GLACIAL DISTRIBUTION OF ELEOLITE-SYENITE. 





from the eleolite-syenite, so that there is no probability of the latter be- 

 ing found at either place in situ. On the other hand, it is worthy of 

 remark that the bowlders in both instances are directly in the course 

 of the glacier* that passed over the region of South Litchfield. 



Another well known locality, especially for that phase of the rock 

 containing sodalite and Large crystals of eleolite, is at Spears Corner, in 

 West Gardiner, on the road from South Litchfield to Gardiner. On the 



FiouttEl— Map showing Distribution of Eleolite-Syenite in thi Town oj Litchj la IV tGardiner, 



Mai i 



northern side of the road and aboul one hundred yards from it. in a 

 clump of bushes near the bottom of a hill, there is a pile of Large blocks 

 resembling in their genera] arrangement the heap ;it South Litchfield. 

 Mosl of these were originally completely buried in the sand and soil 

 They are now well exposed through the active operations of collectors, 

 hut the soil around them has not been sufficiently removed to enable us 



»Cf. T. C. Chamberlin: Map of a Portion of the Terminal Moraiuo, in 3d Ann. Rep. 1 - 

 Survi 



