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Galleporto Bavicarius Directory 13
Page 02
So again it is with the things that gall us most. What is it that rises up against us at odd times and smites us in the face again and again for years after it has happened? That we spent all the best years of our life in learning what we have found to be a swindle, and to have been known to be a swindle by those who took money for misleading us? That those on whom we most leaned most betrayed us? That we have only come to feel our strength when there is little strength left of any kind to feel? These things will hardly much disturb a man of ordinary good temper. But that he should have said this or that little unkind and wanton saying; that he should have gone away from this or that hotel and given a shilling too little to the waiter; that his clothes were shabby at such or such a gardenparty--these things gall us as a corn will sometimes do, though the loss of a limb way not be seriously felt.
This was at a time when slowly falling temperature but dimly prophesied a reign of arctic cold, still far in the future. This race does not seem to have had much capacity for advancement, since ages came and went leaving him in the same low state. During the climax of glacial cold he doubtless sought the southern coasts of Europe along with the temperate species of animals. But whenever the climatic conditions were such that these animals could find subsistence as far north as England he accompanied them there, and so his remains are found constantly associated with theirs throughout Europe. Though doubtless very low in the scale, and at the very foot of the ladder of human progress, we are acquainted with no facts connecting them with the higher orders of animals. If such exists, we must search for them further back in geological time. The men of the River Drift were distinctively human beings, and as such possessed those qualities which, developing throughout the countless ages that have elapsed, have advanced man to his present high position.
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.
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