As to the age of these quarries, it is not easy to form a sound opinion. They have been supposed to be British, and various uses have been found for them, quite at variance with the appearances they present. The only argument for such an origin has been overlooked. The town is in Woking hundred, and Woking, like Wokey in Mendip, may be a corruption of the British “Ogof” (fovea), a cave. But Woking was never the name of the town, and the material evidence of the caverns does not favour this theory. They are certainly not British: the plan of the workings excludes this view. No doubt they might be Roman, but there are no traces of Roman buildings in the neighbourhood, and chalk, even hard chalk, is too plentiful all along the ridge to be carried hence to any great distance. The most probable supposition seems to me to be that they were opened by the builders of the Norman castle, who used chalk largely for their inner, and, indeed, for much of their more exposed, work. The quarries have no communication with any part of the castle. Where they infringe upon its borders, they are far too deep to have been employed against it during a mediæval siege. HARLECH CASTLE, MERIONETH. DESCRIPTION. The Castle of Harlech occupies a bold and rugged headland of rock which juts forward upon the coast-line of Merioneth over the broad alluvial plain known as Morfa Harlech, near to its southern and narrower extremity. Six centuries back, when the Traeth was an estuary, and the waves may have washed the foot of the rock, Harlech, as now Criccaieth, was probably accessible by water,—a circumstance likely to have governed its founder in his selection of the site. Although scarcely 200 feet above the sea level, and connected with a much higher background, the rock of Harlech is nevertheless a very striking object, and by the extreme boldness of its outline and its almost isolated position does justice to its very significant appellation. It commands one of the most remarkable prospects in Britain. Before it is the Bay of Caernarvon with its vast sweep of sandy shore, contained on the right by Snowdon and its subordinate peaks; whence the high land, after rising into the elevations of Carn Madryn, Carn Bodfuan, and Yr Eifl, gradually subsides into the Bay of Aberdaron and the Sound and Isle of Bardsey. Caernarvon and Conway are fortresses more ornate in character and of larger area; but they are not equal to Harlech in natural strength and in grandeur of position; nor is, in these respects, Beaumaris itself, though placed in the very eye of the Snowdon group, by any means its superior.