dolomites, with fragaenta o£ lingulae,. 
3 
of all material collected 
f EI 
X* 
Q8iS6r&L clip is south* Tfa&r© ic & gruciu^uL gradation ,., w . 
• saat^jr, earthy asgaeaiftn iiaestones upward to a finely czar»fall*ne., tore-- 
doIaAto, ,nd into the dense, Wan, hard or light ,:i -Ua^toS. S 
entxre section is not over 
Drove to Evening Shade, and south of that torn exposures of 
.rtter dolomite wart studied (I did not attend). totoUe chart float m 
£mmd on top* 
Drove north through Zvmtag i . do to crossing of _ per Hlver 
ssin typo to 'Em 0» Ulrich, nd Cotter— suit Infills, 0< m- 
turned north about one ails to top of MU and Ulrich found fossils 
{t&aitl iriile) in cter i* See Figure 2* 
CVV^ 777 - 
ts/viesrortf 
CH££?-r 
-DQdOM/T£ 
/=i?/? 7 " CA 53 //V 
th~kss^i 
/ 
z 
z 
zzr z 
SlAC/r /?/t/£/p 
/DSSS//VO 
'SM/T-HV/LLE P 
: tfDtrrry River 
eutlw On top of hill just oouih of Ifcr __ 
ergilltoCitoue doiaeito occurred in eont&ct with limestone* SmithklXe- 
1.*^ v'-rton coi.-.t:-. cu v» ) * XiXiuc;' ton© c -'©curred iXlXJLiig IspJL© or iirr^gulnr 
itjpre^iiion e.u ^ iltfaviXL© (?}■* leathered curxnca of Evortoa liss^tOBO 
yieLdod siXiaifxod. gastatipocUs (Cyclora) « 
XettirKd to Sut3|^llle in evening* 
April 25 — flindy^ duety* 
iiorth from fcteovUie through Uuofeuai to £ lailtc; north of 
tx£Si ns loXXovf^ 5S^XSK— ? Xncicjpendeiico County* on euet 
9* 3 ■.■■■■* 
s € 41(1 4 ® 
