82 JOURNAL AND PROCEEDINGS. 
Cornulites Flexuosa, Cornolites Bella Striata and another (probably 
new) which unfortunately is imperfect. It bears a near resemblance 
to the Teutaculite, figured by Dr. Hall from the Waverly beds, 
Caleolus Herzire. In addition to Crania Anna, already figured and 
described in the Niagara fossils of Dr. Speneer, I succeeded in 
securing the limpet-like dorsal valves of two other species, one of 
which may be Crania Siluriana, as it comes very near the description 
given ; the other differs from any known to me. 
The Ariculede, or Wing Shells, are also represented in the 
upper portion as well as the base of the chert beds. I forwarded to 
a well-known English Palzontologist some years ago a flint-flake 
containing an Aricula, naming it A. Emacerata. He appeared to 
doubt its precise agreement with the European specimen known by 
the name. Indeed, I inferred from his subsequent letter that he was 
rather inclined to look on ours as an American variety. 
Three species of Acidaspis put in an appearance in the chert 
beds, only one of which, I think, has been described ‘A. Halli” 
(Spencer). : 
I do not recollect ever seeing in any geological work a notice 
of the terminal Moraines along the Burton and Glanford stone road. 
One between the turnpike and school house could scarcely have 
escaped observation. It looks like an artificial mound such as we 
read of as occuring in the States. A few years ago a farmer opened 
a drain along the base, and exposed quite sufficient to satisfy me the 
great mass of boulders, sand and clay had heen deposited by a 
retreating glacier. What! Fresh water ice drop such a load as you 
see there? 
In the President’s annual address, published in one of our ex- 
changes (Bulletin Natural History Society of New Brunswick, No. 
XI), Prof G F. Matthews, alluding to modern faunas of oceanic 
tracts, points out: ‘‘ We see in contrast two groups of animals— 
those that inhabit the warm shallow seas and those that may be 
found in the deeper and colder parts of the ocean. As there are 
now tracts occupied by waters of different temperatures, so there 
were in the earliest Paleeozoic times, and this is shown by the re- 
mains of marine animals entombed in the rocks. In certain regions 
ee 
