POET OF PK B3S I. C. WHITE. 



is s many p] sal mg :h banks of the Sus- 



nna ri ss \ - - -. much, eurrent- 



ed, is seen jntting ddes i 



> 425' to 45 earn. 



- ;Jly prominent along eithei - 

 Salt Lick creek : and one of the outcrop 3 mar 

 site McKinne] si ~ _ > miles s th from ».- 



_-. where the foL _ - ined in les 



"iill on the left branch of the stream : Kg 



•eat Be; 



L Gray, current-bedded sandstone, (top 1506 A- T.) 



_ II 



3. Gray, current-bedded sandstone, 2i> 



z r :.- . : Lf-fl : -:- .: I f:_ 1 .".fr- ::. 41 



Kc I extends I the summit of the hill, and its slopes 

 rgefi gmentsl token away from it. The - 



rum is greenish-gray, with the layers 1 2 in shes thick. 



-Autifully current-b- 

 in 2 I me thrr- : irbeds t sands! out they 

 - -i at this local: 



No. : is the - M ~~ ~ 1 ■ rang the 



2i that mal-:— tiff in the hills s - - ss Tip- 

 ward from the base of the hence it be "1 

 marked ho: b e s p ecially _ bS -:ianna. 



sores e seen in Xo. 4 at this locality ; 



the genti j rounded 1 _ -7 of the hill-- pes w oldie 

 the tnsi n ths : ntains nothing :: epts : shales 



•.."-_."._ flaggy sandstone 



About one mile and a half south from the last locality the 



_ ^ Mi y Mom > seen in a 1 a line >i out- 



:^s around the hills with its se I ion 



A. T. or 190 lower than at the school- o x lius 



_ rig a dip in this interval • :: - This b 



local : since northward from the - nseit 



as southward from the same 

 locality. The stratum i $2 7ck and much current-bed* 

 On the op^ site side on. it and other sand- 



ove. are seen jutting out in cliffs far up the fa 



half mile southeast from Great Bend depot 



