fine grained sandstone, W. — granites, syenite, hornblende 

 granite, diorite, Slieve Gallion — Carboniferous conglomerate, 

 South — sandstone, probably Lower Carboniferous strata — 

 crushed pegmatite. 



LXXIV. Drumaneway, Esker two miles west of Randalstown. 

 Erratics : — Riebeckite rock, coarse and fine, Ailsa Craig — 

 rhyolite, probably Templepatrick. 



LXXV. Dervock, Carncullagh Gravel-Pit one mile to East. 

 Erratics : — Riebeckite rock, Ailsa Craig, N.E. — rhyolite, S.* 

 Ballycloughan — pink granites, mica felsites, gneiss, mica 

 schists, quartz schists, fine granite, quartzites, granite and 

 quartz vein, probably from N.E. — granite, felsite with quartz 

 and mica, sandstone, felsite from N.E. or S.W. 



LXXVI. Ballymoney, very small Gravel-Pits. Erratics from 

 Seacon, N. : — Rhyolite from South,* — felsite, quartz-felsite, 

 N.E. — felsite, altered rhyolite, N.E. or South. Erratics from 

 Heagles : — Rhyolite from South Ballycloughan (Quarrytown) 

 — chalk with manganese dendrites, granite, granulitic felsite, 

 felsite, ironstone, quartzite, probably from N.E. Erratics from 

 1 >allybrates : — Ferruginous sandstone, gneiss, felsite, red granite 

 from N.E. Another small pit near (Darcus') consisted almost 

 entirely of basalt boulders in a stiff matrix, but sandstone, red 

 granite, and flint recorded, from N.E. or S.W. 



LXXVII. Macfin, Gravel-Pit right bank of Bann near Macfin 

 Station. Erratics : — Granites, diorites, aplites, quartzites, 

 felsites, N.E. — flint, quartz. 



LXXVIII. Coleraine, Hillman's Fancy, large Sand-Pit near 

 Railway Station. Erratics : — Riebeckite rock, Ailsa Craig — 

 pink granites, porphyritic granite, crushed felsite, pegmatite 

 vein in granite, N.E. — diorite, granite in diorite, andesite, 



*A further confirmation of Mr. Maxwell Close's reading of strialions at 

 Seccaun Quarry and ( 'ullybackey, see Madame Christen's Summary of Glacial 

 Investigations, Appendix VII. to Vol. II., Proceedings B.N.F.C., 1905-06, 

 P- 3 2 5- 



