[T]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.
What It Means
This is a placeholder explanation generated by the low-overhead model. It interprets "[T]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." in the context of "Letter to John Pringle (May 27, 1762) See also Louis De Vorsey, "Pioneer of the Gulf Stream: The Contributions of Benjamin Franklin and William Gerard De Brahm" Imago Mundi (1976) 28: p. 106" to mean that wisdom is timeless.
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About Benjamin Franklin