104 F00TE : GEOLOGY OF THE BFLLARY DISTRICT. ^ 



8. Schists, green. 



7. Trappoid rock, black. 



6. Schists, dark, nearly vertical. 



5. Slates, greenish, badly cleaved. 



4. Schists, green, silky texture. 



3. Schists, green, coarse. 



2. Haematite rock, poor. 



Gap. 

 1. Schist, dark. 



Talus. 



Bed 15 forms the western scarp of the ridge overhanging the cen- 

 tral valley opposite to Hunshahuti. 



The next important section occurs rather more than four miles to 



the south-east in the most easterly of the three 



ravines lying south of the village of Joga. 1 The 



rocks show up well nearly everywhere along this section, and the gaps 



caused by superficial deposits are so small that they may be safely 



ignored. The section extends in descending order from the foot of 



the main northward to Joga valley, a distance of about 2\ miles, and 



practically follows the line of the path, which is very fairly straight. 



The following is the sequence of formations exposed : — 



25. Trappoid. 

 foga low- 24. Schist, dark-chocolate, reddish, or banded, 

 level sec- 2 « argillaceous. 



22. Trap, a thick contemporaneous flow. 



21. Schist. 



20. Conglomerate, thin. 



19, Schist, argillaceous. 



18. Conglomerate, thin. 



17. Schist, argillaceous. 



16. Conglomerate— Schisty micaceous matrix, thick; enclosed pebbles 



altered by pressure. . 

 15. Schists argillite ? 

 14. Haematitic (thin). 

 13. Schists. 



12. Haematitic (very thin). 

 11. Schists. 

 10. Trap (thin). 



9. Schists. 



8. Haematitic (thin). 



1 The map (sheet 58) shows only two out of the three torrents which unite at 

 Joga : the central one has been left out, and the course of the western one is incorrectly 

 given. 1 



( 104 ) 





