324 
[B.N.F.C. 
by Miss Andrews at Portstewart and at Kilkeel, by Mr. H. J. 
Seymour, F.G.S., away down at Waterford and Youghal, and 
by Messrs. W. B. Wright, B.A., and H. B. Muff, B.A., F.G.S., 
at Whiting Bay and other Coik localities . 4 
Its absence from io of our localities is worth analysing, as 
in some cases this seems to tally with other circumstances sug- 
gesting a special period for these deposits. Although none was 
found at No. II., a drift-filled valley on Fair Head, fragments 
occur as loose drift half a mile away. Gleno, VI., Cave Hill, 
XV., and Divis, XIX., are small deposits of very local rocks ; 
Wolf hill, XVIII., and Dungannon, XXX., have not been fully 
investigated, and Killough, XXXIII., and Bloody Bridge, 
XXXV., have special features suggesting that they may be the 
product of later local glaciations. Although none was found in 
Castle Espie, XXVIII., boulder clay, fragments are frequent as 
loose erratics on the shore of Strangford Lough, XXIX., and 
Mr. J. O. Campbell found an isolated morsel on Spinkwee moun- 
tain in the Moume range. In spite of careful search, Mr. Bell 
never found any west of the Bann until this year, when he 
picked up a solitary piece on the shore of Lough Neagh, near 
Moyola River. 
Passing southward to No. III., the esker ridges about 
Killagan and Glarryford, we have another very important sign 
of an unsuspected iceflow to 1 the N.N.W., in the frequent occur- 
rence of Templepa, trick rhyolite, the latter place lying some five 
and twenty miles S.S.E. W^e found rhyolites also at Bally- 
mena, IV., near Cookstown Junction. IX., in boulder clay at 
Macedon, on the western shores of Strangford Lough, and away 
down at' Newry, XXXIV. 
Turning for a moment from, the rhyolite fragments m 
Killagan eskers, let us read an extract from Mr. Maxwell Close’s 
4. See Geology of Cork and Cork Harbour, Drift Memoir. Geol. Surv., 
1905, p. 105, etc. 
Also Proc. Hoy. Dub. Soc., Vol. X., Part 2, p. 269 (1904). Pre-Glacial 
Raised Beach. W. B. Wright, B.A., and H. B. Muff, B.A., F.G.S. 
