the Horton-Windsor District, N. S. 



157 



agents of erosion is evident from the maintenance and 

 rapid undercutting of cliffs. It is only in favored locali- 

 ties, such as over alluvial flats bordering the upper limits 



Tria55ic 



%nn5)//m/c 



k/indsor 



Clie^ene 



Morton 



5//ur/an 



Pr^-Ca 



Oran/t^^ 



Fig. 1. Geological map of Horton-Windsor district. Scale 4 miles — 1 inch. 



of tidal action, that extensive aggradation has taken 

 place, with the formation of estuarine plains such as that 

 of Grand Pre in the north of the district, the historic 

 ground of the early French settlers. 



