rllO NEW YORK STATE MUSEUM 



The only interval between any two adjacent bars of this shore 

 which appears to have any yalue for purpose of comparison is 

 that between the highest bar and the next well developed bar 

 below. This was first suggested by the bars immediately south 

 of Adams/ where two strong bars occur, the summit bar and the 

 next below, with a vertical difference of 27 feet. These bars are 

 conspicuous even from the railroad. The vertical separation 

 seems too great to permit the two bars to have formed at the same 

 time, specially as the lower bar is ordinary fine beach gravel. 



Table of vertical relations 



Tk:ot„^«^ „f Vertical dis- Vertical 

 hiffhMt **°^® between distance be- 

 No. of cross-section v^o,. ok^^I +1,^ highest bar tween highest 



aooye ine ^^^j ^^^^ strong and lowest 



P'*'" bar lower bars 



Feet Feet Feet 



25 .. 37 51 



24 35 10 



E3 25 ? 



22 .. ? 



21 41 •? 14 



aO 35 14 24 



19 41 19 (19 



18 48 ? 28 



17 ft 50 27 42 



16 40 27 27 



15 63 27 40 



14 41 35 35 



13 63 35 43 



12 51 24 24 



11 51 16 le 



10 58 16 38 



9 61 18 4^1 



S 41 15 36 



7 .> 57 11 38 



6 60 15 39 



5 i r*5 13 37 



4 57 ? 35 



3 42 ? 



2 50 ? 



1 44 22 22 



^ See chart of profiles, group G, nos. 15, 16, 17, also pi. 11, 12. 



