Scieyitifi': TnielKgence. 

 lUpferh 



ttora, except perhaps \ 



aliie 



d Vs thes.> points of (litlerenci'. lik 



e th... 



b.'O! 



1 <;|;-'^-^'^'<"l '■roui tho begirn.in 



gof the 





flora 







'il:. 



aj.pL 



Mr to fuUv oorro'oorate the st 



ateinent" 





■p<.c-h, the flora which formed 



\lie con- 







iin.pcaudiiitho United Sta. 



es, a^ d 



itK-icnt 



U^ 



a> relativoly alike, as is now 



the flon 



I of the 



•2. 



0;/ ^-onie uobds conne'-ted ic 



lf/> the C 



V<nrj,„> 



of 'Xorlh Cnroliui ; bv T. A. C 





(From 



Dam 



I, dated (Jreoville. Pitt Co.. 



North* (. 



labelling the e.illection of fossils 



at llah 



^Stam 



exph 



)nng tho uuirl pits and bank 



of Tar I 



■iNor. T 



miicl 



1 of the mixtur.^ of Miocene : 



md ( 'ret; 





deliir 



hted to have an op])Ortnnity 



to vc(> t! 



le bid 



I tho 



light von would like tp haV 



e a ^ket 



rh <M '' 



from 



tnree to iivc feet deep, and i 



ndicate ^ 



the !- 



taceo 



us shore, not an E.Hvne ot.e. 





ind ' 



Silv i 



uid they ai-e eMroaiejy rare. 



*Tlie u'l 



uirl 1 



lu>r.e-to,.tfi, winch I think is Leidy's E. frntern„>'. Lyl. 

 top()t the marl, it liad evidently been thrown up fn'Hi 

 }uirt ol the i)ed, and iv black and mineralized. From tlic 



prove l; h=;;; Mon^-dT'^ /^™' It wlVliv'theT 

 1 ea-^hore clay near Phila<lelphia. Prof Kerr ha- a nc u 

 eight inches hmg, which connects the tvvo gcKTa />-' 

 '^yt'''^i7^'«, for it would belong to the latter if it had 



