GEOLOGY OF THE TORONTO REGION 
sible, turning south to the beach and walking east 
along the foot of the cliffs; or, second, by taking a 
King Street car to the Woodbine, and then a sub- 
urban car on Kingston Road to Stop 32. A lane 
leads two-thirds of a mile south to the cliffs. 
Lambton Mills, to the northwest of Toronto, may 
be reached by taking a Dundas Street car to West 
Toronto and then a suburban car to Lambton Mills. 
An old gravel bar, belonging to the Iroquois beach, 
runs westwards almost.to the Humber. South of 
Lambton Mills along the Humber River there are 
good exposures of Lorraine shale, and also for two 
miles up stream on the west side. 
Excursions out of town may be made by C. P. R. 
northwards to Forks of the Credit, where there is an 
excellent Silurian and Ordovician section on the 
escarpment; and to Longford and Washago, or Parry 
Sound; or by G. T. R., C. P. R. or C. N. BR. to 
Muskoka, where Archaean rocks are displayed. 
One can go by rail or steamer to Hamilton, forty 
miles west of Toronto, where the Iroquois beach is 
finely displayed, and the escarpment exposes a Silur- 
ian section; and one can go east by C. N. R. or 
G. T. R. along the old Iroquois shore, with the hills 
of an interlobate moraine rising to the north. 
One can cross Lake Ontario to the Niagara River 
and go by electric railway to the Niagara Gorge and 
Falls. 
For details in regard to these excursions one is 
referred to the special guide books. 
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