Ross (Ros in Scottish Gaelic) is a region of Scotland and a former mormaerdom, earldom, sheriffdom and county. The name Ross allegedly derives from a Gaelic word meaning a headland - perhaps a reference to the Black Isle. The Norse word for Orkney - Hrossay meaning horse island - is another possible origin. The area once belonged to the Norse earldom of Orkney. Ross is a historical comital region, perhaps predating the Mormaerdom of Ross.
It may be doubted whether the Romans ever effected even a temporary settlement in the area of the modern county. In Roman times, and for long afterwards, the land was occupied by Gaelic Picts, who, in the 6th and 7th centuries, were converted to Christianity by followers of Saint Columba. Throughout the next three centuries the natives were continually harassed by Norse raiders, of whose presence tokens have survived in several place-names (Dingwall, Tain, and others). At this time the country formed part of the great province of Moray (Latin: Moravia), which then extended as far west as the Dornoch Firth and the Oykel, and practically comprised the whole of Ross and Cromary.
William, the 4th Earl of Ross, was present with his clan at the Battle of Bannockburn (1314), and almost a century later (1412) the castle of Dingwall, the chief seat on the mainland of Donald, Lord of the Isles, was captured after the disastrous fight at Harlaw in Aberdeenshire, which Donald had provoked when his claim to the earldom was rejected. The earldom reverted to the crown in 1424, but James I soon afterwards restored it to the heiress of the line, the mother of Alexander Macdonald, 3rd Lord of the Isles, who thus became the 11th Earl. In consequence, however, of the treason of John Macdonald, 4th and last Lord of the Isles and 12th Earl of Ross, the earldom was again vested in the crown (1476). Five years later James III bestowed it on his second son, James Stewart, whom he also created Duke of Ross in 1488.
By the 16th century the whole area of the county was occupied by different clans. The Rosses held what is now Easter Ross; the Munros the small tract around Ben Wyvis, including Dingwall; the Macleods Lewis, and, in the mainland, the district between Loch Maree and Loch Torridon; the Macdonalds of Glengarry, Coigach, and the district between Strome Ferry and Kyle of Lochalsh, and the Mackenzies the remainder.
The county of Ross was constituted in 1661, and Cromarty in 1685 and 1698, both being consolidated into the present county in 1889.
Apart from occasional conflicts between rival clans, the only battles in the county were Invercarron, at the head of Dornoch Firth, when Montrose was crushed by Colonel Archibald Strachan on 27 April 1650—and the Battle of Glenshiel, when the Jacobites, under the Earl of Seaforth, aided by Spaniards, were defeated by a force under the command of General Joseph Wightman on 10 June 1719.
Ross lies south of Sutherland and the Dornoch Firth, west of the North Sea and the Moray Firth, north of the Beauly Firth and Inverness-shire and east of The Minch. There are also a number of small islands off the area's west coast, among which are:
The area of the mainland comprises .
On the North Sea (eastern side) of the area the major firths are the Beauly Firth and the (Inner) Moray Firth, which mark off the Black Isle from Inverness-shire, the Cromarty Firth, which bounds the districts of Easter Ross and the Black Isle, the Moray Firth, separating Easter Ross from Nairnshire, and the Dornoch Firth, dividing north-east Ross from Sutherland.
On the Atlantic (western) coastline—which has a length of nearly —the principal sea lochs and bays, from south to north, include Loch Duich, Loch Alsh, Loch Carron, Loch Kishorn, Loch Torridon, Loch Shieldaig, Upper Loch Torridon, Gair Loch, Loch Ewe, Gruinard Bay, Loch Broom and Enard Bay.
The chief capes include Tarbat Ness on the east coast, and Coigach, Greenstone Point, Rubha Reidh, Redpoint and Hamha Point on the west.
Almost all the southern boundary with Inverness-shire consists of a rampart of peaks, many of them Munros: An Riabhachan (), Sgurr na Lapaich (), Carn Eige (Càrn Eighe) (), Mam Sodhail (Mam Soul) (), Beinn Fhada (Ben Attow) (), Sgurr Fhuaran (), The Saddle ().
To the north of Glen Torridon are the masses of Liathach (), Beinn Eighe (), Beinn Alligin () and Beinn Dearg (). On the northeastern shore of Loch Maree rises Slioch (), while the Fannich group contains six Munros, the highest being Sgurr Mor (). The immense isolated bulk of Ben Wyvis (), forms the most noteworthy feature in the north-east, and An Teallach () in the north-west appears equally conspicuous, though less solitary. Only a small fraction of the west and south of the area is under in height. Easter Ross and the peninsula of the Black Isle are comparatively level.
The longest stream of the mainland portion of Ross and Cromarty is the River Orrin, which rises from the slopes of An Sidhean () and pursues a north-easterly course to its confluence with the River Conon after a run of about , during a small part of which it forms the boundary with Inverness-shire. At Aultgowrie the stream rushes through a narrow gorge where the drop is considerable enough to make the Falls of Orrin. The River Blackwater flows from mountains in Strathvaich southeast for until it joins the Conon, forming soon after it leaves Loch Garve the small but picturesque Falls of Rogie. Within a short distance of its exit from Loch Luichart the Conon pours over a series of graceful cascades and rapids and then pursues a winding course of , mainly eastward to the head of the Cromarty Firth. Situated above Glen Elchaig in the southwest of the region are the Falls of Glomach. The stream giving rise to them drains a series of small lochs on the northern flanks of Beinn Fhada (Ben Attow) and, in an almost unbroken sheet over a metre in width, effects a sheer drop of 110 m, and soon afterwards ends its course in Glen Elchaig. The falls are usually visited from Invershiel 11 km to the south-west. 12 miles south-east of Ullapool, on the estate of Braemore, are the Falls of Measach, formed by the Droma, a headstream of the River Broom. The cascades, three in number, are close to Corrieshalloch Gorge. The River Oykel, throughout its course, forms the boundary with Sutherland. There are many freshwater lochs, the largest being Loch Maree. In the far north-west, above the sea, lies Loch Sionascaig, a loch of such irregularity of outline that it has a shore-line of . It contains several wooded islands, and drains into Enard Bay by the River Polly. Lochan Fada (the long loch), above the sea, is in length, and covers an area of , and is deep, with a mean depth of . Once drained by the Muice (Allt na Muice), it has been tapped a little farther west by the Abhainn na Fhasaigh, which has lowered the level of the loch. Other lochs are Fionn Loch (the white or clear lake), long by wide, famous for its herons, Loch Luichart towards the centre of the area (8 miles long and between wide), fringed with birches and having the shape of a crescent, the mountain-girt Loch Fannich (1 mile wide); and the wild narrow Lochs Monar ( long) and Mullardoch ( long), on the Inverness-shire boundary.
Of the straths or valleys the more important run from the centre eastwards, such as Strathconon, Strathbran, Strathgarve, Strathpeffer and Strathcarron. Excepting Glen Orrin, in the east central district, the longer glens lie in the south and towards the west. In the extreme south Glen Shiel runs between five mountains (The Five Sisters of Kintail to its mouth on Loch Duich. The A87 passes down the glen. Further north lie Glen Elchaig, Glen Carron, and Glen Torridon. The railway from Dingwall runs through Glen Carron to Kyle of Lochalsh.
Within the Torridonian tract the older Lewisian gneiss occupies large areas north of Coigach, on the east of Enard Bay, between Gruinard Bay and Loch Maree. Between the last named and Gairloch, on both sides of middle Loch Torridon and at many other spots smaller patches appear. The Lewisian gneiss is everywhere penetrated by basic dikes, generally with a northwest-southeast direction; some of these are of great breadth. The Torridonian rocks are succeeded unconformably by a series of Cambrian strata confined to a variable but narrow belt west of the line of main thrusting. This belt of Cambrian rocks has suffered an enormous amount of subordinate thrusting. It is composed of the following subdivisions in ascending order: falsebedded quartzite, Pipe Rock quartzite, fucoid beds and Olenellus band, serpulite grit, Durness dolomite and marble, Durness dolomite and limestone: but these are not always visible at any one spot. So great has been the disturbance in the region of thrusting that in some places, as in the neighborhood of Loch Kishorn and elsewhere, the rocks have been completely overturned and the ancient gneiss has been piled upon the Torridonian.
On the shore of Moray Firth at Rathie a small patch of Kimeridge shale occurs, and beneath the cliffs of Shandwick there is a little Lower Oolite with a thin seam of coal. Glacial striae are found upon the mountains up to heights of , and much boulder clay is found in the valleys and spread over large areas in the eastern districts. Raised beaches occur at up to or so above the present sea-level; they are well seen in Loch Carron.
The most fertile tracts lie on the eastern coast, especially in Easter Ross and the Black Isle, where the soil varies from a light sandy gravel to a rich deep loam. As of 1911, among grain crops oats were most generally cultivated, but barley and wheat were also raised. Turnips and potatoes were the chief green crops. The higher grounds contain much good pasturage, with heavy flocks of sheep, blackfaced being the principal breed. Most of the horses, principally half-breds between the old garrons (hardy, serviceable, small animals) and Clydesdales, were maintained for the purposes of agriculture. The herds of cattle, mainly native Highland or crosses, were large, many of them supplying the London market. Pigs were reared, though in smaller numbers than formerly, most generally by the crofters.
Owing partly to the overcrowding of the Isle of Lewis and partly to the unkindly nature of the bulk of the surface—which offered no opportunity for other than patchwork tillage—the number of smallholdings was enormous. Sutherland, alone among Scottish counties, shows an even larger proportion of holdings under , while the average size of all the holdings throughout the county did not exceed .
As of 1911 about were devoted to deer forests, a greater area than in any other county in Scotland, among the largest being Achnashellach with ), Fannich with , Kinlochluichart with , Braemore with , Inchbae with and Dundonnell with . At one time the area under wood must have been remarkable, if we accept the common derivation of the word "Ross" as from the Old Irish ros, a wood, and there was until recent times a considerable extent of native woodland, principally pine, oak, ash and alder.
The fauna was noteworthy. Red and roe deer abounded, and foxes and alpine hares were common, while badgers and wild cats were occasionally trapped. Winged game was plentiful, and amongst birds of prey the golden eagle and osprey occurred. Waterfowl of all kinds frequented the sea lochs. Many rivers and lochs were rich in salmon and trout, and the pearl mussel was found in the bed of the Conon.
The Glen Ord and Glenmorangie distilleries are prominent whisky distilleries.
A railway, the Far North Line from Inverness, enters the county to the north of Beauly and runs northwards to Dingwall. From there the Far North Line continues north/northeast through Sutherland to Thurso and Wick in Caithness, and the Kyle of Lochalsh Line runs west/southwest to the Kyle of Lochalsh.
Among old castles are those of Lochslin, in the parish of Fearn, said to date from the 13th century, which, though ruinous, possesses two square towers in good preservation; Balone, in the parish of Tarbat, once a stronghold of the Earls of Ross; the remains of Dingwall Castle, their original seat; and Eilean Donan in Loch Alsh, which was blown up by English warships during the abortive Jacobite rising in 1719.
The local government county was created under the Local Government (Scotland) Act 1889, which also established elected county councils for all counties in Scotland. The county of Ross and Cromarty was nominally a merger of two older administrative counties, Ross-shire and Cromartyshire, but there were some alterations to boundaries. The alterations became fully effective, for all purposes except parliamentary representation, in 1892.
The county included six burghs: Cromarty, Dingwall, Fortrose, Invergordon, Stornoway and Tain. Dingwall was the county town.
When counties and burghs were abolished as local government areas, in 1975, under the Local Government (Scotland) Act 1973, the area of the county was divided between two new areas, the Highland region and the Western Isles, and the Ross and Cromarty district of the region was created as one of eight districts of the new region.
Stornoway and the district of Lewis merged into the Western Isles. Also, the new Ross and Cromarty district excluded two other areas, which merged into other districts of the region. The electoral division of Kincardine was merged into Sutherland, and the South West electoral division (an area around and including Lochalsh) was merged into Skye and Lochalsh.
In 1996, under the Local Government etc (Scotland) Act 1994, the district was abolished and the Highland region was turned into a unitary council area. The new unitary authority, the Highland Council, then adopted the area of the former district as a council management area, and created area committees to represent it. The management area consisted then of 13 wards, each electing one councillor by the first past the post system of election. The council as a whole had 72 members.
Ward boundaries were altered in 1999, to create 80 new wards, but management area boundaries were unaltered. Therefore area committees ceased to represent exactly the areas for which they were named and made decisions. 18 wards and, therefore, 18 councillors were related to the Ross and Cromarty management area.
Under the Local Governance (Scotland) Act 2004, ward boundaries changed again this year, 2007. Also, the eight management areas were abolished in favour of three new corporate management areas. The Ross and Cromarty area was divided between the Caithness, Sutherland and Easter Ross area and the Ross, Skye and Lochaber area.
This text is licensed under the Creative Commons CC-BY-SA License. This text was originally published on Wikipedia and was developed by the Wikipedia community.
The World News (WN) Network, has created this privacy statement in order to demonstrate our firm commitment to user privacy. The following discloses our information gathering and dissemination practices for wn.com, as well as e-mail newsletters.
We do not collect personally identifiable information about you, except when you provide it to us. For example, if you submit an inquiry to us or sign up for our newsletter, you may be asked to provide certain information such as your contact details (name, e-mail address, mailing address, etc.).
When you submit your personally identifiable information through wn.com, you are giving your consent to the collection, use and disclosure of your personal information as set forth in this Privacy Policy. If you would prefer that we not collect any personally identifiable information from you, please do not provide us with any such information. We will not sell or rent your personally identifiable information to third parties without your consent, except as otherwise disclosed in this Privacy Policy.
Except as otherwise disclosed in this Privacy Policy, we will use the information you provide us only for the purpose of responding to your inquiry or in connection with the service for which you provided such information. We may forward your contact information and inquiry to our affiliates and other divisions of our company that we feel can best address your inquiry or provide you with the requested service. We may also use the information you provide in aggregate form for internal business purposes, such as generating statistics and developing marketing plans. We may share or transfer such non-personally identifiable information with or to our affiliates, licensees, agents and partners.
We may retain other companies and individuals to perform functions on our behalf. Such third parties may be provided with access to personally identifiable information needed to perform their functions, but may not use such information for any other purpose.
In addition, we may disclose any information, including personally identifiable information, we deem necessary, in our sole discretion, to comply with any applicable law, regulation, legal proceeding or governmental request.
We do not want you to receive unwanted e-mail from us. We try to make it easy to opt-out of any service you have asked to receive. If you sign-up to our e-mail newsletters we do not sell, exchange or give your e-mail address to a third party.
E-mail addresses are collected via the wn.com web site. Users have to physically opt-in to receive the wn.com newsletter and a verification e-mail is sent. wn.com is clearly and conspicuously named at the point of
collection.If you no longer wish to receive our newsletter and promotional communications, you may opt-out of receiving them by following the instructions included in each newsletter or communication or by e-mailing us at michaelw(at)wn.com
The security of your personal information is important to us. We follow generally accepted industry standards to protect the personal information submitted to us, both during registration and once we receive it. No method of transmission over the Internet, or method of electronic storage, is 100 percent secure, however. Therefore, though we strive to use commercially acceptable means to protect your personal information, we cannot guarantee its absolute security.
If we decide to change our e-mail practices, we will post those changes to this privacy statement, the homepage, and other places we think appropriate so that you are aware of what information we collect, how we use it, and under what circumstances, if any, we disclose it.
If we make material changes to our e-mail practices, we will notify you here, by e-mail, and by means of a notice on our home page.
The advertising banners and other forms of advertising appearing on this Web site are sometimes delivered to you, on our behalf, by a third party. In the course of serving advertisements to this site, the third party may place or recognize a unique cookie on your browser. For more information on cookies, you can visit www.cookiecentral.com.
As we continue to develop our business, we might sell certain aspects of our entities or assets. In such transactions, user information, including personally identifiable information, generally is one of the transferred business assets, and by submitting your personal information on Wn.com you agree that your data may be transferred to such parties in these circumstances.