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These views of Major Palmer’s are shared by M. Naville, by Sir Wm. Dawson, and others, and have been decisively confirmed by the geological survey of the region. In 1883 the Committee of the Palestine Exploration Fund sent out Professor Hull, the eminent geologist, accompanied by Major Kitchener, R.E., and other competent men, and this party investigated the geology of Lower Egypt, of the Desert of Sinai, the Valley of the Arabah, and the southern portion of Palestine. The results were very remarkable. It appears, for instance, that at a distant period of the past the waters of the seas, lakes, and gulfs of all this region stood some two hundred feet higher than they do now—the proof being found in the fact that at the height of two hundred feet the limestone rocks have been bored into by the well-known “shell-fish,” the pholas, while the sands and gravels at that height contain shells and corals and crinoids, of the same species as those which still inhabit the waters of the Gulf of Suez. With the waters at that height the whole of Lower Egypt would be submerged, together with extensive tracts on either side of the Gulf of Suez. But this occurred in the distant past, probably many ages before mankind dwelt in these regions at all. There was, however, a more recent period, as the land slowly rose out of the waters—and Professor Hull thinks it may have coincided with the time of the Exodus—when the waters were just 26 feet higher than they are at present, and then, although Lower Egypt would not be submerged, the Gulf of Suez must have extended northward as far as the Bitter Lakes, making an arm of the sea about a mile wide and 20 or 30 feet deep.