TABULATION AND DESCRTPTION OF NEW DATA 



225 



dor ice-slieet reached tlie ]>eninsiila, and the local ice-hodies were prob- 

 a.hly thin and short-lived. On the other hand, Newfoundland, larger in 

 area and farther north, held a massive glacier with effective weight. 



Examination should he made of the Cape Canso district and the east 

 part of Cape Breton. The Nova Scotiaii region is a critical area for 

 (•liecking tlie relatioji of the glacier to the diastrophic movements. 



Altitude!^ of the earliest and highest Marine Levels 



Location. 



Sti'oain valley aud station. 



'V 

 •43 0^ 





01)S(M-v('(l altitudes. 



Defi- I Ap- 

 nite. 1 prox. 



xMini 

 mnni 



Ocean shore Yarmouth to Liverpool 



Lahave River Bridgewater 



Mahoiie Bay Chester 



Saint Margaret Bay. . . . Hubbard 

 Halifax Harbor Halifax 



Annapolis Valley 



Digby 



Annapolis . . . . 

 Lawreneetown 

 Aylesford . . . . 

 B(M•^^'iek 



Oaspereau River Gaspereau 



Saint Croix River Newport . . 



Kennetcook River Kennetcook 



Salmon River Truro 



Philip River Oxford Junction. . . 



Maccan River Springfield Junction 



East River New Glasgow 



West River Antigonish 



South River South River 



About George Bay Pomquet 



Tracadie 



Monastery 



Denys River, Cape River Denys 



Breton. 

 On Bras D'oi* Lake Orangedale 



McKinnon Harbor. 

 Saint Andrews Channel. Slienacadie 





 25 

 50 



55 



50 



105 

 115 

 120 

 125 

 125 



120 



110 



100 



90 



150 



165 



80 

 50 

 45 

 40 

 30 

 25 

 10 



15 



10 



5 



138 

 125 



100 



85 



160 



125 



85 



23 



20 

 75 

 50 

 53 

 60 

 50 



125 



100 



90 



200 

 125 



10 



45 

 90 



iio 



95 



'85 



150 



30 

 22 

 30 

 25 



12 



