370 W. E. Logan on the Rocks of the Quebec Group. 
gradually —— the band 3, and finally merge into it; but 
finding farther on, along the outcrops, an exposure of conglom- 
erate at z, reich a answer gost band 4, it is now conceived 
that there may be two layers of sandstone, one above and the 
other below the maaiaiven tient place of band 4; and though 
this band thins to —— at P, it may commence again in its 
— place farther o 
om the sieidhborhiood of the Temperance Monument, the 
orfienon of band 2 is traceable northeastward, running not quite 
parallel with 8,+to the fault, and thence across the St. Joseph 
Church road to the main road. It traverses this obliquely, a 
little beyond the church, and its turn upon the synclinal axis is 
seen on the north side of the road, about 400 yards beyond. In 
the limestone of Guay’s quarry there is a small notch-like turn, 
= serves to augment somewhat its apparent volume; a cor- 
nding twist is more conspicuous in the outcrop of band 3, 
in band 2 it assumes a still further prominence at hese 
aacteaalve forms indicate a plait in the stratification, commencing 
at the quarry, and ra “eile augmenting northeastwardly i in the 
space of 350 yards. ortance of its effect on the dis- 
tribution of the strata ety at this rate of increase, soon 
me considerable, and it serves to show some of the compli- 
cations of the neighborhoo d. 
Without going into detail, it is evident from the map that the 
Middle Ridge is an anticlinal form, and that the South Ridge is 
another. On this, the exposures of the bands 2 and 3 conspicu- 
ously mark the turn on the axis, as they do in the synclinal 
between the ridges. It will be poricrce that, between the 
synclinal and anticlinal axes, the outcrop of band 2 is repre- 
sented as showing a very sharp twist. The or of this is 
not quite satisfactory, and the apparent arrangement may possi- 
bly be due only to a swelling in the volume of the band, with 
parts obscured by drift. 
The esitinatine Monument stands on band 1, with which are 
associated some layers of sandstone. This band is easil 
to nthe iinet ihe across the fief Ste. Anne; = tween 
|e hence by the the church. ne test Seen 
