Tetradiua cellulosum and. eoluanare abundant on slope below this 
bod. Ulrich says the latter is abundant high in 'the Lowille beds from 
Tennessee to C&n&da, via Mew fork and Pennsylvania, 
time be Ims found thorn west of the Mississippi Paver, end tb-t be has not 
found them in the upper Mississippi Valley, 
It appears that the uppermost atones River teas in the section 
north of Cushaan are absent here. 
Miser, wire measured the entire section above the howille (Piattin) 
Stones River contact, gives the following thLckneasest 
Plat tin, 
Kiaaswick. , 
**.**.*..« 2o s 
.... 20 * 
• * m 
The Kiaraasrick is overlain by the FenmJLe, the total thickness 
or which met be SO feet or sore. It appears to be overlain by cherty lime- 
stone of the lower Boone (Seeds Springs) although the contact was not exposed. 
Samples to show Femvale lithology were collected as follows: Wo. 1, 10 feet 
from top} No, 2, IS feet} No. 3, 20 feet} No, 4, 2S feet} Ho. 5. 50 feet} 
Ho, 6, 35 feet. 
There is no Dutchtown present in this section insofar as typical 
fossils or lithology are concerned. 
After lunch went dots Missouri Pacific tracks below glass sand 
plant at Guion and collected large p&Leeypods from argillaceous, sandy 
dolomite in interval 5 feet above St. Peter, The section is as follows: 
J oachia 
Dolomite, argillaceous, sandy? 
tone, cblosit© 
Dolcxaito, argillaceous, sandy. 
Dolomite , s< ndy with pebbles ..... 
i, very sandy. ............ 
#■ # * 
B'jloni. te , very 
St. Peter 
Sandstone 
yelecypods. 
0 * 6 " 
£* 
0* 6 B 
2 * 
l 
April 27 
From Melbourne to Hunt Place and Pilot Knob, located approximately 
8 miles southeast of Calico Bocks collected fauna from basal beds of Fverton 
dolomite exposed at foot of Pilot Knob* Tide aooc is approxlmteiy 155 feet 
below top of i&verbosu With McKnight md Miser climbed Pilot Knob* Also 
found fossils 57 and 75 feet below top of Evertotu Joachim overlies St* 
Peter but apparently is not over 10 feet in thickness* Is overlain by dense, 
gray limestone (the map Plattin of northern Arkansas). Also collected fossils 
from Evorton dolomite 55 feet below base of St# Peter sand on Owen Jones Mt* 
Ills was locality from which McKhighfc had previously collected fossils and 
L steel them to B* 0* ulrich* Among the forms was a Jaeperocaraci Girvan- 
alias were particularly abundant* With MesXer also collected ostreoods about 
~ 8 ~ 
