m. 2.] STRATIGRAPHIC RESULTS. 123 



of 400 ft., and on July 12th, at the margin of the glacier, at a height of 

 100—200 ft. above the sea. As some of these nodules, from the fossils 

 they contained, viz. 



Belemnites sp. indet. 1. 



Cadoceras sp. indet. (? Cad. Elatmm and others) 



Serpula flaccida Goldf., 

 were recognised as Lower Callovian, it seems natural also to refer the far 

 more numerous nodules without fossils to the Lower Callovian. Thus from 

 their occurrence in Windy Gully, the phosphoritic nodules would be confined 

 to a height of about 400 ft. above the sea. 



2. Cone-in-cone (Tutenmergel, Nagelkalk). 

 Several pieces were found loose on the talus on July 10th, NNW. 

 of Elmwood, 100 ft., and on July 12th, at the margin of the glacier, 100 

 to 200 ft. above the sea. Petrographically the pieces agree perfectly with 

 the stone marl of the Middle Callovian (with Cadoceras Nanseni n. sp.). 

 Possibly for this reason, they also belong to the Middle Callovian. No 

 pieces were observed in situ. Judging from their occurrence as debris on 

 the edge of the glacier, at a height of about 200 ft., they must have been 

 in situ at a higher level. 



After becoming acquainted with the faunistic representatives of the entire 

 Callovian, in the "clay formation" below the basalt at Cape Flora, the next 

 point is to establish the age of the rocks and fossils of locality 1. 



On Aug. 2nd, 1896, Professor Nansen found in situ at 

 Elmwood NW. from the hut, at a height of 23—33 ft., 



hard, gray, sandy marl (with small agglomerations of pyrites), together 

 with light gray, soft marl (cf. p. 11 "Lower horizon," Letter-press fig. 2, 1 a 

 and p. 47. No. 4). 



The material which Prof. Nansen collected at this locality contains: 

 Lingula Beani Phill. 

 Discina reflexa Sow. sp. 



„ sp. indet. 

 Pseudomonotis Jacksoni n. sp. 

 Belemnites sp. (cf. Beyrichi 0pp.) 



„ „ ( ? Canaliculati group) 



„ indet. 2(?). 



