Vol. I. Sun — Cambrian Faunas of North China (iv) 11 



SHANTUNG PEOVINCE 

 A. Kao Li Shan. This a low hill, 2 li west of Tai An, is composed of limestone 

 conglomerate, limestone and shale. The lower part consists of unfossiliferous beds 

 occationally with wurmkalk, and probably represents a part of the Chaumitien formation. 

 The upper part is mostly of shale, limestone and limestone conglomerate which is unlike 

 the wurmkalk (intraformational conglomerate) of the Chaumitien formation. The follow- 

 ing section was made by the class of 1923 of the Geological Institute of the National 

 University under the direction of the author. 



Feet Inches 



25 conglomerate limestone (partly covered) F4 30 



24 thin-bedded limestone 6 



23 fine oolitic limestone 3. 5 



22 shale 2 6 



21 conglomerate limestone F 3 1 2 



20 Shale 2 6 



1 9 conglomerate limestone 1 



18 shale 3 7 



17 Obolus limestone F 2 1 



16 oolitic limestone 2 6 



1 5 thin-bedded limestone 9 



14 conglomerate limestone 4 



13 thin-bedded limestone 9 



12 oolitic limestone 4 



11 thin-bedded limestone 1 2 



10 compact and dark gray limestone Fl 1 



9 thin bedded limestone 11 



8 ochery limestone 2 3 



7 thin-bedded limestone 2 .8 



G ochery limestone 2 8 



5 thin-bedded limestone 2 8 



4 intraformational limestone 11 



3 ochery limestone 4 4 



2 thin-bedded ochery limestone 7 



1 intraformational conglomerate 20 



