FREE BOOKS

Author's List




PREV.   NEXT  
|<   365   366   367   368   369   370   371   372   373   374   375   376   377   378   379   380   381   382   383   384   385   386   387   388   389  
390   391   392   393   394   395   396   397   398   399   400   401   402   403   404   405   406   407   408   409   410   411   412   413   414   >>   >|  
During our voyage along this coast, we generally observed that a current set us to the northward, at the rate of ten or twelve miles every day. When in about the latitude of 8 deg. S. we began to be attended by vast numbers of flying fish and bonitos, which were the first we had seen after leaving the coast of Brazil. It is remarkable that these fish extend to a much higher latitude on the east side of America than on the west, as we did not lose them on the coast of Brazil till near the southern tropic. The reason, doubtless, of this diversity, is owing to the different degrees of heat obtaining on different sides of the continent in the same latitude; and, on this occasion, I use the freedom to make a short digression on the heat and cold of different climates, and on the variations which occur in the same places at different times of the year, and in different places in the same degree of latitude. The ancients conceived that of the five zones into which they divided the surface of the globe, two only were habitable; supposing that the heat between the tropics, and the cold within the polar circles, were too intense to be supported by mankind. The falsehood of this idea has been long established; but the particular comparison of the heat and cold of these various climates have as yet been very imperfectly considered. Enough is known, however, safely to determine this position, that all the places within the tropics are far from being the hottest on the globe, as many within the polar circle are far from enduring that extreme degree of cold to which their situation seems to subject them; that is to say, that the temperature of a place depends much more upon other circumstances, than upon its distance from the pole, or its proximity to the equinoctial line. This proposition relates to the general temperature of places taking the whole year round, and, in this sense, it cannot be denied that the city of London, for instance, enjoys much warmer seasons than the bottom of Hudson's Bay, which is nearly in the same latitude, but where the severity of the winter is so great as scarcely to permit the hardiest of our garden plants to live. If the comparison be made between the coast of Brazil and the western shore of South America, as, for example, between Bahia and Lima, the difference will be found still more considerable; for, though the coast of Brazil is extremely sultry, yet the coast of the South Sea, in the same la
PREV.   NEXT  
|<   365   366   367   368   369   370   371   372   373   374   375   376   377   378   379   380   381   382   383   384   385   386   387   388   389  
390   391   392   393   394   395   396   397   398   399   400   401   402   403   404   405   406   407   408   409   410   411   412   413   414   >>   >|  



Top keywords:

latitude

 

Brazil

 
places
 

tropics

 

America

 

degree

 
temperature
 
comparison
 

climates

 

subject


distance
 
circumstances
 
sultry
 

depends

 

extremely

 

hottest

 
safely
 

determine

 

position

 

imperfectly


considered

 

Enough

 

enduring

 

extreme

 

circle

 

proximity

 

situation

 

proposition

 

severity

 

winter


seasons

 

bottom

 

Hudson

 

garden

 

plants

 
western
 
hardiest
 

scarcely

 

permit

 

difference


warmer
 
general
 

taking

 

relates

 

considerable

 

instance

 
enjoys
 

London

 
denied
 

equinoctial