140 SUPERFICIAL GEOLOGY—HONEYMAN. 
clays, having the characteristic shells of the formation. Vide 
Museum Collection. The axe could not have come out of this 
underlying marine bed. This by the way. 
Our collections contain many axes now associated with it. 
These are Nova Scotian. One of them I found in the town 
of Dartmouth. Another with a groove was picked up by a 
boy and presented to the Museum. Our Glacial accumula- 
tions are not far from where the first was found. The last was 
found in a pile of stones above one of these accumulations—not 
in it. 
A magnificent and beautifully-formed spear head has on it 
an inscription which informs us that it was found in an Indian 
grave more than twenty years ago. Sheriff Hill, of Antigonish, 
and I collected stone arrow-heads both well and indifferently 
shaped, at Ogden’s Pond, on George’s Bay, near our Eastern Gla- 
cial terminus. ; 
In Lunenburg County, at Bachman’s Beach on the Atlantic, 
and six miles North of the “Ovens” Gold Diggings, an arrow- 
head maker’s factory was discovered about 1874, Of the first 
collection the late Mr. Lewis Anderson, merchant, Lunenburg, 
presented to our Museum 202 specimens Jasper arrow-heads of 
elegant form and beautiful chips of agates. There are also 
arrow-heads of quartz and porphyrite. Many of them were 
broken in the making. Of these the pieces have been fitted 
together. Associated are needles and other rude implements 
with nuggets of native copper, such as is found in the Triassic 
(T) igneous rocks of Cape d’Or, or Margaretville. Since the dis- 
covery many have gone to the locality and collected specimens, 
and the supply seems yet to be unexhausted. 
We have another collection of Jasper arrow-heads and chips 
from another locality, in Cornwallis, King’s County. The work- 
manship is much inferior to that of the preceding. 
All the implements are of the same character. They corres- 
pond with those of Abbeville. Ours, however, cannot be older 
than early recent. 
4.—-Pre-glacial ? 
This division seems to be represented in the Cobequid Moun- 
tains, as I observed in my examination of the sections of the In- 
