Crellic Pontain Sectory 10

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Crellic Pontain Sectory 10

In the case of the river Somme we have a valley in some places a mile or more in width, and about two hundred feet in depth. This has mostly been excavated in chalk rock. Taking our present large rivers as a basis, it would require from one to two hundred thousand years for the Somme to perform this work.<36> It will not do, however, to take the present action of our rivers as a guide, since we have every reason to suppose this work went forward much more rapidly in past times. But we can not escape the conclusion that it demands a very long time indeed to explain it. The valley has remained in its present shape long enough to admit the formation of great beds of peat in some portions. Peat is formed by the decomposition of vegetable growth. Its growth is in all cases slow, depending entirely upon local circumstances. European scholars who have made peat formation a special study assure us that to form such immense beds as occur near Abbeville, several thousand years are required, even under the most favorable conditions.

The constitution of the _Comitia Centuriata_, as established by Servius Tullius,[45] had undergone a great change between the time of the Licinian Rogations and the Punic Wars, but both the exact time and nature of this change are unknown. It appears, however, that its object was to give more power and influence to the popular element in the state. For this purpose the 35 tribes were taken as the basis of the new Constitution of the Centuries. Each tribe was probably divided into five property Classes, and each Classis was subdivided into two Centuries, one of Seniores and the other of Juniores. Each tribe would thus contain 10 Centuries, and, consequently, the 35 tribes would have 350 Centuries, so that, with the 18 Centuries of the Knights, the total number of the Centuries would be 368.



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