Jules Verne
translation: Frederick Amadeus Malleson

JOURNEY TO THE INTERIOR OF THE EARTH
complete book, e-book

Nové Literární doupě!

Literární doupě bylo modernizováno a přechází pod novou doménu literdo.com!.

Nový web LD vám přínáší ještě více knih s možností výhodného stahování většího množství e-knih podle vlastního výběru (tedy nejen jednotlivých knih nebo balíčků podle autorů) ve formátech ePub , PDF  a MOBI.

 Přejít na nový web Literární doupě

 

CHAPTER XXXVIII.

THE PROFESSOR IN HIS CHAIR AGAIN

To understand this apostrophe of my uncle’s, made to absent French savants, it will be necessary to allude to an event of high importance in a palćontological point of view, which had occurred a little while before our departure.

On the 28th of March, 1863, some excavators working under the direction of M. Boucher de Perthes, in the stone quarries of Moulin Quignon, near Abbeville, in the department of Somme, found a human jawbone fourteen feet beneath the surface. It was the first fossil of this nature that had ever been brought to light. Not far distant were found stone hatchets and flint arrow-heads stained and encased by lapse of time with a uniform coat of rust.

The noise of this discovery was very great, not in France alone, but in England and in Germany. Several savants of the French Institute, and amongst them MM. Milne-Edwards and de Quatrefages, saw at once the importance of this discovery, proved to demonstration the genuineness of the bone in question, and became the most ardent defendants in what the English called this ‘trial of a jawbone.’ To the geologists of the United Kingdom, who believed in the certainty of the fact — Messrs. Falconer, Busk, Carpenter, and others — scientific Germans were soon joined, and amongst them the forwardest, the most fiery, and the most enthusiastic, was my uncle Liedenbrock.

Therefore the genuineness of a fossil human relic of the quaternary period seemed to be incontestably proved and admitted.

It is true that this theory met with a most obstinate opponent in M. Elie de Beaumont. This high authority maintained that the soil of Moulin Quignon was not diluvial at all, but was of much more recent formation; and, agreeing in that with Cuvier, he refused to admit that the human species could be contemporary with the animals of the quaternary period. My uncle Liedenbrock, along with the great body of the geologists, had maintained his ground, disputed, and argued, until M. Elie de Beaumont stood almost alone in his opinion.

We knew all these details, but we were not aware that since our departure the question had advanced to farther stages. Other similar maxillaries, though belonging to individuals of various types and different nations, were found in the loose grey soil of certain grottoes in France, Switzerland, and Belgium, as well as weapons, tools, earthen utensils, bones of children and adults. The existence therefore of man in the quaternary period seemed to become daily more certain.

Nor was this all. Fresh discoveries of remains in the pleiocene formation had emboldened other geologists to refer back the human species to a higher antiquity still. It is true that these remains were not human bones, but objects bearing the traces of his handiwork, such as fossil leg-bones of animals, sculptured and carved evidently by the hand of man.

Thus, at one bound, the record of the existence of (...)

(......)