43 
(54) East side of Roberts bay 650 yards from the north end, also 
(55) Islet, 100 yards west of the last locality, also 
(56) West shore of Long island, 2f miles south of the north end of 
that island, also 
(57) East shore of Long island, 3| miles in a straight line from the 
north end of that island. 
Aucelhs, QiTon^y sheared and so unidentifiable, but probably the sharp ribbed 
species of the canadiana zone 
(58) West side of Long island, barely 2 miles south of the north end 
of that island. 
Aucellae, considerably crushed and so unidentifiable with certainty, but never- 
theless very probably Ancella crassicollis Keyserling 
(59) North side of Twentymile point, one-quarter mile from the 
point, also 
(60) West shore of Harrison lake, one-half mile south of Rock point. 
Pelecypoda, unidentifiable fragments 
"Belemnites” sp. indet. 
(61) Cut bank on south side of main line of Canadian Pacific railway 
838 yards west of the west end of the Harrison River bridge. 
Strongylocenlrolus drobachiensis Muller 
M ytilus edulis Linnaeus 
Terebratalia tramversa Sowerby? 
Balanus crenatus Bruguiere 
(62) Cut bank on south side of main line of Canadian Pacific railway 
750 yards west of the west end of the Harrison River bridge. 
Saxicava rugosa Linnaeus 
Other pelecypoda, indeterminable fragments 
DESCRIPTION OF FOSSILS 
Phylum, ECHINODERMATA 
Class, CRINOIDEA 
Order, Camerata 
Family, mblocrinidae? 
Genus, (?) 
Fragments of large stalks, 10 to 27 mm. in diameter, the joints of 
which exhibit the structure and intercolumnal spaces of those of this 
family. They are imperfectly preserved and do not admit of complete 
study. 
Locality. West side of Bear mountain at 2,000 feet elevation, 1^ 
miles due east of Harrison Hotsprings hotel. Similar crinoid stalks are 
common at the type locality of the Chilliwack series on Chilliwack river, 
also in the Pennsylvanian rocks of Kamloops district, British Columbia. 
