Hydraulic And Nautical Observations On the Currents in the Atlantic Ocean : Forming An Hypothetical Theorem for Investigation ; Addressed to Navigators

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2. Now the Current to the Southward of this fpace, fo far as it hath been obferved, hath been general!}? found in fadl fetting along this line, in a courfe between the Eaft and. Soutli.
3. Where this line is broken by the intervention of deep chan- nels, or is difcontinued by intervals of fea, without foundings ; fo far mufl: the general effect of the Current running along a line of Coaft, as above fuppofed, not take place ; and, in thofe channels and intervals of deep fea, Currents will diverg
...e off from this ge.- neral courfe Eaft, or perhaps North, efpeclally when the winds.
blow ftrong from the Southern board. Now the fa£t is, as the writer's information ftands, that a Current fets off from the general, courfe^ and runs Eaft, between the lilands Pico, and St. Mlchaeli of the Azores. There is alfo a Current diverges off from the general courfe, and fets Eaft, between the Madeiras and the Canaries, di-r redly in and upon the African Coaft. The general Current how- ever to the Southward of the Canaries holds Its general Southeaftern courfe, and fets in, generally fpeaking, in that diredlon, upon the African Coafts in thofe parts.


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