75 S. Kawasaki 



several seams of hrown coal. The younger Tertiary is marine, being 

 made ti]) of conglomerate, sandstone, shaJe, tiitf, and flows of volcanics, 

 rarely with thin seams of brown coal. It is always horizontal and 

 covers tlie older Tertiary or still older rocks miconformably, the dips 

 being different. 



Quaternary:— It is always found in a horizontal jjosition, con- 

 sisting of beds of gravel, sand, clay and i)eat, often associated with 

 basalt flows. These beds, occupying plateaus or elevated jdatforms 

 as Avell as older terraces, and often being associated with basalt 

 flows, are regarded to be Pleistocene in age, while those spread 

 along the plains bordering rivers or seacoasts are considered to be 

 Recent. 



