A STUDY OK THK COW MAY UKACHKS. — D. S. MclNTOSH. 



113 



of granite from the district to the iiortii. I'Vcjin tli'- croilcd 

 part ail the finer material has been washed away by the 

 waves, and but the coarsest remains. The bouhiers in this 

 part of the site, moreover, are not rounded by the waves, but 

 are typically jilacial, and they ajipear not to have been 

 moved from their positi(ju in the drumliii, excei)t in so far 

 as they have fallen from an upper level to a lower. A boulder 

 bottom thus frinu;es the seaward end of the partly eroded 

 drumlins. West of drumlin B about five hundred yards 

 along the beach is a drumlin site C as indicated by the boulder- 

 covered bottom. Nothing but the coarser material remains. 

 A few yards further along towards the west is another drumlin 

 site D. The area that forms the south-western boundary 

 of Cow Bay is also fringed seaward by a boulder-strewn 

 bottom, the remains of a former glacial mound E. 



I'K;. :;. — I'k\( HKS — MoiKKN, KILI, LINKS; OI,U, DOITED LINh;- 

 HR(>U.\BLE BAKLY BK.VCH, DOT A.VD DA.SH LINK. 



