THE DRIFT OF THE SEA. 321 



fast, now slow, now running this way, tlien that — all of which 

 may be taken as so many signs of the tremendous throes which 

 occur in the bosom of the ocean. Sometimes the sea recedes from 

 the shore, as if to gather strength for a great rush against its bar- 

 riers, as it did when it fled back to join with the earthquake and 

 overwhelm Callao in 1746, and again Lisbon nine years afterward. 

 The tide-rips in mid ocean, the waves dashing against the shore, 

 the ebb and flow of the tides, may be regarded, in some sense, as 

 the throbbings of the great sea pulse. 



917. The motions of the Gulf Stream (§ 55), beating time for. 

 the ocean, and telling the seasons for the whales, also suggest the 

 idea of a pulse in the sea, which may assist us in explaining some 

 of its phenomena. At one beat there is a rush of warm water from 

 the equator toward the poles, at the next beat a flow from the 

 poles toward the equator. This sort of pulsation is heard also in 

 the bowlings of the storm and the whistling of the wind ; the nee- 

 dle trembles unceasingly to it, and tells us of magnetic storms of 

 great violence, which at times extend over large portions of the 

 earth's surface ; and when we come to consult the records of those 

 exc[uisitely sensitive anemometers, which the science and ingenu- 

 ity of the age have placed at the service of philosophers, we find 

 there that the pulse of the atmosphere is never still : in what ap- 

 pears to us the most perfect calm, the recording pens of the auto- 

 matic machine are moving to the pulses of the air. 



918. Now if we may be permitted to apply to the Gulf Stream 

 and to the warm flows of water from the Indian Ocean an idea 

 suggested by the functions of the human heart in the circulation 

 of the blood, Ave perceive how these pulsations of the great sea- 

 heart may perhaps assist in giving circulation to its waters through 

 the immense system of aqueous veins and arteries that run between 

 the equatorial and polar regions. The waters of the Gulf Stream, 

 moving together in a body (§1) through such an extent of ocean, 

 and being almost impenetrable to the cold waters on either side — 

 which are, indeed, the ^banks of this mighty river — may be com- 

 pared to a wedge-shaped cushion placed between a wall of waters 

 on the right and a wall of waters on the left. If now v*^e imagine 

 the equilibrium of the sea to be disturbed by the heating or cool- 



