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ude amid the stormy waters of the Firth of Forth, the Bass Rock, once a scene of fiery confusion, of roaring waves and heaving earthquakes, has formed alternately the prison where religious liberty has been strangled, and the fortress where patriotism has taken its last stand against the forces of the invader. Palestine, Greece, Italy, Switzerland, and Scotland, the countries that have had the most remarkable history, and have done most to advance the human race, are distinguished above other countries for their geological convulsions and revolutions. The Roman Forum is thus but one specimen among numerous others of a law of Providence which has associated the strife of nature with the strife of man, and caused the ravages of the most terrible elements to prepare the way for the highest development of the human race. Between the Roman Forum and the valley beneath Edinburgh Castle we can trace a striking resemblance, not only in their volcanic origin and the connection between their geological history and their analogous civil history, but also in the fact that they were both filled with small lakes. Between the ridges of the old and new town of Edinburgh, where the railway runs through Princes Street Gardens, there was in the memory of many now living a considerable collection of water called the North Loch. In like manner, in the hollow of the Roman Forum there was originally a small lake, a relic of the numerous lakes of the Campagna, which remained after the last elevation of the land, and which existed pretty far on into the human period. It was fed by three streams flowing from the Palatine, the Capitoline, and the Esquiline Hills, which now run underground and meet at this point. Let us picture to ourselves the appearance of this lake embosomed in the hollow of its hills in the far-off pastoral times, when the mountains and the high table-lands of Italy were the chosen territory of those tribes whose property consisted chiefly in their flocks. The hills of Rome, whose elevation was far more conspicuous in ancient times than it is now, presented a precipitous front of dark volcanic rock to the lake. Their slopes were covered with grass and with natural copse-wood, intermixed with tall ilex trees, or umbrella pines; while on their summits were little villages surrounded with Cyclopean walls perched there not only for security, but also for the healthier air, just as we see at the present day all over Italy. On t
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