FREE BOOKS

Author's List




PREV.   NEXT  
|<   937   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   >>   >|  
John F. W. Herschel in his Discourse on Natural Philosophy, published in 1830. In preceding works the gradual diminution of the earth's central heat was almost the only cause assigned for the acknowledged diminution of the superficial temperature of our planet. [166] We are indebted to Baron Alex. von Humboldt for having first collected together the scattered data on which he founded an approximation to a true theory of the distribution of heat over the globe. Many of these data were derived from the author's own observations, and many from the works of M. Pierre Prevost, of Genera, on the radiation of heat, and from other writers.--See Humboldt on Isothermal Lines, Mamoires d'Arcueil, tom. iii. translated in the Edin. Phil. Journ. vol. iii. July, 1820. The map of Isothermal Lines, recently published by Humboldt and Dove (1848), supplies a large body of well-established data for such investigations, of which Mr. Hopkins has most ably availed himself in an essay "On the Causes which may have produced Changes in the earth's Superficial Temperature."--Q. Journ. Geol. Soc. 1852, p. 56. [167] Sir J. Richardson's Appendix to Sir G. Bach's Journal, 1843-1845, p. 478. [168] Malte-Brun, Phys. Geol. book xvii. [169] On Isothermal Lines, &c. [170] Rennell on Currents, p. 96. London, 1832. [171] Ibid. p. 153. [172] Ibid. p. 25. [173] Scoresby's Arctic Regions, vol. i. p. 208.--Dr. Latta's Observations on the Glaciers of Spitzbergen, &c. Edin. New Phil. Journ. vol. iii. p. 97. [174] Rennell on Currents, p. 95. [175] Humboldt on Isothermal Lines. [176] Journ. of Travels in S. America, &c. p. 272. [177] Darwin's travels in S. America, p. 271. [178] Mr. Hopkins raises the question whether, in South Georgia, the descent of glaciers to the margin of the sea might not have been mistaken by Capt. Cook for the descent of the snow-line to the sea level. Quart. Journ. Geol. Soc. p. 85, 1852. The great navigator is generally very accurate, and there seem to be no observations of more recent date either to confirm or invalidate his statements. [179] After all these modern discoveries, the area still unexplored, within the antarctic circle, is more than double
PREV.   NEXT  
|<   937   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   >>   >|  



Top keywords:

Isothermal

 

Humboldt

 

America

 

observations

 

Hopkins

 

descent

 
diminution
 

published

 
Rennell
 

Currents


Travels

 
Spitzbergen
 
London
 
Observations
 

Regions

 
Scoresby
 

Arctic

 
Glaciers
 

Georgia

 

confirm


invalidate
 

statements

 

recent

 

accurate

 

antarctic

 

circle

 

double

 

unexplored

 
modern
 

discoveries


generally

 

glaciers

 

margin

 

question

 

raises

 

Darwin

 

travels

 

navigator

 
mistaken
 
collected

scattered
 

indebted

 
founded
 
approximation
 

derived

 
author
 

theory

 

distribution

 

Philosophy

 
preceding