Wright— List of Irish Cretaceous Microzoa 77 
9. Cave Hill, Co. Antrim. Quarries 2 miles N. of Belfast. 
On account of the close proximity of these extensive quarries to the town 
of Belfast, they have been better examined for Chalk powder than any of the 
other localities. In the rubbish heaps outside the quarries occur numbers of 
flints containing Chalk powder, rich in fossil Microzoa. Among the many rare 
forms found at this place the following may be mentioned as of special 
interest, viz.: Lituola ( Haplostichc) clavulina, Flabellina lingula , F. rugosa, 
and Lingulina carinata. 
10. Whitewell, Co. Antrim. Quarry 4 miles N. of Belfast, on the An- 
trim Road. 
The Chalk powder found in the flints in this quarry was rich in the usual 
fossils. Two very rare Foraminifera were found here, viz.: Marginulina 
seminotata, and Cristellaria ( Saractnana) Italica. 
11. Whiteabbey, Co. Antrim. Quarry 1 mile W. of Whiteabbey station 
on the Northern Counties Railway. 
The Chalk powder collected from this quarry contained the usual Chalk 
Ostracoda and Foraminifera, but very few Sponge spicules. 
12. Woodburn, Co. Antrim. Quarry at the head of Woodburn Glen, 
2| miles N.W. of Carrickfergus. 
I only once visited this quarry, and whilst there collected several pounds 
weight of Chalk powder ; it was found to contain Microzoa in great profusion. 
Many rare Foraminifera occurred, and all our Irish Chalk Ostracoda, with the 
exception of Cythere Iernica. Vaginulina costulata and Gaudrytna pupoides , 
va r. prcelonga , were among the rare Foraminifera found here. 
13. Whitehead, Co. Antrim. Quarry convenient to Whitehead station 
on the Northern Counties Railway. 
A small quantity of Chalk powder was collected at this quarry, it con- 
tained the usual Chalk Microzoa ; Frondicularia inversa has been found in this 
quarry. 
14. Blackhead, Co. Antrim. i£ miles N.E. of Whitehead station, rocks 
exposed along the shore under the headland. 
A few flints were met with at this spot ; they contained Chalk powder in 
quantity, which proved highly fossiliferous. 
