448 On Rain-fall at different points on the same Mountain-Range. 



Mr. Beardmore in 1846 and 1847, corresponded to an effective 

 depth of rain-fall somewfiat exceeding that at the rain-gauge F. 



14. I do not bring forward the limited number of observations 

 and comparisons here recorded as possessing any great value in 

 themselves, but as capable of contributing to the attainment of 

 useful conclusions when combined with other data of the same 

 kind. 



Table I. — Comparison of Rain-fall by periods of Bain. 



Table III. 



