104 EF. Andrews—Glacial Markings of unusual forms. 
resented in fig. 7, which is a diagram of the plan of numerous 
specimens seen along the eastern shore from Killarney to Parry 
7 Sound, a distance of a 
le Wyre a one hundred miles 
ge Dp, boss or knob of rock meats 
aa “Dr. ing above the general gla- 
Ma a p< “Ip ——FE—._ ciated surface in an oval form 
iis in fact, a roche moutonneé. 
The sp i 
about four feet high, fifteen 
= wide and thirty long; butall 
— sizes and irregular forms are 
common. ‘The observed spe- 
arr 
as the stri# approach and rise upon the surface of the kno 
they are nance to the right and left and sweep over it 
in an oblique course. This sort of curved deflection, partly 
over and partly oe obstacles is common to the whole coast, 
so that in many places almost all the striw are curved by the 
influence of the knobby surfaces of the gneiss and quartzite. 
TT are two unstriated scoop-marks having a length of about 
ten feet and a width of twelve inches. They begin vaguely 
near to each other, but not in contact, close to the northeast 
of the drift agencies in some fied determined the presence 
and direction of these scoop-ma 
The great belt of fifty-two saben islands, above pared 
to, varies from three to fifteen miles in width and is about 
hundred and fifty miles iong. Beginning at the St. Marie 
River it first outlines the north channel by the great Manitoulin 
group, and thence, passing southeast through Frazer Bay, con- 
finues along the whole east coast of Georgian Bay and termi: 
