FREE BOOKS

Author's List




PREV.   NEXT  
|<   938   939   940   941   942   943   944   945   946   947   948   949   950   951   952   953   954   955   956   957   958   959   960   961   962  
963   964   965   966   967   968   969   970   971   972   973   974   975   976   977   978   979   980   981   982   983   984   985   986   987   >>   >|  
the area of Europe. The surface of the latter contains about 2,793,000 square geographical miles. The unexplored antarctic region, as calculated for me by Mr. Gardner, in 1840, equalled about 7,620,000 square miles. [180] On icebergs in low latitudes, by Capt. Horsburgh, by whom the sketch was made. Phil. Trans. 1830. [181] Scoresby's Arctic Regions, vol. i. p. 234. [182] This follows, observes Herschel, from a very simple theorem, which may be thus stated:--"The amount of heat received by the earth from the sun, while describing any part of its orbit, is proportional to the angle described round the sun's centre." So that if the orbit be divided into two portions by a line drawn _in any direction_ through the sun's centre, the heat received in describing the two unequal segments of the eclipse so produced will be equal. Geol. Trans. vol. iii. part. ii. p. 298; second series. [183] On Isothermal Lines. [184] A full consideration of the effect of changes in physical geography on the distribution and extinction of species is given in book iii. [185] For calculations founded on astronomical data, see Young's Nat. Phil., Lect. xlvii.; Mrs. Somerville's Connex. of Phys. Sci., sect. 14, p. 110. Laplace, endeavoring to estimate the probable depth of the sea from some of the phenomena of the tides, says of the ocean generally, "que sa profondeur moyenne est du meme ordre que la hauteur moyenne des continens et des isles au-dessus de son niveau, hauteur qui ne surpasse pas mille metres (3280 ft.)" Mec. Caleste, tom. xi. et Syst. du Monde, p. 254. The expression "du meme ordre" admits in mathematical language of considerable latitude of signification, and does not mean that the depth of the water below the level of the sea corresponds exactly to the height of the land above it. It appeared from the observations of Sir James Ross, communicated to me in 1849, by himself, and his fellow voyager, Dr. Joseph Hooker, that in latitude 15 degrees 3 minutes S., longitude 23 degrees 14 minutes W. (the island of Trinidad, the nearest land, being 486 miles distant, and bearing S. 47 W.), they sounded with a weight of 76 lbs., and 4600 fathoms of line,
PREV.   NEXT  
|<   938   939   940   941   942   943   944   945   946   947   948   949   950   951   952   953   954   955   956   957   958   959   960   961   962  
963   964   965   966   967   968   969   970   971   972   973   974   975   976   977   978   979   980   981   982   983   984   985   986   987   >>   >|  



Top keywords:

describing

 

received

 

latitude

 

moyenne

 

hauteur

 

centre

 

degrees

 
minutes
 
square
 
dessus

niveau

 

fathoms

 

Laplace

 

bearing

 

distant

 

metres

 

surpasse

 

continens

 
endeavoring
 

generally


profondeur

 

phenomena

 

weight

 
Caleste
 

estimate

 

sounded

 

probable

 

Hooker

 
Joseph
 

height


corresponds

 

appeared

 

fellow

 

communicated

 
observations
 
voyager
 

nearest

 

expression

 

admits

 

mathematical


language

 

Trinidad

 

signification

 

longitude

 
considerable
 

island

 

extinction

 

Regions

 
Arctic
 

Scoresby