PAINKANDA SECTIONS. 



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o:i • .. B sides of the Pethathali and Silakank streams, 



Suunans on the as- f 



cent to Niti pass. the gorge of the Ganes Ganga between the as- 



cent to the Niti Pass (see fig. 16) and the junction with the Silakank 

 stream is also composed of rocks belonging to the silurians. The 

 beaten track which leads to the Niti Pass within this gorge travels 

 over fans composed of debris of silurian rocks. Near the halting 

 ground Ganes Ganga, the middle silurian quartzites are well exposed 

 and yielded some few fossils chiefly Orthis. 



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