FREE BOOKS

Author's List




PREV.   NEXT  
|<   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   988   989   990   >>   >|  
companied by a map. [199] See Proceedings of Geol. Soc. vol. ii. p. 334. [200] It may be observed, that the facts and inferences exhibited in this map bear not merely on the theory of climate above proposed, but serve also to illustrate the views explained in the third book respecting the migration of animals and plants and the gradual extinction of species. [201] See Sir R. Murchison's Paper on the Alps, Quart. Journ. Geol. Soc. vol. v. and my Anniversary Address for 1850, ibid. vol. vi. [202] Allgemeine Literatur Zeitung, No. cxxxix. July, 1833. [203] In this estimate, the space within the antarctic circle is not taken into account: if included, it would probably add to the excess of dry land; for the late discoveries of Capt. Sir James Ross, who penetrated to lat. 78 degrees 10 minutes S., confirm the conjecture of Captain Cook that the accumulation of antarctic ice implies the presence of a certain quantity of terra firma. The number of square miles on the surface of the globe are 148,522,000, the part occupied by the sea being 110,849,000, and that by land, 37,673,000; so that the land is very nearly to the sea as 1 part in 4. I am informed by Mr. Gardner that, according to a rough approximation, the land between the 30 degrees N. lat. and the pole occupies a space _about equal to that of the sea_, and the land between the 30 degrees S. lat. and the antarctic circle about one-sixteenth of that zone. [204] See papers by Mr. Smith of Jordanhill, F. G. S., and the author, Proceedings Geol. Soc. No. 63, 1839, also that of Prof. E. Forbes, before cited, p. 86, note. [205] The theorem is thus stated:--"The eccentricity of the orbit varying, the total quantity of heat received by the earth from the sun in one revolution is inversely proportional to the minor axis of the orbit. The major axis is invariable, and therefore, of course, the absolute length of the year: hence it follows that the mean annual average of heat will also be in the same inverse ratio of the minor axis."--Geol. Trans. second series, vol. iii. p. 295. [206] Ann. du Bur. des Long. 1834. [207] Poisson, Thaorie Mathamat. de la Chaleur, Comptes Rendus de l'Acad. des Sci., Jan. 30, 18
PREV.   NEXT  
|<   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   988   989   990   >>   >|  



Top keywords:

antarctic

 

degrees

 

circle

 

quantity

 

Proceedings

 

author

 

Forbes

 
varying
 
eccentricity
 
stated

theorem

 

papers

 

Gardner

 

approximation

 

observed

 

informed

 

received

 

sixteenth

 
occupies
 

Jordanhill


Poisson

 

series

 

Thaorie

 
Mathamat
 

Rendus

 

companied

 

Chaleur

 

Comptes

 
invariable
 

proportional


revolution

 

inversely

 

absolute

 

length

 
inverse
 
average
 

annual

 

cxxxix

 

illustrate

 

Zeitung


Allgemeine

 

Literatur

 

estimate

 

account

 
included
 

climate

 

proposed

 

extinction

 
species
 

explained