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S]ECTJ©r?S SHOWNT, THE MLATliOK oi' THE iKlBUVnifll. .1.VJ) ;"3AUC1;J :P)CI':I:,;Sin tiii: CffliLK m xirE IPliESJEKT SraiFAf IE ot the €(OTri>f'iriY 



FROM THE HILLS SOUTH OF HIOM 



TO THE CHA 



.HARLFIELD COPPER-MILLS NEAR filCKMANSWORTM . 



.Lotidcrt Cla.y - — — 



WeolwirA mui. Ttfodin^ Serirs _ 



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TSpr.^lmd. Jcwti rrcni nHuaZ .ntney an- marked -wiOi « 



Scf I^xpT/mcciiart of Time 



71 air Ifigli Wyaoinhc 



2 . FROM CRAYFORD TO UPNOR NEAR ROCHESTER 



hill A'ln^lcwtU 



l.imt Mnmrtht 



Jjinsbiay Ppnur 

 Ouuth ChulMpit 



TMlEmiETKCM; BIAfiHAMS m iixtfSTBATioN oi- a JPAST (dlDKBITIdDK m the JLH^ID) whick avE iuse to the JK©»I[ATI»(>i 'iSMWE, mn ^^M) JPIOPE^S 



A. THE DRIFT-GRAVEL AS A 



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Tfrtiteahlc San^£ ._ ht'..v.Tl 



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T7tf'£jtoit' fff'the -fme htm.x<mlriJ- JiriM 

 marJis die fidffltt at. H'TufJi tJw waffi- 

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 fhmun^ thc'tSand' and -fravd/pipts . 



HE LOWER TERTIARY SAN DS AS WATER- BEARING STRATA RANGING TO A HIGH LEVEL 



