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the note. The reader, it is confidently presumed, will be satisfied with what was said of it in the account of the former voyage.--E.] [Footnote 30: The judgment of the ingenious author of _Recherches sur Americains_, on this question, seems to be very deserving of a place here: "Qu'on calcule, comme on voudra, on sera toujours contraint d'avouer, qu'il y a une plus grande portion de continent situee dans la latitude septentrionale, que dans la latitude australe. "C'est fort mal a-propos, qu'on a soutenu que cette repartition inegale ne sauroit exister, sous pretexte que le globe perdroit son equilibre, faute d'un contrepoids suffisant au pole meridionale. Il est vrai qu'un pied cube d'eau salee ne pese pas autant qu'un pied cube de terre; mais on auroit du reflechir, qu'il peut y avoir sous l'ocean des lits & des couches de matieres, dont la pesanteur specifique varie a l'infini, & que le peu de profondeur d'une mer, versee sur une grande surface, contrebalance les endroits ou il y a moins de mer, mais ou elle est plus profonde."--_Recherches Philosophiques_, tom. ii, p. 375.--D. We offered some observations on this topic in the preceding volume, and need scarcely resume it, as it cannot be imagined that any of our readers still entertain the belief of the necessity for such an equilibrium. The object in again alluding to it, is to call attention to some observations of another kind, which Mr Jones has hazarded in one of his Physiological Disquisitions. According to him, no such thing as a southern counterpoise ought to have been expected, for it seems to be the constitution of our globe, that land and water are contrasted to each other on its opposite sides. "If," says he, "you bring the meridian of the Cape of Good Hope under the brazen circle, or universal meridian of a terrestrial globe, observing that this meridian passes through the heart of the continents of Europe and Africa, you will find that the opposite part of the meridian passes through the middle of the great, south sea. When the middle of the northern continent of America, about the meridian of Mexico, is examined in the same way, the opposite part passes very exactly through the middle of the Indian ocean. The southern continent of America is opposed by that eastern sea which contains the East India islands. The southern continent of New Holland is opposite to the Atlantic ocean. This alternation, if I may so call it, between the land and sea, is
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