THE MAGOTHY. 35 



3 inches thick, which was filled with fossils. This mass of sand- 

 stone, collected along 1 with the crustacean nodules, was not in 

 situ, and being different in its lithologic characters from any 

 material observed imbedded in the clay at this point, it may have 

 been transported to this locality from elsewhere. It is somewhat 

 similar in its lithologic characters to certain sandy, fossiliferous 

 nodules occuring 1 in the clay pits of the Cliffwood Brick Com- 

 pany, a little over 1.5 miles distant, on Whale Creek. The fauna 

 yielded by this standstone undoubtedly indicates its Qiffwood 

 age, although several species occur which have not been observed 

 elsewhere. The species identified are the following: 



PELECYPODA. 



Leda cliff wo odensis n. sp. 

 Yoldia cliff wo odensis n. sp. 

 Trigonarca triquetra Con. 

 Trigona-rca cliff wo odensis n. sp. 

 Axinea congest Con. 

 Anatina sp. undet. 

 Cardium cliff wo odensis n. sp. 

 Isocardia cliff wo odensis Weller. 

 Cymbophora lintea (Con.). 

 Corbula cliff wo odensis n. sp. 

 Corbu-la jerseyensis n. sp. 



GASTROPODA. 



Gyrodes sp. undet. 

 Turrit ella jerseyensis n. sp. 

 Anchura pergracilis Johns. 

 Herchorkynchus jerseyensis n. sp. 

 Volwtomorpka kanei (Gabb) ? 



Locality 186. At Geldhaus' clay pits, a little over i mile west 

 of Cliffwood Point, on Whale Creek, crustacean-bearing nodules 

 similar to those collected on the beach at Cliffwood, occur in situ 

 in the clay. Besides the numerous imperfect crustacean remains, 

 the following species have been recognized at this locality : 



