Stop at Junction U. S. 61 unci State 74, soutimet of Ceps 
Girardeau; at Adaas Filling Station, northeast comer of junction in 
outcrops ext raiding diagonally from 61 to 74, tad at latter particularly, 
are rather thin 6— inch beds of blue, fine-grained limestone, interbedded 
with gray, somewhat earthy Haas tone, the former particularly we&therftg 
with vugs or rather assail cavities, light gray to brown nodular chert is 
cotxaon. Fossils, brachiopods, large ostr&eods are comae. A striking feature 
■is the pre ■ Lch, with the other fos 
Ls known to be ehoractaristie of the Ridley fermution of Central Tennessee, 
Bare, then, is. the first known occurrence of the Stones River (Kiddie) in 
Missouri, and adds 'to the knowledge of what constitutes (in Missouri) the 
thick section of rocks to which the neae Flattxn has always ' been gives. 
The occurrence of the Ridley boro is of importance in that it represents 
the first known section where beds ranging in age from Buffalo River, thru 
Stones River to Black River are known to occur. 
Further Butebtom localities, according to Ulrich, ares 1st rail- 
road cut west of &elie Stations railroad cut 6 to 7 miles west of Ste. 
Genevieve. 
■ ; ... p ■ ' . - ' -• • 
Bciiaxmad to Caps Girardeau in the mmn ing* 
April ES- 
Gape Girardeau to Batesville, Arkuii sea* From Gape Girardeau to 
abaridoned Baaly Quarry (north quarry of Ilarquette district) * Faulting 1 
present but -Stones Elver-Blade Paver contact is probably present In central 
part of we at face* Must check this later* 
■m 
April 24 
One and 
south of Cave City* Arkansas , on B&tesvllle 
road (Arkansas No* li), in eon tor 29-16H-SW* P Independence County* Jrkam.as., 
are outcrops of dense, light to dark-colored limestone, overlying St* Peter 
• a represent lower 10 feet of limestone* 
a 
Light colored lime stone carries ostracods, but darker (Bathyurus)* 
lore finely crystalline dolomite yielded oetracocia (Tube-Tot radium?) , nr&cmo- 
pods, trilo bites, gastropods* This mapped as Fiattin by Miser in Bull* 724* 
ow,;aeeian limestone* Contact i&t 
gray, sandy a bale - 24 *j£ followed by magnesian, yellow, earthy dolomite# 
Ulrich says ^compare with. Dutchtom® * Fossils are same as those found in 
reworked material at top of St* Peter in Minnesota* i*e** the material be- 
neath the GlenwoodL 
Lame as preceding locality — up hill a quarter to a sixteenth of 
a mile at contact with underlying St*. Peter sand* top of which is Tory 
ferruginous * The succeeding material consists of of red sard and grayish* 
green clay stele* (Collected samples for melting for eonockmts*) The ro~ 
worked sand end shale ire followed by sandy., e* rthy Agnesi an limestones or 
