BULL. GEOL. SOC. AM. 



VOL. 23, 1911, PL. 16 



FiGLKE 1. IX THE FuKEGlJOl XD. THE CO.Ml'LETELY DIS.SECTEU CHAUAC'TEU OF THE 



Topography 

 The liills rise rapidly toward tlie rear, as the limestones and dolomites are a])i)roaehed 



Fkmkk "J. —A TVPicAi, Khxm: wrrii an aemust nouizoNrAL Si M.Mir Lim: 



It is [jraetically in aliiiiiincnl wilh llie ;;r(>a1er nnmhers of llie liill ami ridp' lojis in the 



district 



DISSECTED CHARACTER OF THE TOPOGRAPHY IN AREAS OF THE MESOZOIC BEDS 



