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Spate Toran Sectory 21 Page 11
This would give us a long Spring and Summer, but a short Fall and Winter. This in itself would make a great difference. We must beer in mind, however, that at such a time as we are here considering, the earth would be ten millions of miles nearer the sun in Winter than at present. It would certainly then receive more heat in a given time during Winter than at present.<16> Mr. Croll estimates that whereas the difference in heat received during a given time is now one-fifteenth, at the time we are considering it would be one-fifth. Hence we see that at such a time the Winter would not only be much shorter than now, but at the same time would be much milder.
The archeologist's answer is that the real drama of daily life of the settlers--the life they knew 24 hours a day--is locked in the unwritten history beneath humus and tangled vegetation of the island. Here a brass thimble from the ruins of a cottage still retains a pellet of paper to keep it on a tiny finger that wore it 300 years ago. A bent halberd in an abandoned well, a discarded sword, and a piece of armor tell again the passing of terror of the unknown, after the Indians retreated forever into the distant hills and forests. Rust-eaten axes, wedges, mattocks, and saws recall the struggle to clear a wilderness. The simple essentials of life in the first desperate years have largely vanished with traces of the first fort and its frame buildings. But in later houses the evidence of Venetian glass, Dutch and English delftware, pewter, and silver eating utensils, and other comforts and little luxuries tell of new-found security and the beginning of wealth. In all, a half-million individual artifacts at the Jamestown museum represent the largest collection from any 17th-century colonial site in North America.
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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