the congiomer- 
ae over the shale. These reveal, at the depth of thirty feet, 
Nearly six inches width of a richer and more beautiful coal than 
the Albert, gradually thinning out to the width of coarse paper 
atthe surface, and most unequivocally cutting vertically across 
nearly horizontal layers of sandstone. As before, we have here 
we phenomena of shifts constantly working the vein southward, 
and a slight leaning in the same direction. Following the line 
to the Petiteodiac, there are seen other openings upon the vein of 
extent, 
0 veins crossing the anticlinal are very ss ae 
gs tiv 
Upon parallel lines about a mile apart, their course is N.E. an 
the 
branch 
ha them are branching threads of the same material, joining 
sea are 
ateral seams at various angles. I think there 
area of tin veins. Like the others, this vein-field leans 
: slightly southward. It will be interesting to watch the develop- 
Ale of these veins to see whether they will develop like the 
ie rt shaft where the coal is nearly six inches wid 
foregoing and kindred facts. 
e. 
from voy the following conclusions may be drawn legitimately 
