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The Pilgrims who settled New England were Independents, peculiar in their ecclesiastical tenet that the single congregation of godly persons, however few or humble, regularly organized for Christ's work, is of right, by divine appointment, the highest ecclesiastical authority on earth. A church of this order existed in London by 1568; another, possibly more than one, the "Brownists," by 1580. Barrowe and Greenwood began a third in 1588, which, its founders being executed, went exiled to Amsterdam in 1593, subsequently uniting with the Presbyterians there. These churches, though independent, were not strictly democratic, like those next to be named.

And yet if, on the other hand, one compares the subsequent fame of men of action with the fame of men of letters, the contrast is indeed bewildering. Who attaches the smallest idea to the personality of the Lord Lichfield whom Dr. Johnson envied? Who that adores the memory of Wordsworth knows anything about Lord Goderich, a contemporary prime minister? The world reads and re-reads the memoirs of dead poets, goes on pilgrimage to the tiny cottages where they lived in poverty, cherishes the smallest records and souvenirs of them. The names of statesmen and generals become dim except to professed historians, while the memories of great romancers and lyrists, and even of lesser writers still, go on being revived and redecorated. What would Keats have thought, as he lay dying in his high, hot, noisy room at Rome, if he had known that a century later every smallest detail of his life, his most careless letters, would be scanned by eager eyes, when few save historians would be able to name a single member of the cabinet in power at the time of his death?

The only races of men that we could expect to find in Europe during the Glacial Age would be Paleolithic tribes, and it is equally manifest that we must find traces of them in beds of this age, or in association with animals that are characteristic of this age, or else we can not assert the existence of man at this time. The valley of the river Somme, in Northern France, has become classical ground to the student of Archaeology, since it was there that such investigations as we have just mentioned were first and most abundantly made. It is now well known that the surface features of a country--that is, its hills and dales, its uplands and lowlands--are mainly due to the erosive power of running water. Our rivers have dug for themselves broad valleys, undermined and carried away hills, and in general carved the surface of a country, until the present appearance is the result. It must be confessed that when we perceive the slow apparent change from year to year, and from that attempt to estimate the time required to produce the effects we see before us, we are apt to shrink from the lapse of time demanded for its accomplishment. Let us not forget that "Time is long," and that causes, however trifling, work stupendous results in the course of ages.