Gormlaki Audacia Directory 07
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Gormlaki Audacia Directory 07
Page 05

Some 13 kil. farther, the river being smooth but swift, we came to a basin 700 m. broad, where the river described a turn toward the north-east. We came upon a large clearing on the hill-side on the left bank. There we saw the remains of two or three huts which had been destroyed by fire. We perceived one or two people, and we landed. We found that it was the shed of an enterprising Peruvian trader who had established himself there in order to collect rubber. Only a few days before we arrived a great fire had taken place, which had destroyed nearly all he possessed; but--fortunately for us--they had saved a few things, and I was able to purchase a quantity of rice, biscuits, dried meat, beans, _farinha_, condensed milk, _banho_ (liquid lard in tins), and a number of other things, such as clothes, shirts, rope, nails, axes, etc., which we needed badly.

Upon reaching Tarentum he began to make preparations to carry on the war with activity. The Tarentines soon found they had obtained a master rather than an ally. He shut up the theatre and all other public places, and compelled their young men to serve in his ranks. Notwithstanding all his activity, the Romans were first in the field. The Consul M. Valerius Laevinus marched into Lucania; but as the army of Pyrrhus was inferior to that of the Romans, he attempted to gain time by negotiation in order that he might be joined by his Italian allies. He accordingly wrote to the Consul, offering to arbitrate between Rome and the Italian states; but Laevinus bluntly told him to mind his own business and retire to Epirus. Fearing to remain inactive any longer, although he was not yet joined by his allies, Pyrrhus marched out against the Romans with his own troops and the Tarentines.

No one can doubt but that this deposit of cave earth itself requires a prolonged time for its accumulation.<8> But this period, however prolonged, at length comes to an end. From some cause, both animals and man again abandoned the cave. Another vast cycle of years rolls away--a time expressed in thousands of years--during which nature again spread over the entombed remains a layer of stalagmite, in some places equal in thickness to the first formation. Above this layer we come to a bed of mold containing remains of the later Stone Age, of the Bronze, and even of the Iron Age. Below the first layer of stalagmite--the completed biography of Paleolithic times; above, the unfinished book of the present. Such are the eloquent results obtained by the thorough exploration of one cave. The results of all the other explorations, in a general way, confirm these. Mr. Dawkins explored a group of caverns in Derbyshire, England. These caverns and fissures are situated in what is known as Cresswell Crags, the precipitous sides of a ravine through which flows a stream of water dividing the counties of Derby and Nottingham.


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