Gulf Stream

• Gulf Stream

29:2.15The elec­tronic or­ga­ni­za­tion of uni­verse power func­tions in seven phases and dis­closes vary­ing re­sponse to lo­cal or lin­ear grav­ity. This sev­en­fold cir­cuit pro­ceeds from the super­uni­verse power cen­ters and per­vades each super­cre­ation. Such spe­cial­ized cur­rents of time and space are def­i­nite and lo­cal­ized en­ergy move­ments ini­ti­ated and di­rected for spe­cific pur­poses, much as the Gulf Stream func­tions as a cir­cum­scribed phe­nom­e­non in the midst of the At­lantic Ocean.

• Gulf Stream
• ancient course

59:1.17360,000,000 years ago the land was still ris­ing. North and South Amer­ica were well up. West­ern Eu­rope and the British Isles were emerg­ing, ex­cept parts of Wales, which were deeply sub­merged. There were no great ice sheets dur­ing these ages. The sup­posed glacial de­posits ap­pear­ing in con­nec­tion with these strata in Eu­rope, Africa, China, and Aus­tralia are due to iso­lated moun­tain glaciers or to the dis­place­ment of glacial de­bris of later ori­gin. The world cli­mate was oceanic, not con­ti­nen­tal. The south­ern seas were warmer then than now, and they ex­tended north­ward over North Amer­ica up to the po­lar re­gions. The Gulf Stream coursed over the cen­tral por­tion of North Amer­ica, be­ing de­flected east­ward to bathe and warm the shores of Green­land, mak­ing that now ice-man­tled con­ti­nent a ver­i­ta­ble tropic par­a­dise.

• functioned in Miocene as today

61:3.9The Ice­land land bridge sub­merged, and the arc­tic wa­ters com­min­gled with those of the At­lantic Ocean. The At­lantic coast of North Amer­ica rapidly cooled, but the Pa­cific coast re­mained warmer than at pres­ent. The great ocean cur­rents were in func­tion and af­fected cli­mate much as they do to­day.