44 THE PHYSICAL GEOGRAPHY OF THE SEA. 



level, than Nature is sure with her efforts to restore equilibrium in 

 both sea and air whenever, wherever, and by whatever it be dis- 

 turbed. Therefore, though the waters of the Gulf Stream do not 

 extend to the bottom, and though they be not impenetrable to the 

 waters on either hand, yet, seeing that they have a waste of waters 

 on the right and a waste of waters on the left, to which (^ 2) they 

 offer a sort of resisting permeability, we are enabled to compre- 

 hend how the waters on either hand, as their specific gravity is in- 

 creased or diminished, wdll impart to the trough of this stream a 

 vibratory motion, pressing it now to the right, now to the left, ac- 

 cording to the seasons and the consequent changes of temperature 

 in the sea. 



54. Plate VI. shows the limits of the Gulf Stream for March 

 and September. The reason for this change of position is obvi- 

 ous. The banks of the Gulf Stream (§ 1) are cold water. In 

 winter, the volume of cold water on the American, or left side of 

 the stream, is greatly increased. It must have room, and gains it 

 by pressing the warmer waters of the stream farther to the south, 

 or right. In September, the temperature of these cold waters is 

 modified ; there is not such an extent of them, and then the warmer 

 waters, in turn, press them back, and so the pendulum-like motion 

 is preserved. 



55. The observations made by the United States Coast Survey 

 indicate that there are in the Gulf Stream threads of warmer, sep- 

 arated by streaks of cooler water. See Plate VI., in which these 

 are shown. Figure A may be taken to represent a thermomet- 

 rical cross section of the stream opposite tne Capes of Virginia, 

 for instance ; the top of the curve representing the thermometer 

 in the threads of the warmer water, and the depressions the height 

 of the same instrument in the streaks of cooler water between, 

 thus exhibiting, as one sails from America across the Gulf Stream, 

 a remarkable series of thermometrical elevations and depressions 

 in the surface temperature of this mighty river in the sea. 



56. As a rule, the hottest water of the Gulf Stream is at or near 

 the surface ; and as the deep sea thermometer is sent down, it 

 shows that these waters, though still far warmer than the water on 

 either side at corresponding depths, gradually become less and 

 less warm until the bottom of the current is reached. There is 

 reason to beheve that the warm waters of the Gulf Stream are no- 



