A Briefe Introduction to Geography by William Pemble
page 23 of 50 (46%)
page 23 of 50 (46%)
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will runne awaie vpon any inequality of ground, for euery 500.
foote allow one for descent, & so much we may with reason, in regard of the swiftnes of many riuers, yea the most, which in many places runnes headlong, in all places very swiftly (especially _Nilus_ whose cateracts or downfalls are notable) which cannot bee without some notable decliuity of the ground. Thus then the whole course of _Nilus_ being 2700. miles from (_F_) to (_B_) the perpendicular or plumb descent of it (_CF_) will be 5. miles. And so high shall the fountaine stand aboue the mouth, and the surface of the plaine Land (for riuers commonly arise at foot of hills) which is (_BXF_) swell vp aboue the surface of the Sea (_BWC_) or (_BY_) which hight of the Land aboue the Sea although it bee greater then is the height of the highest mo[~u]taines aboue the plaine Land, yet it is nothing in comparison of the whole Earth. And this being granted (as with most probabilitie of reason it may) it will appeare that God in the beginning of the world imposed noe perpetuall violence vpon nature, in gathering togeather, the waters into one place, and being so gathered in keeping them from runing backe to cover the earth. At the first so soone as those hollow channells were prepared, the water did naturally slide downe into them, and out of them without miraculous power they cannot returne. For if the sea (_BY_) should overflow the land towards (_F_) the water must ascend in running from (_B_) to (_F_) which is contrary to its nature. Certainly the midland countries, whence springs of great rivers vsually arise, doe ly so high, that the sea cannot naturally overflow them. For as for that opinion that the water of the sea in the middle lies on a heape higher then the water that is by the shore; and so that it is a harder matter to saile out of a Haven to seaward, then to come in (because they goe |
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