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sailing in from Cowes, proud, beautiful shapes, their polished brass-work glinting in the sunlight, while farther out in the Channel a great ocean liner steams steadily towards the Solent, altering her course repeatedly as she nears the Needles. And yet, with all her desirable qualities and attractive features, Bournemouth is not to everyone's taste, particularly those whose holidays are incomplete without mediaeval ruins on their doorsteps. The town, however, is somewhat fortunate even in this respect, since, although she has no antiquities of her own, she is placed close to Wimborne and Poole on the one hand, and to Christchurch, with its ancient Priory, on the other. Poole itself is not an ideal place to live in, while Wimborne and Christchurch are out-of-the-way spots, interesting enough to the antiquary, but dull, old-fashioned towns for holiday makers. The clean, firm sands of Bournemouth are excellent for walking on, and make it possible for the pedestrian to tramp, with favourable tides, the whole of the fourteen miles of shore that separate Poole Harbour from Christchurch. By a coast ramble of this kind the bold and varied forms of the cliffs, and the coves cutting into them, give an endless variety to the scene; while many a pretty peep may be obtained where the Chines open out to the land, or where the warmly-coloured cliffs glow in the sunlight between the deep blue of the sea and the sombre tints of the heather lands and the pine-clad moor beyond. The clays and sandy beds of these cliffs are remarkable for the richness of their fossil flora. From the white, grey, and brownish clays between Poole Harbour and Bournemouth, no fewer than nineteen species of ferns have been determined. The west side of Bournemouth is rich in Polypodiaceae, and the east side in Eucalypti and Araucaria. These, together with other and sub-tropical forms, demonstrate the existence of a once luxuriant forest that extended to the Isle of Wight, where, in the cliffs bounding Alum Bay, are contemporaneous beds. The Bournemouth clay beds belong to the Middle Eocene period. Westwards from the Pier the cliffs are imposing, on one of the highest points near the town being the Lookout. A hundred yards or so farther on is Little Durley Chine, beyond which is a considerable ravine known as Great Durley Chine, approached from the shore by Durley Cove. The larger combe consists of slopes of sand and gravel, with soft sand hummocks at the b
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