g® The American ^Geologist. Ai m*-\W 
12. Liniestone, buff, top full of FusuMma ...j 2 'f >(fai " £<3 
11. Shale .: 5±: •" Ob " i 
10. Limestone .-WOrfg. Jtfii. ■ 2± " " .0 3 
9. Covered JS M " 
8. Liiiest'one? weathering to a dirty. dark gray.vcfliti 'fesflkriS" .8£ 
7. " Cohered . w . ahoumteQ .bas. z9&Bfl ,3iafikj liltr " Q 5" ?*, 
6. Shale, yellow, green and red with rotten.iime* 
stone near the middle, thin sandstone of r : y ofsrig .0* 
1 inch or 2 inches near top 35 " ffaiJ" .3* 
5. Limestone in«thin layers made up of peiecypiStlSF' 1-r- " o " .^ 
4. Shales, soft clayey, and weathered slope 3$: vat' iSksiQ" 
3. Liniestone, massive brownish, forming fall -in .S£ 
creek n .- i.dil 1 " 8 
~2r. — Shal es, g r e en and blue soft clayey 5 
1. Limestone, brown-, massive with Produetus 
<cora .1 1 - »; " 
:— — | ' 'r.ri3 — £& 
Total Si , , aoo?$3& ftafcfifichi&S 
Xumbers I to 3 are in the creek west of the road just : 
northwest of Reece, the remaining loweY' part of the sei- 
tion (numbers 4 to 9) extends, up the bluff from the creek- 
Numbers 10 to 21 are in the cuts- near. the spring about 1^/4 
miles west of' Reece on the railroads This "part -of the. see*: 
tion corresponds to Wooster's section.* X timbers 22' antf 
■2-x extend from the top of these cuts 'to the big fill about 7 
miles N. W. of ..Recce. Xumbers 2\ to 40 are shown in the. 
cut and stripping by the big fill (which is the same; as the 
big' trestle mentioned by Pressor); 40 to 49 are in the 
fourth tut easVof Summit siding; so to 56 are in the third : 
cut east of Summit, s7 to 63 in the second and 61 to 76 are 
' ' " . . . ' ' EiJ .fcS 
in the first cut eaM ot .Summit. , .. 
Just prior to our .visit, the great trestle on ti>e>?eastern 
face of th 1 escarpment bad been filled, as had the smaller: 
ones between it and the crest of the ridge. In securing the 
material for the fills, the available soil and loose material 
had been removed from the right of wav in the vicinity of 
the cuts, leaving ideal exposures from which to make exact 
sections. These exposure's threw light on points which 
were before obscure. In the light of our sections we make 1 
the following summary Of formations. 
Numbers i $o 40 are Coal Measures or Pennsylvauian.; 
**KanV Univ? Quart., vi, p. 153, footnote. v 
