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Laing such a towering advantage over them all. "An authority like Prestwich," who "cannot be accused of theological bias," influenced, however, by a servile astronomical bias, "reduces to 20,000 years a period to which Lyell and modern geologists assign a duration of more than 200,000 years;" which "shows in what a state of uncertainty we are as to this vitally important problem;" for this time assigned by Prestwich "would be clearly insufficient to allow for the development of Egyptian civilization, as it existed 5,000 years ago, from savage and semi-animal ancestors; as is proved to be the case with the horse, stag, elephant, ape," and so on.

His report, therefore, to the Royal Society, accompanied by a photograph showing the position of the flint tool in situ before it was removed from its matrix, not only satisfied many inquirers, but induced others to visit Abbeville and Amiens; and one of these, Mr. Flower, who accompanied Mr. Prestwich on his second excursion to St.

Gunn was the first to perceive this mistake, which he explained to me on the spot when I revisited Mundesley in the autumn of 1859 in company with Dr. Hooker and Mr. King. Prestwich has given a correct account of this section in a paper read to the British Association, Oxford, 1860.

Now Prestwich, we are told elsewhere, is "the first living authority on the tertiary and quaternary strata." If, then, astronomical prepossession can reduce 200,000 to 20,000 years, the sin of theology, which reduces 20,000 to 7,000 is comparatively venial.

Prestwich, and compared by some antiquaries to a sling-stone, was obtained in 1836 by Mr. Whitburn, 4 feet deep in sand and gravel, in which the teeth and tusks of elephants had been found. The Wey flows through the gorge of the North Downs at Guildford to join the Thames. Mr.

However, Prestwich has some "facts" as well as prepossessions, such as "the rapid advance of the glaciers of Greenland," which does not accord with the generalization from the Swiss glaciers; and the quicker erosion of river valleys, due to a greater rainfall; facts which, however, are met by "a minute description of the successive changes by which in post-glacial time the Mersey valley and estuary were brought into their present condition, with an estimate of the time they may have required;" which is "in round numbers 60,000 years," as opposed to Prestwich's 10,000 or 8,000.

"'Not proven' is the verdict which most geologists would return." "The confidence with which Croll's theory was first received has been a good deal shaken." "We have to fall back, therefore, on the geological evidence of deposition and denudation ... in any attempt to decide between the 200,000 years of Lyell and the 20,000 years of Prestwich."

Sciences, vol. i. . Geikie, Geological Sketches at Home and Abroad, p. 271 . Prestwich, Geology, vol. i. p. 370, quoting from Richthofen. The origin of geysers is variously explained; see Prestwich, Geology, vol. i. p. 170. They are probably due to heated waters suddenly converted into steam by contact with rock at a high temperature.

Prestwich, in his admirable Memoirs on the eocene deposits of England and France, is able to draw a close general parallelism between the successive stages in the two countries; but when he compares certain stages in England with those in France, although he finds in both a curious accordance in the numbers of the species belonging to the same genera, yet the species themselves differ in a manner very difficult to account for considering the proximity of the two areas, unless, indeed, it be assumed that an isthmus separated two seas inhabited by distinct, but contemporaneous faunas.

The subject has been brought before the Geological Society by Mr Prestwich, as regards the Holmfirth flood, with a view to collect data as to the power of moving water, the height of the flood, the time in which the water ran off, together with exact measurements of the fall of the ground, and the amount of denudation.