N0 . 2.] JURASSIC SEDIMENTARY ROCKS 49 



basalt at Elmwood on the southwest side of Gape Flora, Newton and Teall l 

 also mention clay sandstone in situ, about 50 feet below the basalt, that is to 

 say, at a height of about 550 feet above sea-level. The most important of 

 the clay sandstone fossils which Newton describes from this height, can be 

 identified with the clay sandstone fossils examined by myself. 



A very much weathered piece of clay sandstone was also found loose on 

 the talus on July 12th, 1896, 100200 feet above the sea, IVa klm. NW. 

 from Elmwood, cf. p. 17, "doubtful horizon". 



A small portion of the material before me consists of fossil fragments 

 without adhering rock. These pieces, at any rate to some extent, can be 

 recognized as having been weathered out of several of the types of stone 

 here mentioned. I shall return to these pieces in the last section of this 

 treatise. 



1 E. T. Newton and J. J. H. Teall, I. c p. 496. 



