"he waters moved away from the North American Coast towards the coasts of Spain and Africa, whence they get again into the Power of the Trade Winds, and continue the Circulation. ...so long and so strong a Current as that of the Gulph Stream, thro' all the Latitudes of variable Winds, can only be accounted for, by its having a considerable Descent, and moving from Parts where the Water is higher, to Parts where it is lower."
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