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tween Lechlade and Cricklade, and nearer to the latter. But a river has a second topographical and historic function. It cannot only be considered longitudinally as a highway, it can also be considered in relation to transverse forces and regarded as an obstacle, a defence, and a boundary. This function has, of course, been of the highest importance in the history of all great rivers, not perhaps so much so in the case of the Thames as in the case of swifter or deeper streams, but, still, more than has been the case with so considerable and so rapid a river as the Po in Lombardy or the uncertain but dangerous Loire in its passage through the centre of France. For the Thames Valley was that which divided the vague Mercian land from which we get our weights, our measures, and the worst of our national accent, and cut it off from that belt of the south country which was the head and the heart of England until the last industrial revolution of our history. The Thames also has entered to a large, though hardly to a determining, extent into the military history of the country; to an extent which is greater in earlier than in later times, because with every new bridge the military obstacle afforded by the stream diminished. And finally, the Thames, regarded as an obstacle, was the cause that London Bridge concentrated upon itself so much of the life of the nation, and that the town which that bridge served, always the largest commercial city, became at last the capital of the island. We have already said that the establishment of the site of London Bridge was a capital point in the history of the river and the principal line of division in its course. What were the topographical conditions which caused the river to be crossed at this point rather than at another? It is always of the greatest moment to men to find some crossing for a great river as low down as may be towards the mouth. For the higher the bridge the longer the detour between, at the least, _two_ provinces of the country which the river traverses. It is especially important to find such a crossing as low down as possible when the river is tidal and when it is flanked upon either side by great flooded marshes, as was and is the Thames. For under such conditions it is difficult, especially in primitive times, to cross habitually from one side to the other in boats. Now it is a universal rule of early topography, and one which can be proved upon twenty
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