10? .ib-tBW^btt&Bbo^&nermaD.^eQ/pgffsifi ,o {i^*P*wKi?PP 
1. Limestone, BfayucriOttenioo. j-jbiL . .igasxa Janofr )0n. " 
I rr-i-s — t*W 
Total . .ioqqu. < aslBA& suoq-iboIso .JjiiB. t :^lBifi0^nolfe..3.iinches 
6 " 3 auo'ialiliaaol viav ,ji£q 
M Ntim'berS ito .io^r'ifti * fifth cut >><§#■ "Sie big 
curve going east. NtfrrrFek^W 
14. to {6 .in tjie third, ^ to ig^n^^e^o^^l 20 to 25 
are. in <jh© firgt cut on the big curve gojng ea^t, $ Wfcbeia 
26 to 33 are in. the cut a. hall mile. east, of TBeatimcmt: Junc- 
tion arid nurrtbers 34- to 40- are- in the- first cut^st'e^f Beau- 
mont. °In'otr;er.words the' sectif.n beginning at number M 
and pacing Eastward ;d6wp Bl th a g°f ^|nH-nt along the rajfe 
road i^ exposed in the first seven cuts. ?Ymo\ 
It seems pF-©b^bl«othat ) Kt«Bbeiri'i2 i ^ 7 :ldiis.-sect2ioii; is lit 
the approxiniatvoli^rizbin'iof biTfehe ,, /^^tt6«i^oc^°f 1 lfrriestone; 
judgin| iron? its • general • appearance a t ria" 4 p r osVfI6 ! n' in the 
T- v " j £ aliagoi 9jno3 ^bobnaotniaib .b'ifiri ,91/ld, .sl^nS ,t)S 
section and number 13 carries a fauna .similar to ths, 
Flarena, shalejB and has a resemblance to them. ILtJkysspug* 
ges-tiont) should] prove to be correct the. thickness maf ^theGae^ 
risoh f&nnati&h at this locality would '^^46 ; fee*? f * riS - 2S 
"Trfe twokreams heading on the crestof th'e ridge have' 
rernpved khe_;Wreford fimestorie from the P oir ^ a ^^^fi th^- 
railroad croTseiJ^^d^JJ^ jg^d 'j&ffgfai>'y& %8f$&9 Q»r 
the»ridge jusfe south of .the railroad- too 
" EighfeenStailes s©Utip^ofreBeaH¥fi©Ti>t> f i^ tfre^Cirtfnifl&im^ 
m it/ region famous for its fossils. ■ The logical a$|loaT3i t& r 
th^ re|iop i^^^f'^^'^ffl^S'^^^fe^ft 
furnishes ..a va^a.bl^e^Cjjt^ [Y 5<^il89R8oJ»$*§iI t89ljsrf8 . 8I 
This section. will,' be 3e©fksid«i?ed ki .twfo^pwwtsa'tteenGtfandr 
Summit, or lower, section and the -Cambridge^BuTden, or 
upper, section^ The d^l!Ped , s^ti6r} w of a { J Re I €ra"nd : Dimmit 1 
half follows: , . . '. . 
GRAND StfMMI^|jgTJ9^ oo tdsll .aefeilB .8 
29. "ShaOes," blufe, with calcareous sheets and rail benvoO 
Jioris off fos8flfefrSfl.Yte43.4tfw .,a?np. nirfJ pwlgagnfltetyqi^heg 
28. Lirrfestone.^blue, clayey . . ; .• .• .-..- .- . eprq9iB0lfiq . ,quld » a ^sxf3« .3 
27. Shales, blue,? JpeOOw" abovfe " vV<\\ L . ! :-. ?. . ::i-. ... '5 ■ '""" fir" 1 ™* ■* 
26. Shales' and- shaly lkneBt0ne&&°<J9te4fl??. fms sp%q-ro»te<$ 
25. Limestone, gomdwhtetfi mMiSfVe, f 1 >We£fie¥lHg"< ,9no*a9mL] 
" Kght .2........... ,.,,it............-.-. 4 ..-.-.-.-.-.-.-.-..-.«HBliaaq8 « 
24. 'Shaltes.'cal&ireous, and impure • lfcn^fSfll .9™.°. 7 9I,frf .^ rfq ' - s 
23. Shales, clayey, with calcareous layer, very fos- 
