local abattoir capacity. Spring Barley is the predominant crop, and in lowland Winter Wheat, Oil Seed Rape & Potatoes would be more common than oats. There is also a significant area of carrots grown. With no slaughter capacity in Scotland the pig industry is diminishing but still
Aberdeen North - Misplaced Pages Continue
2176-531: The authorities ordered subscription to the National Covenant . The people of Aberdeenshire responded so grudgingly to this demand that James Graham, 1st Marquess of Montrose , visited the shire in the following year to enforce acceptance. The Cavaliers , not being disposed to yield, dispersed an armed gathering of Covenanters in the affair called the Trot of Turriff in 1639, one of the first skirmishes in
2244-489: The boundaries of Aberdeenshire. The city of Aberdeen, already independent for local government purposes, was subsequently also removed from Aberdeenshire for lieutenancy and other purposes in 1899, when the city was made a county of itself . Shortly after its creation, the county council built itself County Buildings in Union Terrace, Aberdeen, to serve as its headquarters, which was completed in 1896. In 1975
2312-494: The city became one of 32 unitary council areas of Scotland . Also, the name of the city became, officially, Aberdeen City . In this period the constituency was made up of the City of Aberdeen District electoral divisions of Balgownie, Brimmond, Danestone, Mastrick, Middleton, Northfield, Summerfield, and West Don, as provided for by the Parliamentary Constituencies (Scotland) Order 1995. Since 2005
2380-409: The city. The county of Aberdeen was now again divided between East Aberdeenshire and West Aberdeenshire , with both of these constituencies entirely within the county. The same boundaries were used for the 1951 general election . By the time of the 1955 general election , a boundary review had taken account of a small enlargement of the city area, and Aberdeen North was defined as consisting of
2448-530: The coast, as proved by the deposit of red clay north of Aberdeen. At a later date the local glaciers laid down materials on top of the red clay. The committee appointed by the British Association proved that the Greensand, which has yielded a large suite of Cretaceous fossils at Moreseat in the parish of Cruden , occurs in glacial drift, resting probably on granite. The strata from which
2516-460: The component strata occur in Glen Clunie and its tributary valleys above Braemar. Eastwards down the Dee and the Don and northwards across the plain of Buchan towards Rattray Head and Fraserburgh there is a development of biotite gneiss , partly of sedimentary and perhaps partly of igneous origin. A belt of slate which has been quarried for roofing purposes runs along the west border of
2584-495: The constituency is made up of the Aberdeen City Council wards of Auchmill, Berryden, Castlehill, Cummings Park, Donmouth, Hilton, Kittybrewster, Mastrick, Midstocket, Newhills, Pittodrie, St Machar, Seaton, Sheddocksley, Springhill, Stockethill, Summerhill, Sunnybank, and Woodside, as provided for by the Parliamentary Constituencies (Scotland) Order 2005. As redefined for the 1997 general election , Aberdeen North
2652-454: The constituency was made up of the City of Aberdeen District electoral divisions of Ashgrove, Brimmond, Kittybrewster, Mastrick, Northfield East, Northfield West, St Machar, Seaton, Summerfield, and Woodside. The 1983 general election , the 1987 general election and the 1992 general election took place during this period. In 1996, under the Local Government etc (Scotland) Act 1994 , local government regions and districts were abolished and
2720-679: The county from 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 epidiorite and hornblende gneiss in Glen Muick and Glen Callater , which have been permeated by granite and pegmatite in veins and lenticles , often foliated. The later granites subsequent to
2788-414: The county of Aberdeen. Kincardine and West Aberdeenshire covered the county of Kincardine minus the burgh of Inverbervie , which was covered by Montrose Burghs , and part of the county of Aberdeen. The same boundaries were used in the 1922 general election , the 1923 general election , the 1924 general election , the 1929 general election , the 1931 general election , the 1935 general election and
Aberdeen North - Misplaced Pages Continue
2856-739: The county, and which is celebrated in John Imlah 's song, O gin I war faur the Gadie rins, and Foudland, 466 m (1,529 ft). The chief rivers are the Dee , 90 miles (140 km) long; the Don, 82 miles (132 km); the Ythan , 37 miles (60 km), with mussel-beds at its mouth; the Ugie , 20 miles (32 km), and the Deveron, 62 miles (100 km), partly on the boundary of Banffshire. A pearl in
2924-475: The course of excavations in Aberdeen. The glacial deposits, especially in the belt bordering the coast between Aberdeen and Peterhead, furnish important evidence. The ice moved eastwards off the high ground at the head of the Dee and the Don, while the mass spreading outwards from the Moray Firth invaded the low plateau of Buchan ; but at a certain stage there was a marked defection northwards parallel with
2992-576: The fishery districts of Peterhead, Fraserburgh and Aberdeen, the last of which includes also three Kincardineshire ports. The herring season for Aberdeen , Peterhead and Fraserburgh lasts from June to September, at which time the ports become crowded with boats from other Scottish districts. Valuable salmon-fishings exist – rod, net and stake-net – on the Dee, Don, Ythan and Ugie. In 1911 the average annual despatch of salmon from Aberdeenshire comprises about 400 long tons (450 short tons ). Manufactures mainly cluster in or near Aberdeen , but throughout
3060-490: The foot of Bennachie, and on the top of the Buck of Cabrach. A banded and mottled calc-silicate hornfels occurring with the limestone at Derry Falls, west-northwest of Braemar, has yielded malacolite , wollastonite , brown idocrase , garnet , sphene and hornblende. A larger list of minerals has been obtained from an exposure of limestone and associated beds in Glen Gairn , about four miles (6 km) above
3128-450: The functions of the commissioners (which were eventually abolished in 1930). The burgh of Aberdeen was deemed capable of providing its own county-level local government functions, and so it was excluded from the administrative area of the county council, although the county council still chose to base itself in the city. The first meeting of Aberdeenshire County Council was held on 22 May 1890 at Aberdeen Town House , which as well as being
3196-521: The headquarters of Aberdeen Corporation also served as the county's main courthouse and meeting place of the commissioners of supply. Alexander Morison Gordon of Newton House in the parish of Culsalmond was the first convener of the council. The 1889 Act also led to a review of boundaries, with exclaves being transferred to a county they actually bordered, and parish and county boundaries being adjusted to eliminate cases where parishes straddled county boundaries. There were several such changes affecting
3264-520: The height of their power in the first half of the 16th century, when their domains, already vast, were enhanced by the acquisition, through marriage, of the Earldom of Sutherland in 1514. King's College, Aberdeen was founded in 1495, followed by Marischal College in 1593; the two colleges subsequently merged to become the University of Aberdeen in 1860. The Reformation of the 16th century
3332-433: The historic county (as it was prior to the removal of Aberdeen in 1899) are still used for some limited official purposes connected with land registration, being a registration county . The Aberdeenshire lieutenancy area covers the area of the pre-1975 county excluding the parts within the modern Aberdeen City council area. The historic Aberdeenshire is traditionally divided into five districts: The interior mountains of
3400-414: The intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Aberdeen_North&oldid=932501558 " Category : Disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages Aberdeen North (UK Parliament constituency) Aberdeen North is a burgh constituency of
3468-542: The lairds. In the subsequent Jacobite rising of 1745 there was much less support for the cause in the county, although the insurgents held Aberdeen for five months until February 1746. In 1852 Prince Albert , husband of Queen Victoria , bought the Balmoral Castle estate in the valley of the River Dee and subsequently rebuilt the castle there. Aberdeenshire's origins as a shire (the area administered by
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#17327801393283536-532: The largest SNP vote share and relative majority, effectively making it the safest SNP seat, although this majority was heavily reduced at the subsequent 2024 election. There was also an Aberdeen North constituency of the Scottish Parliament , created in 1999 with the boundaries of the Westminster seat of that time. This constituency was abolished in 2011, its area thereafter being covered by
3604-482: The new constituencies of Aberdeen Donside and Aberdeen Central . (See also Scottish Parliament constituencies and regions .) The seat covers much of the northern half of the Aberdeen Council Area. It includes affluent suburbs like Kingswells and Bridge of Don, alongside areas with significant social housing within the city proper such as; Tillydrone, Northfield, Mastrick and Bucksburn. Following
3672-414: The next most important industry to agriculture. Aberdeenshire fishing developed almost exclusively due to the introduction of steam trawlers. In 1911 the total value of the annual catch, of which between a half and a third consists of herrings, amounts to £1,000,000. In 1911 the industry produced both speldings (salted and rock-dried haddocks) and finnans (smoked haddocks). The ports and creeks belong to
3740-556: The northern boundary of the Aberdeen City council area. At that time, Aberdeen Central and Aberdeen South covered the rest of the Aberdeen City council area, and all three Aberdeen constituencies were entirely within the council area. *Pirie was endorsed by the Coalition Government but refused to give it his support. 57°10′34″N 2°08′06″W / 57.176°N 2.135°W / 57.176; -2.135 County of Aberdeen Aberdeenshire or
3808-425: The parish of New Machar and elsewhere. Duns or forts occur on hills at Dunecht , where the dun encloses an area of two acres (8,000 m ), Barra near Oldmeldrum , Tap o' Noth, Dunnideer near Insch and other places. There are numerous monoliths , standing stones and stone circles in the area, along with many examples of the sculptured stones of the early Christian epoch. Missionaries aiming to convert
3876-477: The plication of the schists have a wide 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. Though consisting mainly of biotite granite, these later intrusions pass by intermediate stages into diorite , as in the area between Balmoral and the head-waters of
3944-553: The point where that river joins the Dee. Narrow belts of Old Red Sandstone , resting unconformably on the old platform of slates and schists, have been traced from the north coast at Peterhead by Turriff to Fyvie , and also from Huntly by Gartly to Kildrummy Castle . The strata consist mainly of conglomerates and sandstones, which, at Gartly and at Rhynie , are associated with lenticular bands of andesite indicating contemporaneous volcanic action. Small outliers of conglomerate and sandstone of this age have recently been found in
4012-514: The royal lodge on Loch Muick , 411 m (1,348 ft) above the sea, grow larches, vegetables, currants, laurels, roses, etc. Some ash-trees, 1 to 1.5 m (4 or 5 ft) in girth, grow at 400 m (1,300 ft) above the sea. Trees, especially Scotch fir and larch, grow well, and Braemar has plentiful natural timber, said to surpass any in the north of Europe . Stumps of Scotch fir and oak found in peat sometimes far exceed any now growing in size. Moles occur at 550 m (1,800 ft) above
4080-623: The sea, and squirrels at 450 m (1,480 ft). Grouse, partridges and hares abound, and rabbits are often numerous. Red deer abound in Braemar, which in 1911 had the most extensive deer forest in Scotland . Except in the mountainous districts, Aberdeenshire has a comparatively mild climate, owing to the proximity of much of the shire to the sea. The mean annual temperature at Braemar reaches 6 °C (43 °F), and that at Aberdeen 8 °C (46 °F). The mean yearly rainfall varies from about 750 to 950 mm (30 to 37 in). In summer
4148-483: The sheriffs. In 1667 Commissioners of Supply were established for each shire, which would serve as the main administrative body for the area until the creation of county councils in 1890. Following the Acts of Union in 1707, the English term 'county' came to be used interchangeably with the older term 'shire'. Elected county councils were established in 1890 under the Local Government (Scotland) Act 1889 , taking most of
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#17327801393284216-580: The upper Dee and Don valleys provide the driest and most bracing climate in the British Isles , and grain grows cultivated up to 500 m (1,600 ft) above the sea, or 100 to 150 m (330 to 490 ft) higher than elsewhere in North Britain. Poor, gravelly, clayey and peaty soils prevail, but tile-draining, bones and guano, and the best methods of modern tillage, greatly increased the produce. Indeed, in 1911, no part of Scotland had
4284-456: The wards of Cairncry, St Andrews, St Clement's, St Machar, St Nicholas and Woodside. The same boundaries were used for the 1959 general election , the 1964 general election , the 1966 general election and the 1970 general election . For the February 1974 general election there was, again, no change to the boundaries of Aberdeen North, but a review had defined the constituency in terms of
4352-466: Was anciently occupied by the Picts , whom Ptolemy , writing c. 150 AD , called Taexali . There is some evidence of Roman activity in the area, notably with a camp at Normandykes near Peterculter . Weems or earth-houses were a common type of ancient dwelling in the west. Relics of crannogs or lake-dwellings exist at Loch Kinord and Bishops' Loch (historically called Loch Goul) in
4420-526: Was cattle-feeding. Aberdeenshire fattens a great number of the home-bred crosses for the London and local markets, and imports Irish animals on an extensive scale for the same purpose, while an exceedingly heavy trade in dead meat for London and the south occurs all over the county. Farmers also raise sheep , horses and pigs in large numbers. Since the encyclopedia article was published in 1911, there have been significant changes. Few Irish cattle now come in,
4488-519: Was created by the Redistribution of Seats Act 1885 and first used in the 1885 general election , so was Aberdeen South. Aberdeen North then consisted of the municipal wards of St Clement, St Andrew, St Machar and Greyfriars, and the 10th and 11th Parliamentary Polling Districts. The rest of the county of Aberdeen was covered by the county constituencies of Eastern Aberdeenshire and Western Aberdeenshire . The same boundaries were used in
4556-620: Was one of three constituencies covering and entirely within the Aberdeen City area, the other two being Aberdeen South and Aberdeen Central . Aberdeen South shared boundaries with both of the other two constituencies. As redefined by the Fifth Review of the Boundary Commission for Scotland , and subsequently first used in the 2005 general election , Aberdeen North is entirely within the Aberdeen City council area and one of five constituencies covering that council area and
4624-421: Was slow to reach Aberdeenshire. Churches were still being built and decorated in the old Catholic style in Aberdeenshire for some years after southern Scotland had started moving away from such styles. Opposition to the changes to Protestant forms of worship and church leadership saw rioting in Aberdeen, with St Machar's Cathedral being damaged. George Gordon, 4th Earl of Huntly offered some resistance on behalf of
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