GEOLOGY OF ANTIGONISH COUNTY—HONEYMAN. SEG 
f CARBONIFEROUS. 

Igneous. Trap. Middle & East Branches of 
z Conglomerate. Doctor’s Brook. 
3 OSES ITICON OO ee 
a SILURIAN. 
e | “Powiliferons,* Lowery ¢ Bi] de. ol...) ole 
3 4 Adar 0 A eS Me oe 
a | per OCtes ile Ons MAM rg ae A abc Ase | 
ae te Men emrneeer: Synclinal awis........ 
S | Lower Srurtan. [By genital bh zon « 
2. ene A | Road sl ae 
L. Stturtan, Metamorphic. al ......2-.2250 502 eee: 
| Carpontrerous, Igneous. Trap. ...-.-...2seeee estes 
REMARKS ON THE ABOVE, 
1. Archzean of McNeil’s Mountain does not appear to the west, 
of the Mountain. It stretches out northerly towards the shore 
section so as to approach the Archzean of the section. A singular 
syenitic porphyrite which occurs in the mountain is also seen in 
sections about ? of a mile to the north; occupying the space that 
2, 3, 4, 5 Cambrian ? of MceDougall’s Mountain would oceupy is 
extended eastward, The latter (Cambrian ?) extends westward 
beyond the county line. 
6. Lower Silurian extends eastward and is parted into two 
by the associate igneous diorites. One part passes to the north 
of the 1 Syenitic, terminating, apparently, on the back of the 
Malignant Cove and Brook, Sugar Loaf (mountain) constituting, 
with the igneous diorites, the rocks of the mountain. The other 
part comes to the front in a prominence not far from the road 
to McNeil’s Mountain. After being much shattered, it terminates 
like a ved vein. With diorites the same red argillites extend 
westward, suffering displacement or being faulted and conse- 
quently thrown out of line and seems to terminate in a mountain 
south of Arisaig Pier, unless certain red slates that occur to the 
south of MzAra’s Brook on the side of a branch of Bailey’s 
Brook be the termination. This may be the western termination 
