FOLDING AND FAULTING 



363 



not very clearly shown except by the areal distribution and contiguous 

 structural details. These faults, as shown on the general map, lie in a 

 curved line passing from the Little Gunpowder near Hess to the valley 



S-S-r^sS Hranite 



C t* Y ST ALL* W£ 



^^^? ^>-^% ^-v^<H Limestone. 



S^ v CS . ^J H I C KQV SCH I S T. 



set TEff's 



<}UART2ITE. 



LEGEND. 



/— -V 



WISSA HICKOI 



SCHIST. 



LJ 



n 



m 



M 



PSEyoo- 



6A LTiMOKE 

 GW El SS. 



z 



Line. 



SECTio N 



LINE. 



Dip A n D 



S THIKE. 



■S 



SECTION ALONG LINE AB. 



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Figure \.—Map of Vicinity of Warren. 



of Jones falls in the vicinity of Mount Washington. They are all in the 



nature of thrust faults, but the almost complete absence of anything 

 approaching contacts renders it difficult to demonstrate this fact, There 



XLIX— Bull. Geol. Soc. Am., Vol. 10, 1904 



