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Llandudno and District Field…

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Llandudno and District Field Club. EXCURSION TO THE BLACK ROCKS, DEGANWY. The first excursion of the above Club took place on Saturday last, under the guidance of Mr. W. Bezant Lowe, M.A., of Llanfairfechan, who is at present acting as hon. excursion secretary, in the place of Mr. W.R. Brookes, who has had to re- sign that office owing to pressure of busi- ness. Members from Colwyn Bay and Llandudno met at Deganwy station at 2.20 p.m., and proceeded along the pro- menade to the shore. As soon as the sands were reached, Mr. Lowe directed the at- tention of the party to the present course of the Conway, which could be well seen as it was low water, and pointed out how this course had been altered by the build- ing of the railway embankment and of the tubular and suspension bridges. Before this time the river flowed nearer the Denbighshire side, and the width of the, ferry in those days must have been much greater, as the old Ferry House was situated where the new signal box of the L. and N.W. Railway is now situated to the west of the present Llandudno junc- tion. Close by was the famous Ferry Hotel, near which some coins were dug up, and the Ferry itself is rendered notable for one or two terrible accidents, one about 1805, when the boat was upset and all the occupants, except two, were drowned. About 1650 there was another accident in which only one person was saved, a young woman, who was going to Llanfairfechan to meet her sweetheart, who also was thrown out of a convey- ance on the terrible round round Pen- maenmawr. He also escaped, and they both lived to a great age, the wife to the age of 116. They are now buried in Llan- fairfechan Churchyard. Proceeding the Black Rocks were soon reached and carefully examined. As is well-known the cliff here consists of a mass of boulder clay, full of stones, of all sizes and of every kind, very many show- ing striations, the result of glacial action. They are most varied in character, in- cluding grit from Denbighshire, sand- stone from Cheshire, igneous rocks from Snowdonia, and granite from Cumber- land, thus giving an indication of their origin. They were left there by that great ice-sheet which came from the north of Scotland, crossed the Isle of Man and the Lake district, and thence proceeding by the coast of Lancashire, reached the neighbourhood of Cheshire, where it div- ided, one portion coming along the north coast of Wales, crossing the Great and Little Orme's Heads and leaving its traces in the rounded character of these head- lands, and the mass of clay and stones which is to be found near Llanddulas, to the back of Colwyn Bay and then from the Black Rocks of Deganwy to the neigh- bourhood of Gogarth Abbey. The party then proceeded to the Go- garth Abbey Hotel, where an excellent tea was provided by Mr. Dutton, and a discussion took place afterwards. We are pleased to see from the excur- sion programme that several walks have been arranged at an interval of a fort- night, including a visit to the Little Orme to study marine life, Conway Castle and its architectural history, and the famous Eisteddfod stone at Bryn Eisteddfod. We feel sure that it is only necessary to mention this to induce numbers to join this Club, which is doing good work in the archaeology and natural history of the district. The hon. sec. is Mr. L. S. Underwood, of Bodnod, Lloyd-street, who will give full information regarding the Club. The next excursion will take place on Saturday, February 5th, when the mem- bers will, under the guidance of Mr. Harry Thomas, examine the marine life on the shore near the Little Orme. The members will meet at 2-30 p.m. at the tram stopping station at Nantygamar- road, near Bethania Chapel.

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Political Meetings at Penmachno.

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