162 



Some other ^Mce//a-forms were also found; two left valves 

 bear some resemblance to Aucella Pallasii^ Keys. The Aucella- 

 shells are abundant in a light-grey calcareous marl. Casts and 

 impressions oi Aucella concetitrica, Fisch, var. rugosa, Keys, occur 

 in various sizes in the quartz-sandstone. 



On the south coast have been found (in the fine-grained 

 sandstone): — 



Ostrea sp. ind. in great abundance. 

 Goniomya V-scripta, Sow. sp. 

 Myacites sp. ind. 



Modiola sp. cf. Strojeskianus, d'Orb. sp. 

 Aviciila Miinsteri, Goldf. sp. 

 Belemnites cf. fusiformis, Qu. 



(in the coarse-grained shelly sandstone): — 



TricMtes, Lycett ? 



Patella cf. Aîibentonensis, Arch. 



Patella sp. ind. 



Nerita cf. hemisphœrica, Rom. 



Trochus sp. ind. 



Spines of Echinodermata. 



The Jurassic deposits of Jameson's Land were examined 

 later by N. Hartz and Edv. Bay during the Danish expedition 

 to East-Greenland, undertaken in the years 1891 — 2 under the 

 leadership of C. Ryder ^). Bay reports that Rhaetic and Jurassic 

 beds have been found along Hurry's Inlet in Jameson's Land 

 and that similar beds may possibly crop out also on the west 

 side of Jameson's Land. The western shores of Hurry's Inlet 

 consist of high, steep chffs, the so-called Neill's Cliffs, which 

 have their beginning southward at Cape Stewart and rise grad- 

 ually to a greater elevation towards the north. Bay is of 



^) Bay, Edv. 1896. Geologi. Meddelelser om Grönland. Hefte 19, p. 163. 



