>r 1 
Pago 17, 
Ulrich notebook !To. ?A* 
Sept* 11, 1915* At Bedford, Ohio, in linkers Greek 
with H- P. Cue nine* 
Hot conodonts and ostracoda from extreme top of Cleveland 
(uppermost 1 inch) and Protosalvinia 1 ft. higher - latter 
extend up sone distance in Bedford - observed them up 10 ft. 
or more above base. Cushing took all of the? Bedford fossils 
worth while. ;/ith lower water hiany night have boon procured 
Made 3 photos of Chagrin-Cleveland contact 
Ho. 1 (-^ sec. l/l6 at 6 ft.) 
of new film 
shows offset in baso of 5 inches, and 
slight anticlinal upturn of - Chagrin 
layers beneath same. Hob* 2 and 3 (dujJlicates f r second and 
1 second -l/l6 at 6 ft.). Pacts in case are peculiar and 
hard to explain: — 1 
E 
.. M **»* >•*••** 1 * ' 
* V 
Probably reworked Chearin 
Chagrir. Green slii-7 Cleveland Black shale 
w 
-■' &V **" *■ .-vr .«■> 
/ >I ,J ■'a**’ *"— 
.mi:. 
y 
Chrgrar- - B®mr 20-25 ft. 
Almost entirely" of green shale 
Flags very thin ana very in* 
conspicuous. J 
)eposited in part under thin 
overhanging Chagrin ledge. 
Or all three parts of this 
Chagrin material may liave 
been deposited after beginning 
of Cleveland deposition. 
Chagrin material 
washed in after 
beginning of 
Cleveland tine. 
ConSct-^#* 5 ^- 
/.Bout 75 ft.- 
V. v 
... bnwr. ■ ■■'. 
Aft J 
w «•.* - 
Chagrin - top siirfece wife a£ w oia 6r offee t. 2 ^ dossils rar 
-—-Stream level Sossils x Reddish, san<^ 
ibesilB r 
> Fossils practically confined to upper 5 ft. of 
sE.'as.NS* • • 
SJPmte? «rSd «?h 
C V A crowaect wirn 
be lnr.1? ^ 9 of sped on seeus to 
out mny # rare u forns? co ^ ec ting, however, may bring 
f; . _ .1 J \ 
■ 
> - 
.ft - L* • - - ui'X 
