252 GREAT SERPENTIXE-BELT OF NEW SOUTH WALES, VI., 



pebble-bands are frequent, quite parallel to the bedding-plane, as 

 is shown bv comparing the inclination of the sandy layers, thin 



^B&'^>€M:t^ 



Baldwin faull" Borah CreeW 



Text-fig. 8. 

 The Baldwin Fault, Borah Creek. 



intercalated beds of cherty material, or the underlying mudstone. 

 Continuing up Borah Creek, we may note the succession of well- 

 marked faults; the first brings the Barraba rocks down against 



O 

 CO 



Ground Plan Borah fault 

 E3 Slickensidecl layers oF Tuff 



Text-fig. 4. 

 Ground-plan of the Borah Fault, Borah Creek. 



the base of Baldwin agglomerates, and crosses the stream in 

 Section 24, Parish of Hobden (Text-fig. 3). Another very inter- 



