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Ward & Lock's descriptive and pictorial guide to the Isle of Man ...

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130 Guide <strong>to</strong> <strong>the</strong> <strong>Isle</strong> <strong>of</strong> <strong>Man</strong>.in aome parts eighteen feet thick. Here, according <strong>to</strong> localhie<strong>to</strong>ry, was a strong military position, which <strong>the</strong> <strong>Man</strong>xmenfound <strong>to</strong> bo valuable in <strong>the</strong> disturbed times wheninvasion <strong>and</strong> piracy were fashionable recreations, <strong>and</strong> <strong>the</strong>Irish were ra<strong>the</strong>r troublesome nciglibours. The fort didnot, however, always afford protection, for we find it recordedthat in May, 131G, one Richard M<strong>and</strong>eville <strong>and</strong> astrong following <strong>of</strong> Irish adventurers invaded <strong>the</strong> isl<strong>and</strong> <strong>and</strong>dem<strong>and</strong>ed supplies <strong>of</strong> provisions, cattle, <strong>and</strong> money. Thesebeing relused, <strong>the</strong> freebooters made a raid in<strong>to</strong> <strong>the</strong> interior,<strong>the</strong> <strong>Man</strong>xmen retreating <strong>to</strong> this stronghold, from which<strong>the</strong>y <strong>of</strong>fered a front <strong>of</strong> resistance. The Irish attacked withsuch fury that <strong>the</strong> <strong>Man</strong>xmen fled in confusion, <strong>and</strong> <strong>the</strong>pirates enjoyed what <strong>the</strong> Americans call "a good time,"roaming through <strong>the</strong> country, <strong>and</strong> plundering it <strong>of</strong> everythingon which <strong>the</strong>y could lay <strong>the</strong>ir h<strong>and</strong>s. The abbey <strong>of</strong>Rushen was robbed <strong>of</strong> its treasures, <strong>and</strong> <strong>the</strong> flocks <strong>and</strong> herds<strong>of</strong> <strong>the</strong> good monks were carried away. " After spending amonth in this pleasant manner, at <strong>the</strong>ir leisure digging upmuch silver, which had been buried in various places, <strong>the</strong>yfilled <strong>the</strong>ir vessels with <strong>the</strong>ir spoil <strong>and</strong> returned safe home."Geologists will scarcely fail <strong>to</strong> notice that on <strong>the</strong> nor<strong>the</strong>asternside <strong>of</strong> <strong>the</strong> mountain is an immense mass <strong>of</strong> granite,locally known as Granite Mount. There is nothing uncommonin that ; but when it is found that blocks <strong>of</strong> this granite havesomehow been deposited on <strong>the</strong> <strong>to</strong>p <strong>of</strong> South Barrule, atleast eight hundred feet above <strong>the</strong> mass <strong>of</strong> <strong>the</strong> gi-anite formation,<strong>and</strong> that boulders <strong>of</strong> <strong>the</strong> same rock <strong>and</strong> <strong>of</strong> granite maybe traced continuously for about two miles along <strong>the</strong> ridge<strong>of</strong> what is locally known as <strong>the</strong> Round Table, <strong>to</strong> <strong>the</strong> <strong>to</strong>p <strong>of</strong>Cronk-na-Irey-Lhaa, geologists may be justified in exercisinga little curiosity. These gentle men do not, as a rule,believe in fairy <strong>and</strong> o<strong>the</strong>r legends, however poetical ; so, ifwe were <strong>to</strong> tell our scientific friends that in old times twothree-legged <strong>Man</strong>x giants quarrelled, <strong>and</strong> threw s<strong>to</strong>nes ateach o<strong>the</strong>r, or had a hurling match with granite boulders,our explanation would probably be received in a mannernot complimentary <strong>to</strong> our veracity, <strong>and</strong> a more satisfac<strong>to</strong>rysolution would be sought for. The late Mr. CharlesDarwin was <strong>of</strong> opinion that <strong>the</strong> whole isl<strong>and</strong> sank down in<strong>the</strong> sea in <strong>the</strong> Glacial period, <strong>and</strong> that blocks <strong>of</strong> granite,frozen in<strong>to</strong> ice-floes, were deposited at different heights, <strong>and</strong>when <strong>the</strong> l<strong>and</strong> re-emerged, <strong>of</strong> course <strong>the</strong> granite blocks <strong>and</strong>boulders emerged with it. In connexion with this subjectwe may quote a sentence from <strong>the</strong> Rev. J. Gumming, who

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