FREE BOOKS

Author's List




PREV.   NEXT  
|<   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65   66   67  
68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   91   92   >>   >|  
force of water ejected from the river receives no immediate repellent action from the Gulf, but extends into it many miles without the least signs of disturbance, as may be plainly discovered even in the most casual observation. It is known as well that the water of the river remains perfectly palatable at a very close proximity to the sea. This is a very good evidence of the superior force of the river's current. The two volumes of water mix a considerable distance out at sea. An able engineer states that, upon examination, he found a column of fresh water seven feet deep and seven thousand feet wide, and discovered salt water at eight feet below the surface. As the result of his investigations, he divides the water into three strata, as follows: 1. Fresh water, running out at the top with a velocity of three miles an hour. 2. Salt water, beneath the fresh, also running out at about the same velocity. 3. A reflex flow of salt water, running in slowly at the bottom. It is this inward current, he thinks, that produces the deposit, and in doing so carries with it no small degree of sea drift. The influx of the lower column flowing up stream, after it passes the dead point, is allowed time and opportunity for the sediment to deposit. The principle of the reflex current is somewhat that of an eddy, not only produced by the conflict of two opposing bodies of water, but also is much influenced in the under currents by the multitude of estuaries presented by the irregular sea front of the coast. A gentleman, who seems to have taken a very statistical view of these bars, makes the following business-like and curious calculation as to their immensity: we introduce it on account of its originality. He says the average quantity of water discharged per second is five hundred and ten thousand cubic feet. The quantity of salt suspended, one in three thousand by volume. The quantity of mud discharged, one hundred and seventy cubic feet per second. Considering seventeen cubic feet equal to one ton, the daily discharge of mud is eight hundred and sixty-four thousand tons, and would require a fleet of seventeen hundred and twenty-eight ships, of five hundred tons each, to transport the average daily discharge. And to lift this immense quantity of matter, it would require about seven hundred and seventy-one dredging machines, sixteen horse power, with a capacity of labor amounting to one hundred and forty tons, working eight
PREV.   NEXT  
|<   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65   66   67  
68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   91   92   >>   >|  



Top keywords:

hundred

 

quantity

 

thousand

 

running

 

current

 
reflex
 

seventy

 

deposit

 

column

 

seventeen


average
 

discharged

 

velocity

 

require

 

discovered

 

discharge

 

statistical

 
working
 

amounting

 

gentleman


presented

 

conflict

 

opposing

 

bodies

 

produced

 

influenced

 
business
 
irregular
 

estuaries

 
multitude

currents

 

curious

 

twenty

 
transport
 

matter

 

immense

 

principle

 

volume

 
suspended
 

dredging


machines

 

calculation

 

immensity

 

Considering

 

capacity

 

introduce

 
sixteen
 
originality
 

account

 

evidence