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BUTE
, the most important, though not the largest, of the islands constituting the See also:county of the same name, in the See also:Firth of See also:Clyde, See also:Scotland, about 18 m
.
S.W. of See also:Greenock and 40 m., by See also:water, from See also:Glasgow
.
It is hounded on the N. and W. by the lovely Kyles of Bute, the narrow winding strait which separates it from See also:Argyllshire, on the E. by the Firth of Clyde, and on the S. and S.W. by the See also:Sound of Bute, about 6 m. wide, which divides it from See also:Arran
.
Its See also:area is about 49 sq. m., or31,161 acres
.
It lies in a N.W. to S.E. direction, and its greatest length from Buttock Point on the Kyles to Garroch See also:Head on the Firth of Clyde is 151 M
.
Owing to indentations its width varies from 1* m. to 41 M
.
There are piers at Kilchattan, Craigmore, See also:Port See also:Bannatyne and See also:Rothesay, but Rothesay is practically the See also:harbour for the whole See also:island
.
Here there is See also:regular communication by railway steamers from Craigendoran, See also:Prince's See also:Pier (Greenock), See also:Gourock and See also:Wemyss See also:Bay, and by frequent vessels from the Broomielaw See also:Bridge in Glasgow and other points on the Clyde
.
Pop
.
(1891) 11,735; (1901) 12,162
.
The See also:principal hills are in the See also:north, where the See also:chief are See also:Kames See also:
See also:Loch Fad, about 1 m
.
S. of Rothesay, 21 M. See also:long by a m. wide, was the source of the See also:power used in the Rothesay See also:cotton-See also:spinning See also: At Kilchattan a See also:superior See also:clay for bricks and tiles is found, and See also:grey See also:granite susceptible of high See also:polish . The island is divided geologically into two areas by a See also:fault See also:running from Rothesay Bay in a south-south-See also:west direction by Loch Fad to Scalpsie Bay, which, throughout its course, coincides with a well-marked depression . The See also:tract lying to the north-west of this dislocation is composed of the metamorphic rocks of the Eastern High-lands . The See also:Dunoon phyllites See also:form a narrow See also:belt about a mile and a See also:half broad See also:crossing the island between Kames Bay and Etterick Bay, while the area to the north is occupied by grits and See also:schists which may be the western prolongations of the Beinn Bheula See also:group . Near Rothesay and along the hill slopes west of Loch Fad there are parallel strips of grits and phyllites . That See also:part of the island lying to the See also:east of this dislocation consists chiefly of Upper Old Red Sandstone strata, dipping generally in a See also:westerly or south-westerly direction . At the extreme south end, between Kilchattan and Garroch Head, these conglomerates and sandstones are overlaid by a thick cornstone or dolomitic See also:limestone marking the upper limit of the formation, which is surmounted by the See also:cement-stones and contemporaneous lavas of See also:Lower Carboniferous See also:age . The bedded volcanic rocks which form a See also:series of ridges trending north-west comprise porphyritic basalts, See also:andesite, and, near Port Luchdach, brownish See also:trachyte . Near the See also:base of the volcanic series intrusive igneous rocks of Carboniferous age appear in the form of sills and bosses, as, for instance,the See also:oval See also:mass of See also:olivine-See also:basalt on Suidhe Hill . Remnants of raised beaches are conspicuous in Bute . One of the well-known localities for See also:arctic shelly See also:clays occurs at Kilchattan See also:brick-See also:works, where the dark red clay rests on tough See also:boulder-clay and may be regarded as of See also:late glacial age . As to the origin of the name of Bute, there is some doubt .
It has been held to come from both (Irish for " a See also:cell "), in allusion to the cell which St See also:Brendan erected in the island in the 6th See also:century; others contend that it is derived from the See also:British words ey budh (Gaelic, ey bhiod), " the island of See also:corn " (i.e. See also:food), in reference to its fertility, notable in contrast with the barrenness of the Western Isles and See also:Highlands
.
Bute was probably first colonized by the vanguard of Scots who came over from See also:Ireland, and at intervals the Norsemen also secured a footing for longer or shorter periods
.
In those days the Butemen were also called Brandanes, after the See also:Saint
.
Attesting the antiquity of the island, " Druidical " monuments, barrows, See also:cairns and cists are numerous, as well as the remains of See also:ancient chapels
.
In virtue of a See also:charter granted by See also:
Off the western shore of Bute, ; m. from St See also:Ninian's Point, lies the island of Inchmarnock, 2 M. in length and about t m. in width
.
See J
.
See also:
Buteshire and See also:Renfrewshire form one sheriffdom, with a See also:sheriff-substitute See also:resident in Rothesay who also sits periodically at Brodick and Millport
.
The See also:circuit courts are held at Inveraray
.
The county is under school-See also:board See also:jurisdiction, and there is a secondary school at Rothesay
.
The county See also:council subsidizes technical See also:education in See also:agriculture at Glasgow and See also:Kilmarnock
.
The See also:staple crops are oats and potatoes, and See also:cattle, See also:sheep and horses are reared
.
See also:Seed-growing is an extensive See also:industry, and the fisheries are considerable
.
The Rothesay See also:fishery See also:district includes all the creeks in Buteshire and a few in See also:Argyll and See also:Dumbarton shires, the See also:Cumbraes being grouped with the Greenock district
.
The See also:herring fishery begins in See also:June, and See also: |
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