MORXE SECTIONS. 



59 



16. Micaceous slialy sandstone ... ..• 



17. Sandstone ripple-mavked 



18. Micaceous shaly sandstone and cla3^s alternating 



19. Shaly coal, with partings of shales 



20. Shales 



21. Flaggy sandstone and shales alternating ... 



22. Shaly coal 



23. Sandstone flags and shales 



24. Thick bed of sandstone, ferruginous and capped by bed 



of hasmatite (2") 



25. Shales with fossils 



26. Sandstone flags and shales 



27. Thick bed of sandstone 



28. Soft felspathic sandstone in irregular beds. 



Fault. 



28. Sandstone. 



Shales, &c. 



At first the dip is 15° north-west, but it increases to 20° north- 

 west within a short distance. 



.. .3' 



1" 







6" 



4' 





. 1' 



'J." 



. r 



4" 



. 3' 



6" 



0' 



6" 



. 18' 





. 2' 



10" 



. 4' 



8" 



. 25' 





. 1' 





21. — Sections in the Suidud, Kuhia, and Andhenia Nullahs and the coimtry 



ta£stwards. 



The sections along the Suidud, Kubia, and Andherua nullahs seem to 

 be equally affected by the parallel faults noticed in the Morne river, 

 for the Gondwanas there are completely shattered, and it is scarcely 

 possible to identify the beds. The only point I could settle with any 

 degree of certainty is, that the metamorphics south of these nullahs, 

 near Dand Karua for instance, are covered by a considerable thickness of 

 Talchir boulder.bed and shales; enormous boulders of lenticular shape 

 are scattered throughout the silty matrix of the Talchirs, many of them 

 being weathered out by sub-aerial denudation. Above Talchirs follow 

 the remains of Barakar sandstones, shales, and coal-seams. The Barakar 

 sandstone of the Suidud nullah, containing Noggerathiojisis hislopi, 

 Bunb., affords a very good illustration of erosion by water; large pot-holes 

 and narrow gorges are formed by the rush of the water during the 

 rainy season, as shown in the annexed drawing, fig. 3 : — 



( 187 ) 



