A Manual of the Antiquity of Man. J. P. Maclean

A Manual of the Antiquity of Man - J. P. Maclean


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they were obtained by Mr. Vivian.

      Mr. Godwin-Austen, in his communication to the Geological Society in the year 1840, states, in his description of Kent's Hole, he found works of art in all parts of the cave.

      The fossil Man of Denise was discovered by a peasant, in an old volcanic tuff, near the town of Le Puy-en-Velay, Central France, an account of which was first published by Dr. Aymard, in 1844. Able naturalists, who have examined these bones, especially those familiar with the volcanic regions of Central France, declared that they believed them to have been enveloped by natural causes in the tufaceous matrix in which they are now seen.

      In the years 1845–1850, Casiano de Prado made discoveries on the banks of the Manzanares, near Madrid. They consisted of portions of the skeletons of the rhinoceros, and a nearly perfect skeleton of an elephant in the diluvial sand. Lying beneath this ossiferous sand, were several flint axes of human workmanship.

      

Fig. 1. Sir Charles Lyell.

      Near the town of Aurignac, France, a workman named Bonnemaison, in the year 1852, accidently discovered a cave containing the remains of seventeen human skeletons. These bones were taken by Dr. Amiel, the mayor of Aurignac, who was ignorant of their value, and consigned to the parish cemetery. The spot of their re-inhumation has been forgotten, and this treasure is now lost to science. In 1860, the cave was explored by Edward Lartet. After a long and patient examination, he came to the conclusion that the cave was a human burial place, cotemporary with the mammoth and other great animals of the quaternary epoch.

      It was at the meeting of the British Association, in 1855, that Sir Charles Lyell declared his belief in the great antiquity of the human race. He had before opposed the idea, but was convinced of the truth by personal examination of human bones and flint hatchets, from the quarries of St. Acheul. He became enthusiastic in his investigations, and, in order to present the discussion clearly to the scientific public, he published his "Geological Evidences of the Antiquity of Man," in 1863. In the last edition of his "Principles of Geology," he bestows considerable space to the discussion of the subject. He was closely followed, in the same view, by other eminent geologists.

      The remains of the ancient Lake Dwellings of Switzerland were discovered in the winter of 1853–1854. That winter was so dry and cold that the water of the lakes fell far below its ordinary level. On account of this, a large tract of ground of Lake Zurich was gained by the people throwing up embankments. In the process of the work, the piles on which stood the dwellings, fragments of pottery, bone and stone implements, and various other relics, were discovered.[5] Dr. Keller, of Zurich, examined the objects, and at once came to a right understanding as to their signification. He carefully examined the remains, and described these lake habitations in six memoirs presented to the Antiquarian Society of Zurich, in 1854, 1858, 1860, 1863, and 1866. In 1866 these memoirs were translated into English by J. E. Lee, together with articles from other antiquaries, under the title of "The Lake Dwellings of Switzerland, and other parts of Europe." This work contains ninety-seven plates, besides many wood-cuts.

      Memoirs of the Dwellers of different lakes have, from time to time, been published, but they are included in the translated work of Dr. Keller.

      The far-famed Neanderthal skull was discovered by Dr. Fuhlrott, in the year 1857, in a limestone cavern, near Düsseldorf, in a deep ravine known by the name of Neanderthal. This skull, with parts of the skeleton to which it belonged, was found under a layer of mud, about five feet in thickness. It is now in the cabinet of Dr. Fuhlrott, Elberfeld, Rhenish Prussia.

      In 1858, a bone-cavern was found near Torquay, not far from Kent's Hole. This cave was examined by a scientific commission. At first it was undertaken by the Royal Society, 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.

       Table of Contents

       Table of Contents

      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


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