WEATHER AND GLACIATION REEDS 



323 



shown that there is a real rchitioii between sohir radiation varia- 

 tions and weather chanjres; and, since weather atlecls the condiiion- 

 \nrr of fdaciers and is reflected in the varve fjraphs shown herewith, 



a suf^gestcd correlation of solar radiation weather and varved clay 

 variations is here proposed. 



CONCLUSION 



It may be stated that weather, as distinguished from climate, 

 affects the conditions of ice masses daily, seasonally, annually, and 



