Here should be mentioned one of Buffon's contemporaries and countrymen; one who was the first true field geologist, an observer rather than a compiler or theorist. This was Jean E. Guettard (1715-1786). He published, says Sir Archibald Geikie, in his valuable work, _The Founders of Geology_, about two hundred papers on a wide range of scientific subjects, besides half a dozen quarto volumes of his observations, together with many excellent plates. Geikie also states that he is undoubtedly entitled to rank among the first great pioneers of modern geology. He was the first (1751) to make a geological map of northern France, and roughly traced the limits of his three bands or formations from France across the southeastern English counties. In his work on "The degradation of mountains effected in our time by heavy rains, rivers, and the sea,"[69] he states that the sea is the most potent destroyer of the land, and that the material thus removed is deposited either on the land or along the shores of the sea. He thought that the levels of the valleys are at present being raised, owing to the deposit of detritus in them. He points out that the deposits laid down by the ocean do not extend far out to sea, "that consequently the elevations of new mountains in the sea, by the deposition of sediment, is a process very difficult to conceive; that the transport of the sediment as far as the equator is not less improbable; and that still more difficult to accept is the suggestion that the sediment from our continent is carried into the seas of the New World. In short, we are still very little advanced towards the theory of the earth as it now exists." Guettard was the first to discover the volcanoes of Auvergne, but he was "hopelessly wrong" in regard to the origin of basalt, forestalling Werner in his mistakes as to its aqueous origin. He was thus the first Neptunist, while, as Geikie states, his "observations in Auvergne practically started the Vulcanist camp." We now come to Lamarck's own time. He must have been familiar with the results of Pallas's travels in Russia and Siberia (1793-94). The distinguished German zoölogist and geologist, besides working out the geology of the Ural Mountains, showed, in 1777, that there was a general law in the formation of all mountain chains composed chiefly of primary rocks;[70] the granitic axis being flanked by schists, and these by fossiliferous strata. From his observations made on the Volga and about its mouth, he presented proofs of the former extension, in comparatively recent times, of the Caspian Sea. But still more pregnant and remarkable was his discovery of an entire rhinoceros, with its flesh and skin, in the frozen soil of Siberia. His memoir on this animal places him among the forerunners of, if not within the ranks of, the founders of palæontology.