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My life : a record of events and opinions - Wallace-online.org

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136 MY LIFEthe valley beyond, thesmoke from which gives thehill much the appearance <strong>of</strong> an active volcano. Tothe south-west the view extends down the valley toSwansea Bay, while to the north-east stretches theVale <strong>of</strong> Neath itself, nearly straight for twelve miles,the river winding in a level fertile valley about aquarter to half a mile wide, bounded on each side byabrupt hills, whose lower slopes are finely wooded,<strong>and</strong> backed by mountains from fifteen hundred toeighteen hundred feet high. The view up this valleyis delightful, its sides being varied with a few housespeeping out from the woods, abundance <strong>of</strong> lateralvalleys <strong>and</strong> ravines, with here <strong>and</strong> there the glint <strong>of</strong>falling water, while its generally straight directionaffords fine perspective effects, sometimes fading inthe distance into a warm yellow haze, at othersaffording a view <strong>of</strong> the distant mountain rangesbeyond.At twelve miles from the town we come to thelittle village <strong>of</strong> Pont-nedd-fychan (the bridge <strong>of</strong> thelittle Neath river), where we enter upon a quitedistinct type <strong>of</strong> scenery, dependent on our passingout <strong>of</strong> the South Wales coal basin, crossing the hardrock-belt <strong>of</strong> the millstone grit, succeeded by thepicturesque crags <strong>of</strong> the mountain limestone, <strong>and</strong>then entering on the extensive formation <strong>of</strong> the OldRed S<strong>and</strong>stone.Within a mile <strong>of</strong> Pont-nedd-fychan is the Dinasrock, a tongue <strong>of</strong> mountain limestone jutting outacross the millstone grit, <strong>and</strong> forming fine precipices,one <strong>of</strong> which was called the Bwa-maen or bow rock,from its being apparently bent double. Lower downthere are also some curious waving lines <strong>of</strong> apparentstratification, but on a recent examination I aminclined to think that these are really glacial

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