Wright— Foraminifera of North-East of Ireland. 
f Estuarine Clay of brownish colour and with offensive smell ; 
„ , . ^ Foraminifera very common— Miliolina oblonga, Trocham - 
Estuarine Clay, j ■ ■ n * , r , 
22 feet. } mina m J iata ( y ery fine), macrescens, Lagena lucida, Poly - 
j morphina lactea, Rotalia Beccarii , Polystomella striato - 
^ punctata ,. Nonionina depressula. 
Fine Sand, 
24 feet. 
Boulder Clay, 
50 feet. 
’Fine Sand; Foraminifera rare, possibly washed in from the 
overlying Estuarine Clay during the sinking of Well— 
Trochammina inflata, Rotalia Beccarii, Polystomella striato - 
„ , punctata , Nonionina depressula. 
j Clay very fine ; Foraminifera very rare —. Rotalia Beccarii, 
( Polystomella striato -punctata. 
Boulder Clay, 
100 feet. 
■ Boulder Clay as it usually occurs in our neighbourhood ; 
Foraminifera plentiful — Miliolina seminulum, Lagena 
■{ 14 illiamsoni, costata, lucid a, melo, Globigerina bulloides, 
Cassidulina ctassa, Rotalia Beccarii, Polystomella striato - 
punctata, Nonionina depressula. 
4. Estuarine Clay exposed in the deepening of Mr. MacLaine’s dock 
Corporation Street, Belfast, 1879. 
5. Magheramome— Estuarine Clay on the West shore of Larne Lough— 
An extensive bank of this clay occurs along the shore, a few hundred yards 
south of the ferry-slip, close to the railway station. Lagena striato-punctata, 
now one of our rarest British Lagenas , occurs here in abundance, as also at 
Limavady Junction. Shells and Foraminifera are abundant. 
6. Blackstaff Bridge, Strangford Lough, on Blackstaff River, about two 
miles South of Kirkcubbin and East of the road to Portaferry. 
7. Limavady Junction, Lough Foyle— Estuarine Clay slightly above high 
water, close to the railway station. To Mr. Gray is due the credit of being 
the first to discover Estuarine Clay at this place, as also at Blackstaff Bridge. 
The clay is exceptionally rich in Foraminifera. A few Polycistinse were found 
here. 
