قراءة كتاب A Manual of the Antiquity of Man

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A Manual of the Antiquity of Man

A Manual of the Antiquity of Man

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but when its grants had failed, Miss Burdett-Coutts paid the expenses of completing the work. In this cave, under a layer of stalagmite, were found many flint knives, associated with the bones of extinct mammals.

M. A. Fontan found in the cave of Massat (Department of Ariége), in 1859, human teeth and utensils associated with the remains of the cave-bear, the fossil hyena, and the cave-lion (Felis spelœa).

In 1861, M. A. Milne Edwards found certain relics of human industry mingled with the fossil bones of animals, in the cave of Lourdes, France.

In 1862, Dr. Garrigou published the result of the researches which he, in conjunction with Rames and Filhol, had made in the caverns of Ariége. These explorers found the jaw-bones of the cave-bear and cave-lion, which had been wrought by the hands of man.

In the upper strata of the tertiary beds (pliocene) at St. Prest (Department of Eure), in the year 1863, M. Desnoyers found the bones of extinct animals which were cut or notched by flint instruments. In the same strata Abbé Bourgeois discovered implements of stone. He communicated his discoveries to the International Congress held at Paris in 1867.

In 1864, James Brown found flint implements midway between Gosport and Southampton, included in gravel from eight to twelve feet thick, capping a cliff which at its greatest height is thirty-five feet above high-water mark. These flint tools exactly resemble those found at Abbeville and Amiens. Some of them are preserved in the Blackmore Museum at Salisbury.

In 1865, there was found in the loess of the Rhine, near Colmar, Alsace, human bones in the same bed with bones of the mammoth, horse, stag, auroch, and other animals.

In 1866, Alfred Stevens first dug out a hatchet from the gravel at the top of the sea-cliff east of the Bournemouth opening, Southampton river. Soon after, Dr. Blackmore, to the west of the valley, obtained two other flint implements. The spot was examined by Lyell in 1867.

Dr. Edward Dupont, an eminent Belgian cave explorer, in the year 1866, found a fragment of a human jaw in the Trou de la Naulette, a bone cave situated on the bank of the river Lesse not far from Chaleux.

At the International Congress of 1867, M. A. Issel reported he had found several human bones in beds of Pliocene age, near Savonia, in Liguria.

The Reindeer Station on the Schusse, in Swabia, was discovered in 1867, during the operations undertaken for the improvement of a mill-pond. The Schusse is a little river which flows into the lake of Constance, and its source is upon the high plateau of Upper Swabia between the lake of Constance and the upper course of the Danube.

In 1868, Thomas Codrington discovered an oval flint implement in gravel at the top of the Foreland Cliff, Isle of Wight, five miles southeast of Ryde.

The fossil Man of Mentone was discovered, in 1873, by M. Riviére, in a cave near Nice, France. The skeleton was almost entire, and imbedded twenty feet below the surface of the deposit.

In 1873, M. Riviére discovered another human skeleton, by the side of which lay a few unpolished stone implements, in one of the caves in the same neighborhood.

In 1873 and 1874, M. Riviére was again so fortunate as to discover, in neighboring caves, the remains of three persons, two of them those of children. The skeletons were in the same condition, and decked with similar ornaments, as those he had previously discovered.


CHAPTER II.

GLACIAL EPOCH.

Happily for the Archæo-geologist, there is given him a point from which to start in his researches into the antiquity of his race. Without it his calculations would be very indefinite and his efforts would be shorn of much of their interest. The Glacial Epoch, that has puzzled the mind of both the geologist and the astronomer, is a guide-post where he may not only look both ways, but also estimate the length of ages and number the years of man. Nothing, then, is of more importance, in this investigation, than an understanding of the condition of the earth prior to the glacial, and the knowledge of the date and length of this epoch.

For untold ages the earth, to all appearance, had been preparing itself for the reception of man. There was an abundance of game, the forests were beautiful, the domestic animals had made their appearance, the climate was warm, the soil rich, and the coal had been formed. Everything seemed to point to a bright and glorious future for man, who had already entered upon the scene. It is true there were fierce and savage beasts to contend with. These seemed but a motive power to stir man to action and develop the resources of his mind. Should he fail for a time to overcome the wild beasts a retreat was provided in the hollow recesses of the earth. But nature felt her work was still unfinished. The earth had passed through the ordeal of fire, and withstood the devastations of water, and now her long summer must come to an end. The arctic regions had been growing colder and colder, and the change was felt in the countries to the south. The northern animals were being clothed with a hairy or woolly garment for their protection. The aspect began to be forbidding. The future prospect of man was not only gloomy, but foreboded he should perish along with the many species of animals that were gradually succumbing to the cold. Great fields of ice were slowly accumulating at both the poles, and at last, by the power of their great weight, assisted by some geographical changes, began to move toward the equator, crushing and grinding the great rocks, and either driving before them, or else destroying, every living thing in their relentless march. Slowly but surely they moved on. The mountains groaned under the enormous weight of ice. Their heads were scarred, their sides bruised, torn and cut. The icy monsters listened not to the pleadings of earth, the lowing of cattle, or the cries of man. Centuries elapsed before the sun re-asserted his power. The rays of the sun, the internal heat of the earth, and other causes, produced a change. The northern ice was broken up by the time it reached latitude 39° North America, leaving its indelible traces in the bowlders, gravel, beds of sand and clay which mark its course. In Europe this sheet of ice extended as far south as Spain and Corsica. The glaciers of the Antarctic regions extended as far as latitude 41° south.

Fauna of Europe.—Among the Fauna may be mentioned the gigantic elephants, of nearly twice the bulk of the largest individuals that now exist, which roamed in herds over England, and extended across the Siberian plains and from Behring Strait to South Carolina. Two-horned rhinoceroses wallowed in the swamps of the ancient forests. Hippopotamuses inhabited the lakes and rivers. The great cave-bear, which sometimes attained the size of a horse, and the cave-tiger, twice as large as the living tiger, preyed upon the animals of less strength than themselves. Troops of hyenas, larger than those of South America, disputed with other beasts of prey. A species of wild-cat, lynx, and leopard found retreats in the same forests. Then there was a remarkable carnivorous animal called Machairodus, about the size of a tiger, and from the shape and size of the sword-like teeth, must have been a very destructive creature. The lemming and the musk ox found a home, and the wild horse pranced about unrestrained by the hand of man. The great Irish elks swiftly moved over the ground, and must have been very numerous, as their remains occur in abundance in peat-bogs and marl-pits. Nor should it be unmentioned that there was also a species of gigantic ox nearly as large as an

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