with Height in the Atmosphere, 



Table I. — continued. 



209 



Table II. — General Synopsis, 



I have compared the results of this Table, which are pro- 

 jected in the uppermost curve of Plate II., with the results ob- 

 tained on the far larger scale of a difference of level of 6836 

 English feet, between Geneva and the Convent of St Bernard, 

 as given by Kaemtz in the second volume of his Lehrhuch der 

 Meteorologie. Considering the different circumstances of the 

 two, these curves (which I have purposely reduced to a similar 

 range) approximate wonderfully. They both indicate a most 



