NOVA SCOTIAN GEOLOGY—HONEYMAN. 243 
renders mining easy and comparatively inexpensive. I have 
on my former visit noticed the stratum underlying with its 
arsenopyrite crystals. Large quantities of quartz were ready 
for the mill. 
From this we went to 
JEGOGGIN POINT. 
Between this and the mines no rock exposures were observed. 
At Jegoggin is found an interesting exposure. The rocks are 
chiefly micaceous schists. In these are quartz veins, large and 
small. One of the former is 10 feet thick. Interbedded are len- 
ticular masses of hornblendic rock with crystals arranged in 
stellar form. Some of these schists are full of small garnets. 
This series of garnetiferous and hornblendic schists is evidently 
a section of the schists of Lake George and the line of railway. 
The strike of the strata is N. 50 E., 8.50 W. We did not take 
time to collect the sand among the rocks. It must be garnet 
sand. 
I have thus, in a somewhat irregular manner, examined every 
important outcrop of rocks from Jebogue Point on the south to 
Meteghan Point on the north. I would now arrange the several 
outcrops in the form of a general section, thus: 
1. Jebogue Point. 
2. Sunday Point. 
3. Town of Yarmouth. 
4. Lighthouse Point. 
5. West Point. 
6. Jegoggin Point. 
7. Cranberry Head. 
8. Red Head. 
9. Beaver River (County Line). 
10. Salmon River to Cape Cove. 
11. Meteghan. 
Boundary Line of the two metamorphic series, auriferous and 
fossiliferous, in the Counties of Yarmouth, Digby and Annapolis, 
I begin at Cape Cove, making the extensive diorite with 
quartzite the starting point. Passing on to the line of railway 
