140 THE PHYSICAL GEOGRxVPHY OF THE SEA. 



run with great force. On a voyage from the Society to the Sand- 

 wich Islands, I encountered one running at the rate of ninety-six 

 miles a day. 



And what else should we expect in this ocean but a system of 

 currents and counter-currents apparently the most uncertain and 

 complicated ? The Pacific Ocean and the Indian Ocean may, in 

 the view we are about to take, be considered as one sheet of wa- 

 ter. This sheet of water covers an area quite equal in extent to 

 one half of that embraced by the whole surface of the earth ; and, 

 accordinsT to Professor Alexander Keith Johnston, who so states 

 it in the new edition of his splendid Physical Atlas, the total an- 

 nual fall of rain on the earth's surface is one hundred and eighty- 

 six thousand, two hundred and forty cubic imperial miles. Not 

 less than three fourths of the vapor which makes this rain comes 

 from this waste of waters ; but supposing that only half of this 

 quantity, i. e., ninety-three thousand, one hundred and twenty 

 cubic miles of rain falls upon this sea, and that that much, at 

 least, is taken up from it again a^vapor, this would give two 

 hundred and fifty-five cubic miles as the quantity of water wdiich 

 is daily lifted up and poured back again into this expanse. It is 

 taken up at one place and rained down at another, and in this 

 process, therefore, we have agencies for multitudes of partial and 

 conflicting currents, all, in their set and strength, apparently as 

 uncertain as the winds. 



The better to appreciate the operation of such agencies in pro- 

 ducing currents in the sea, now" here, now there, first this way, 

 and then that, let us, by way of illustration, imagine a district of 

 two hundred and fifty-five square miles in extent to be set apart, 

 in the midst of the Pacific Ocean, as the scene of operations for 

 one day. We must now conceive a machine capable of pumping 

 up, in the twenty-four hours, all the w^ater to the depth of one 

 mile in this district. The machine must not only pump up 

 and bear off this immense quantity of water, but it must discharge 

 it again into the sea on the same day, but at some other place. 

 Now here is a force for creating currents that is equivalent in its 

 results to the effects that would be produced by bailing up, in 

 twenty-four hours, two hundred and fifty-five cubic miles of wa- 

 ter from one part of the Pacific Ocean, and emptying it out again 

 upon another part. The currents that would be created by such an 



