3. A zone of glendonite pseudomorphs at 1,480 feet 

 (approximately) below the same point. 



I am indebted to Mr. W. S. Dun, Government Palaeon- 

 tologist and Lecturer in Palaeontology at the University of 

 Sydney, for the following list of fossils collected by me 

 during a hurried visit to the section described above. The 

 list is far from complete, fossils being very abundant and 

 well preserved in the belt immediately overlying the 

 En rijdcsma zone. 



In the Upper Marine Glacial Sandstones : — Stroplialosia 

 Cbivkci; Eurijilcsuui hoburtcuse; Dcliopcclcn xiibijitin- 

 quelineatus; Prodnctus brach ntluvrux : h'cucstclln (!) 

 fossula; Clurnomiia hHlicvhhjri: Mm-l ini<>i>sis submdiatu 

 (var.) ; Mceonia cavhuita (var.). In a largo erratic of 

 Silurian limestone : — Favorites gothlandica traces of a 



I 2 Photographs of a block of gla< 

 jreserved Eurydesma hobartense. 



