348 HT. Y. Hind on the Laurentian and 
bay of Chaleurs to the boundary line between New Brunswick 
and Maine are supposed to represent the Laurentian and are 
described in my Report on New Brunswick, published in 1865 
(pp. 42-52 
ena 
Dawson to be foreshadowed with some degree of accuracy ; and 
it is proper to repeat here Dr. Dawson's first paragraph o 
i Map” :— 
edition, though greatly improved, is still to be regarded as 
merely a rude approximation to the truth, and the colorimg ™ 
many places, more especially in the interior, remote from the 
coast lines, is little more than conjectural.” ; 
In various parts of “ Acadian Geology” reference is made to 
rocks which were suspected by Dr. Dawson to be older than the 
Lower Silurian slates and quartzites. (See particularly page 620, 
granitoid gneiss on which they rest, with the Laurentian. 
Dr. Sterry Hunt visited Nova Scotia in November, 1867 ie 
the purpose of making some observations on the gold-bearmg 
o* i Pasiaces ott ths Geology and Mineralogy of Nova Scotia: by Abraham Gesnet; 
-_ $ Acadian Geology, Ist edition. 
ree sae stroenee Peposesie ge = Co., penn ae 
_F Geological Maps of Canada ‘and the adjacout regions, 1869; London, Baward 
