Notebook no. 24 - Ohio, Tennessee, Virginia, 1914, 1915

■ til. if ft

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Dover Bay, Sept.b,1915

with H.P. Cushing and A.B.Hyde

dan

~1,~ prfijr ah. jfl

* * **j

SJ $4

black sh*

w*P s
ceo

(

20 *-25 *

t. r
/ ■

v

■ ,u*

interbe&dod blue and blk.

sh.vith occasional thin
flags or lenses of fine
sandy material.

at iiickle Piste road*

about 15 f

ntxvr-'

V;v

. Possible brpak but

above fS) trolley line* physical evidence very

' A scant - Ceratiocarid

\ and rugulose plant*

Not ovei
Id ft.

rugulose p!

Looks exceedingly like
upper 25 ft,of Chagrin

‘.of trolled line

/

Chance f*or break - but, seemingly of no con,
u .,. • sec."^®nce •

20-25' Black sh.with striated strep like plants.

20

iteS;

*' Black, blue.green and a few flags - blacksh.is

dark-gray rather than black am not fissile.
Has a black strep like plant. Daw no other
fossils — also no Protosalvinia.

l sf ■

Lak^ 4 or 5 sand flags - rusty, l/2 - 3 in.thick - in

basal 18 inches#

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Pages 15 and lurxcn notebook No. £4.

♦

Sept. 9, 1915, with H. P. Cushing and A. E. Hyde.

At John Goetz house (Felsaneck). Sane section (with beds

dipping HW. ) as .at uinz’s. Contact well shown at water’!
edge at west enu of bay and rising east about 5 ft. in

250 ft.

Blocks and slabs of a six-inch
ss. lie at water’s level but
no corresponding ledge is seen
in section. May be one of tho
2-4 in. beds.

... Black, basal Olmsted ss.

0 - jjpjg#

10" -12" Banded sh., dark and green

2"-4"--rryS. ,

3" -4”

2” -4'’

r '■‘,‘afci/ 1 -

r i

SS.

green shale
ss.

Contact Chagrin-olmsted-Lake Erie

at Goetz *s - lower part of section in detail

100 yds. east of stairs.

Ss

Olmsted

Chagrin

/ t r t ,

usual dark gray, or black sh. at base, here
thin and interbanaed witn greenish

0-2" ss.

A

• -

~7

' f

1 ft. greer. aiiale with intermittent in.fl^

j ^ ^

1^-3" flag, current formed

9 about 1 ft. as above but flags fewer

*See variation
on opp. page

L 3"-4" 2 sand layers or series of lenses with '

le 0 *

J * ~ ' " 'shale between

9" soft greenish or grayish - laminated shale

R ed s s. x

. * *

- 5 <£>.

- V v v t

2-3" darker and harder shale

2 in. flag -reddish icf. Porter Creek)

irregular nods
2 ft»

Large nods 2 1 ft. wide 8 in. thick

Art

«h»

1 in.

4"

. ’<*

6" green clay shale

J*

1 in. reddish layer of confluent nods

4"-6" nodular fine limy ss
Shale and ? ss. or nods

Lake 1 ft.

*2his double layer of sandstone varies as it is followed

along cliff. f 3ia two layers are thicker and more persistent
toward wost (beginning 100 yds. east of stairs) ana near
stairs (50' east of) the two show tender.cv to merge into one
by elimination of clay parting. At the stairs itself the
horizon is covered by talus. It is suggested that in the
covered soace the two layers tiro f’lllv merged and that the
thick blocks or slabs on'tho shore represent the combined beds.

•soqoax gx qrjcuq
Vi ***4sna - j puns g jo

# 8"j;ujA>X8BO^Oj:^ ou OSTU — STISSOl

' e ^lTI cloaks 3(Ouxq t* shh

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<I*H TRIM
*/&V{ MAO(£

9, 1915, with H. P. Cushing and A.

Sept

Contact Chagrin-Clmsted-Lake iirie
Cliff at house of W. -• Hinz*
by Prosser in 1913. 1/3 to 3

house.

'Drift

all black.shale, as m
orfer section.

hsstirsiSsi.’W"xssse

SMJ-SlrSS SSr’Wft

mrd, fossillferous

34’ (accord
§&§s£8r).

'^ast thin fle£ s basal part of
section at Nussaorfer s house.

rid black shale
eaves

hpwer pr basal
bed with 2 or
about 5 in. =
section. Con
but rare.

ss. Isminose
park and green banded shale

Current folined ss.

X* Dax^k and green bands

Ulrich notebook Ho. 24

>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

I

i

!

Page 23, Ulrich notebook Ho. 24.

Slate Cut, Ohio, Sapt , Monday, 13, 1915. With Cushing.

Mery warm!

i

..gscs*^ ■ " ■■■-•

:i "f. | . 1 gfc -

~.

Prout Is.
'1 inches exposed.

H.R.

*4*^ I ITT 8 ? ■

r **a»^

The Huron here is black, Jiard. and very fissile, mak
it difficult to procure fresn surfaces showing the cono<
which it contains. Brought about a dozen specimens.

The Prout Is. is a crystalline rock, apparently
dolomitic, with corals and crinoidal remains. The corals
comprise, so far as observed, Zaphrsntis cf. gigantea
(3 inches in diameter and 1 ft. long) Z. cf. prolifica,
Heliophllum Halli, Favosites with cells 1/33 to 1/16 inch.

Upper part of rock usually in "spalls" as though ex¬
posed" to weather. In one place across (on south siae ox;
track it is solid to the top. Generally, however, 4 or 5
inches at top appear as "shaly."

ww » » • _ __

The

n

s

extreme top is smooth or but
slightly uneven, and replaced by
marcasibe to a depth of 1/8 to 1
! The upper inch contains occasional green
spots. Corals sometimes project slightly above general
level of surface.

The contact, as intimated, is a sharp but^ even line,
with no trace of conglomerate or soil. The black shale
begins at once in typical character and, - under cover
beyond the oxydafcion of the marcasite, - adheres firmly to
the limestone floor.

Beached Milan about noon. Examined good exposure of
lower member Ohio shale along west bank Huron river,
beginning about 100 yds. above bridges- Exposure fairly
well reported by Px*osser except that the beds dip more
gently at upper end than suggested by him.

Possible ooundarjCf, ^

(b e t we on Bur on
and 01mste&>-~

y

O

ij'wvn..,,,

o 0

Siver

O

Page 19, Ulrich notebook No* 24.

Sept. 12, 1915.

Pacts bearing on Chagrin-Ohio shale problem observed in
passing westward from Bedford to Beach Park, Ohio.

(1) There is a definite though often inconspicuous con¬
tact between the top of the unquestionable Chagrin and what
ever rests on it throughout the distance of its exposure.

(2) At Bedford the interval between the top of the Chagrin
and the base of the Bedford is about 20* or 24 1 and consists
practically wholly in its unweathered condition of hard,
slaty, though not decidedly fissile black shale, evidently
representing the upper half or more of the typical Cleveland
In Doan brook the Cleveland has increased to 40* or more.

The upper 20-25 ft. represents the shale found at Bedford.
Beneath this come some 8 or 10 ft. with green (and olack
shale?) interbedded, and including several ss» flags. Under
this come 10-12 ft. black fissile shale to top of Chagrin.
These two places are on east side of Cuyahoga Diver.

West of the Cuyahoga the interval between the Chagrin

and the Bedford increases continuously.

In Big Creek, 1 m. west of Brooklyn, the interval has
increased by underlap addition of at least 40 ft. more of
intercalated basal beds.

On Bocky Diver, 1 or 2 m. S. of Kamrns bridge over 70
ft. have been added making the total of Cleveland -f- Olmsted

here 110 ft. or so.

Farther west at Dover Bay, Fagle Cliff, Avon Point jl
and Beach Park, though full thickness could not be determined,!
it is evident that still other beds are added to the base j
from point to point. The total may have risen to 150 or

200 ft. ^ ®

(3) On the east side of the Cuyahoga and goind west Irom

Bedford, greenish shale with S3, flag© are first added to the

Cleveland as developed in the section at Bedford. These

greenish sh. and ss. are observed in Doan brook 20-30 ft.

beneath top. See §2. Similar beds holding the same or a

little lower position are still recognizable in Big Creek

but west of this area their place i3 occupied by rather soft

black shale. ,

Under this upusr greenish zone comes_black shale wnich
increases ranidly in Big Creek - o ft. go 2 o it. in about 1
mile. One or 2 flags are present in this but they are no

east of the Cuyahoga some irregularity or unevenness of ^op
of Chagrin is indicated

Chagrin brook {• / Big creek

(See sketches on reverse.)

Page 21, Ulrich notebook No. 24.

Sketches illustrating deductions on p. 19 .

Sept. 12, 1915,

At—

Bedford

Doan Brook

Typical Cleveland shale^r

*1 /

»«. <•-'4 H

% \

< ^

>e s ';

■V.

8 ‘'«as\i l y"«* lnor 3i

< s *rr-~-atiors

\—*L •V ^ 1 1

^86j

/-i < ' /

< ' j

-- Qz*^'/ ’ <

contact grows more and more inconspictious
westward. Both receive sand from same source
and the Ohio got little of its sand from
erosion of Chagrin.

sh

or®

m

s>: - >

^ - ■- _ , *»*««»

;robaole condition in vicinity (to southeast)

of Huron river at Milan.

Berea escarpment
Berea
-Bedford
Cleveland

i

o

p

H-

<

0>

h°'°

foncaaia

(r

SE

Huron

, uirich notebook Ho. 24. ’*
Sept. 10, 1915.

Beech Parle, 0. Section made by T^ydo.

£t 1 SS«

r * —'•

mrr • w -***rr~

■ISW.105-.; 1 ? 1

^- 1

afcale above Ub 6" es

<s

_ >p _

—. •.'... -f y.i

^ _ __

'nods and rich ss. as in Porter Creek & Goetz’s

x t® break lies from 27 to 29 inches beneath the lower of
two layers of sandstone, each 2-5 incaes thick and less than
a foot apart.

at Coetz*s tly quit ® as 1311021 sandstone here in the Chagrin as

/ 1 «„.* Contac ' t raarlred by a thin but varying thickness of easily
decomposing clay snale carrying minute globules of pvrite. ‘

thnhSh +?^S, Ct cut ! und ? r lying Chagrin sedimentation planes
throu^i tnickness of an inch or so in distance of 4 to 6 ft.

lens e s \e r e°Inri W t w «^5J li teri 2 n l /as tested. Sandstone
lenses here ana there beneath contact may accentuate the

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Page 11, Ulrich notebook No. 24

V

2-4”

.X.***.- •»>«•< ■ ' •'.*

Page 11, Ulrich notebook Ho. 24.

Sept. 0, 1915, with A. P. Cushing and A. 3. Hyde.

Calioon Creek - nile west of stop 25 on traction line.

Black shale with ceratiocar.id and usual rognlose surfaced plant remains.
Greenish initial deposit.

Current marked bed.

Under

trolley

trussle.

C

645

I c

12 ’

about 20

»»■« V - x

P.athor harder and more fissile and mainly black shale
usually without flags.

15

Oh

>

C

!

>

Ordinary but rather soft grayish black shale, fissile|
interbeddefi with nearly equal thicknesses of blue
gray shale. 1 or 2 thin flags at top and locally
at two lower horizons. Htraplike plants with nearly]
smooth surface, jcugulosities faint and long lines
indistinct.

i ;

Og 1

Of 10*

Oe

Oc

1

V-

Od 9 • c

'r i.

J ■

Urey ftnd black shale , ra ther soft, the gray checking
under weather with 2 ft. at top containing current
narked flags. 10-ft. bed overlying is the same
lithologically as 9-ft. bed.

Gray and black shale, rather soft, the gray checking
turner weather with 2 ft. at top containing current
narked flags. 10-ft. bed overlying is the same
lithologically as 9-ft. bed.

- , i fH iS ■ ' T -

I > M Ak •

Ceratlocarid.

Ob 10*

Oa

' >

Cerntiocarid.

/ ,• e

' *■

1*

f * •

’ W:,

(OVER)

2-4 ft

Od

Oc

Ob

Oa Olmsted

Oc Chagrin 10

Cb

Ca

gray blue fissile

/

s.

black shale

wagon

f

roni

K

\

9' 5" blue sh. slightly fissiloaud more clayey than above but less
than below, with 2 or 3 thin flags, 2-in. flag 3 ft. above

u 0 •

8" blub sh. base of Olnnted-.

soft blue and dark slmlo with 5
or 6 or more 1-3” flags and rusty
nods, between the flags.

dark sh.

7*

t

Lake Erie 3V
573

■ ' ■

8” dark clayey shale with sharply
striated plant straps

mainly soft blue clay shale

1’ black bands alternating with green,
each 2-3 in. thick.

2* dark sh.

All the Chagrin dark
1 "black**) shales are

TthS 1 85SIt tlJ<m 11,089

e oimstea. EXppsed
e creek beds, Their

top surfaces soon check.

?n

'These correspond, to, the
best brick shale along
Big Creek.

645

573

72

72’ r diff. in altitude

87’ - estimated and measured thickness of beds
passed over in going from lake shore to
Hickle Plate R.R. track,
fop of Cleveland to 740 ft. contour
3 wiles south of Hickle Plate II.I;.

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Page 12, Ulrich notebook No. 24*

In Porter Creek -?r mile west of Gaboon Creek
tho lower beds of the Olmsted (,0a to Oh, in¬
clusive) contain less flags than in the Cahoon
section, ^io proportion of dark and black shale
to the gray also is greater, *he Chagrin, whose
top lies about 18-20 ft. above the lake, on the
contrary has rather more and thicker flags and
particularly of irregularly shaped rusty nods;
also a foot or two beneath the top a worm bored
fine earthy red ss. 1 in. _ thick, beneath which
1 ft. or so the irregularly shaped, nodose to
finger shaped nods fire very abundant. r ^he con-
Contact in "^.tact between the Olmsted and the Chagrin in

places cuts out the top sandstone. 'Ihe
\ latter seems to bo tho sane layer that is
beneath the contact in the nearby Cahoon
/ Creek.

places cut
out the top
sandstone
flag of the
Chagrin.

J

Black 01nsted

Olmsted member.

'4 17)119 above railroad bridge <pn Big Creek;
1 l/3 miles of South Brooklyn, Clovolmd
With Cushing, Sept.2,19?.5.

•ift

About 12• Kard.blocky,fissile bl.sh.

-,r>- *

Bather soft bl.sh.

typical

Cleveland

A

About 12 f

ss* l"-3»

J

2* greenish to black sh.
es. l"-« r 5"

5 t « 6* Mostly greenish sh• intorbedeled with

ale.to d 1#seams,both rather soft.

K2v;,;.

Bather soft bl.sh.

About 20*

■ ss. flag.

Bl.sh., not very li&rd

5* 2 " wi * h rlg^Js and ceraticarids

ana conoaonts #•

] lA v- *<"•;

Chagrin

Big Creek level

* Collected and nailed in unlabeled material pro¬
cured here from tlie basal bed of Olmsted.

r '

1

P *

I

I

- -— -TTz*

\

/■

In Big Creek
30—40 M

Under foot bridge 1 mi.W* of main
bridge in Brooklyn.

6”

2"

4"

about 3 ft.

0-l«
about 22"

3lack sh.

Alternating green
and black sh.

black sh.
greenish sh.

black sh.
green sh.

black sh.

2” ss-and green sh.

s&.as below - slialy flags 8-9”
green soft sh.

blaxk more or less fissle sh

s '.•;••••• -. ••
^ ;. r .

soft green sh.

Vc« -V - • 4 .

fine ss.,dark-gray

black sh.

This interval expands
in 1 mi.SW* to o' 2**

<! ( k

12-15 ft .more or less ss.and sssh.

upper part sandy plates
fewer than in middle and basal
thirds. At brickworks -J* mi.E.
of bridge and in cuts E.of that
ss.layers are more prominent than

J

"/.V-

\

under bridge

v

/

8 or 10 ft. almost wholly of

soft blue sh. chieflv in
brickworks.

25-35 ft .mostly soft blue sh.
in brickworks and bluff along
creek. Concretions abundant.

4- mi.up stream these beds are
Beautifully shown in bluffs. The

whole becomes more sandy in this
direction and apparently thicker,
\ sand layers (some of them bluish
and calc.inside,brown outside)

\ being prominent, and in part pre¬
dominant rock through thickness
of 25 feet beneath base of Cleve¬
land .

numerous conodonts,ceratiocarids
(cf.klumulites of Whitf.),and many re¬
mains of plants. Apparently a shallow lagoon-like depression in which
surface regolitli ana new bl.sh.deposit is mixed and fused.

Valley of | 5* 2” from contact to first ss. (see note above)

. Big Creek.

_

Contact between Cleveland and Chagrin is abrupt and nearly even line that is difficult
to see in clightly weathered cut or bluff. On close insj^ection the line is sharply traceable
with slight to 2 inch undulations. The depressions are filled with granular dark-gray
material - some grains appear to be of rounded quartz, others and perhaps majority are of
minute golbules of pyrite. Just above top line of shallow depressions the sh.is ? the usual
fine-grained black or very dPark-gray type comonlv spoken of as black shale.

oa ? e con ^ act shows m similar manner in bluffs along creek above bridge to second wagon
bridge, thence up creek to -> mi a above wagon br. which i 3 on U.-Y/.road 1-4 mi.W.of S. Brooklyn
where contact is at water level. * _ ,

At last place .centact. plane, sinks some 6-lOinches and is fused in a single layer,which

e specimen).The 6-10 inch

w t V Y ^ w x v cl « wctiiCi Lcvoi.

* 0 last place ^contact plane sinks some 6-10inches ___ „ _

dpnfSfabove,the contact an uneven plane(see specimen)
depression is filled with somewhat granular 2)1.sh. cont? * *

lining many small flakes of mica,

I- 1 *

.1

- -jr m _

'M

$

Ksrna bridge over Rocky River*
Sept*4, 19lb*

'fiadod3ms —

Soft weathered, blade and
gray-green sh*;to top of
bridge about S3 ft#

Black sh# medium hiird
About 38*

Chagrin
.about 37*

Rocky River

-»****»,

T*

ast bluff Rocky River,just below wagon road bridge
1 nile SW. of harms#

xt~

All bl.sh#,rather soft but yet more or
less decidedly fiseil©

6* v ?5*

;i

V S \ V >. '

(rr&v and dark to bl#fissile sh. ss.lens at

top.

; 2* Gray fissile sh* - thin ss.lens at top.

2 M -3” black sh. Olnoted

At ss.laminose.- fine- A*—s»-

^ grained.

Soft kne&dv gray-green sh. Chagrin

Rocky ^ „ ss.and greenish sh.

River

Contact represented by a thin(0-l/3 in.) sean of
rather rusty clay followed a*c once by 2'-3“ of black fis¬
sile sh. or by intervening b inch or so of bluish shale*
This is the same boundary observed in Big Creek and. Doan
BrooTT" sections*

-

Small creek 1 mi.east of Dover Bay, outcroo in v;est bank just
IT. of IT.Y.C.and St.l.H.R.

Chagrin

§*-

hr.

14» "h / \

4 f ' eray fissile sh.,1 layer sandy and somewhat fissile and 1* thick,

lb inches above base.

6 ,f v Black shale

# 2 "

Grayish greenish blue sh. y $ore or less fipsile with 4 to 6 thin
sandy iayors m upper 2/o, the latter fissile and scarcely a
sandstone, one layer about midheight reaches 3 in. in thickness.

2V 1 ft. mostly -olaty and partly fissile sandy sh.and ss. Bluish fresh.

t 1 ft. slaty bl.sh. with conodonts,ceraticarids,and plant remains,all

rather rare..1 rotosalvinia of small size,exceedingly abundant,
nothing of kind observed in underlying Chagrin. Lower 2 in. or so
of bed not so black as remainder.

•> v*.

~. &

3* Soft ,unctuous,green to dark-gray shale,nearIv 1 ft. at top,beneath

which sandy layers occur frequently in similar shale.

Contact in exposure shows a rusty,unlaninated seam l/32 to l/4 inch thick.

Lake shore 573

Farther up creek to crossing of main (Korth ridge) road - a mile more from lake -

higher beds are seen in bank of creek and in excavation on roadside to east and west of
culvert. r/ „

oad f*^ #

15 ft.

abundant

Protosalvinia.

Here somethin* like 15 nV* 15 ’ Blui ? h „ Bh * in creak ^* of ridge road.

of rather soft,moderately fissile
very dark or black shale, the base of

which can hardly be more than 15 ft. - and. may be less - above the top of preceding
section of basal Omsted section. 'Tiis shale contains ceratiocarid, few conodonts, and
plant remains, these were not found in place but seem to have come from the lower part
which may have been loss fissile than the main part of bed. The ceratiocarid however
also occurs in the upper foot of the black shale near the transition into the overlying
gray shale•

The black is overlain by about 6 ft. (all exposed) of gray shale rather soft yet fis¬
sile sh. The layers and flakes when thrown out in excavation weather white when the fresh

a P^ fusty where tho older partings are concerned. The material does not
meit down like uhe simulating but really much more clayey Chagrin; and it contains^

Page 13, Ulrich notebook No. 24

Stop 55 on fraction line.

Sept. 9, 1915, with H. P. Cushion and A. 2. Updo.

Sa^ie Cliff, near its eastern extremity. In short ravine
beside W. E. liussdorfer’s house.

About 40 ft.
cliff.

t

t ' • f- v

' ;

t '

j a.

Lake level

Mostly black medium hard, fissile shale
with some beds of a foot or less that
are softer and light to dark gray in
color. All of this section is Olmsted.
Flags of S3, are practically and probably
sholly lacking above the one at top of
green bands at base of cliff. The latter
may correspond to Ob of the Cahoon Creek
section, while the remainder to top of
cliff is precisely like Ob and higher beds
as developed in the Porter Creek section,
except that flags are now entirely^absent.

Plant fragments of the kind seen in Oh of Cahoon
Creek section.

. Lake level

, —X.—f... • T" • * ' ! «• 'f -

2 * 5"

-vyi- 1 '—/j

1 - 2 "

flag

May correspond to Og of Cahoon Creek section
’?> but it seems more likely to represent Ob or

0d.

-2" greenish shale X, X Composition somewhat variable but

V V~ _-- __ •_ +

3"

V

/

1-2" black sh.
greenish ss.. and black seam

essentially as in detailed section (see

.

1 ft. soca dark shale

EC-'

Lake”

Nv.

/

" ; ‘ ft -w.: : ~

.,,1 PV/**'

' - > 4

-■■

•— -r *

Iw-wMKB- ,i r9-

V

Contact of Cleveland "black sh* on greonish-gray
soft Chagrin - in 3>oan Brook,Cle5reland f C. f Sept*l
^ 1915#

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Index.

Arnheim Island sh. - in Silurian section in Jefferson
Co#,Ky# - according* to Butts(1914) - verified *
by Ulrich (1914) . 45

Avon Point - in facts bearing on Chagrin-Ohio shale,
westward from Bedford to Beach Park,Ohio ... 19

Bakers Station, Term., to Ridgetop - section -

with Bassler .43

Bassler - with Ulrich - section. Bakers Station,

Tern,, to Ridgetop .. A 3

Beach P$,rk,Ohio: __

section at - made by Hyde.. 15

westward from Bedford to - facts and sketch

bearing oh Chagrin-Chio shale problem . . .19,21

Beacraft or New Scotland - in section, east side

of Powell River, Big Stone Cap, Va. ..... 25

Beacraft. not Hew Scotland - in sketch and de¬
scription of hill at Rock Cut above sink of

Wild Cat Creek, Va.. 38

Bedford, Ohio:

part of formation in sketch of contact of
Cleveland and Chagrin at Doan Brook, Cleve¬
land, Ohio, seems to be represented at . . 1

Tinkers Creek at - section -"with Cushing . 17

westward from to Beach Park - facts bearing
on Chagrin-Ohio shale problem.19,21

Bedford fauna - in section, contact of Cleveland and
Chagrin, Doan Brook, Cleveland, Ohio .... 1

Big a lit. - in Devono-Mississippian section -

Cleveland to Dump Creek, Va.' . . 51

Big Creek:

in section, contact of Cleveland and Chagrin,

Doan Brook, Cleveland, Ohio.. 2

section on, above railroad bridge. South

Brooklyn, Cleveland, OLiio - with Cushing • 3

emu Doan hrook sections — boundary at Rocky

River bluff same as at ......... . 5

one mile west of Brooklyn — in facts bearing

oh Chagrin-Ohio shale problem.. . 19

Big Spring - in section east side of Powell Rivor.

Big Stone Cap, Va. 35

Big Stone Cap, Va. :

section, east side of Powell River at 25

section, elbow of wagon road to Slverton and

north to Dummy line - with Williard .... 29

above bridge at - Clinton-Sneedville contact

£? ^an* Jorth Pork of Powell Itiver - with
Williard. 33

Big Stone Gap,Va., cont’d#:

one mile from schoolhouse at - Clinton-Sneed-
vil&e contact on South Fork of Powell River -
with Williard... 33

Dumrmr line at - west end. of hill northeast

of shcoolhouse - sketch of Heldorbergian zones

SW. side of - on South Fork of Powell River -

section at old woolen mills — with Williard • 39

SC p°Bi^°at 9 curve ffi^’of . 41

section at - with Butts and Mesler * c f m S Kk f 53

Brassfield Is. - in Silurian section in Jefferson
County, according to Butts(1914), verified by

Ulrich (1914) . ... . . . .

Brooklyn. f Ohi o:

in section, contact of Cleveland and Chagrin

at Doan Brook, Cleveland, Ohio.. •

Big Creek 1 mile west of - in facts bearing
on Chagr in-Ohio shale problem • •••••*

45

stir

verified by Ulrich (1914] • ••••••••• 47

Buttes

generalized Mississippian section of Louisville
by (1914) - verified by Ulrich (1914) * • .47

and Mesler - withUlrich - section at Big Stone

Gap, .. 53

and Williard - locality collected from by -

in section at Cumberland Gap, Tenn. / ... 49

Cahoon Creek, Ohio: __ _

section on - with Cushing and Hyde • • • • 11,IE

fig.Stg&SM’WfcSi? G lx ; ie f he?tliS 9 on . 13

Cambrian section at Cleveland, Va. ,««•••• 51

Chagrin: 7 /

shale in Devono-Uississippian^ section, Cleveland
to Dump Creek, Va., looks like . SI

contact of Cleveland and Chagrin - Doan Brook,

Cleveland, Ohio. 1*3

in section on Cahoon Creek - with Cushing and

Hyde 11*1E

in section in Eagle Creek, short ravine beside

Hussdorfer* s house - with Cushing and Ilyde • 13
in section above railroad bridge on Big Creek,

8outh Brooklyn, Cleveland, Ohio ...... 3

in section at Karam 3 bridge over Rocky River,

Ohio. 5

5

Chagrin* cont’d*:

in section east bluff of Rocky River* SV7*

of Kamras , Ohio.• •••••••

in section west bank of small creek east of
Dover Bay, north of N*Y.C*& St*L*R.R* * • 7

in section on Dover Bay .*•****•*• 9

in section at John Goetz’s house, Felseneck * 14

contact with Olmsted - in section at Beach

Park,Ohio - by Hyde.15

in section on Tinkers Creek, Bedford,Ohio * 17

Chagrin-Ohio shale problem - facts bearing on and
sketch - observed in passing westward from

Bedford to Beach Park, Ohio •••••••• 19,21

Chagrin-Olmsted contact - in section at Beach

Park, Ohio - by Hyde **.«**.*.»« 10

Chattanooga sh.: „ , _ ^

in section. Bakers Station, Term#, to Ridge top -
with Bassler ..*-**•*****«* 1

contact of Chattanooga and Hew Providence .
shales at Brooks, Ky* - in generalized Mis-
sissippian section of Louisville district -

its -fl914) - verified by Ulrich

47

in section at Cumberland Gap* Term* * • • • 49

in section at Big Stone Gap, Va* - with Butts

53

and Mesler

Chemung - in section at Big Stone Gap, Va# • • • 53

Cleveland, Ya *j . .

to Dump Creak - Devono-Mississxppian section • 51
Cambrian section at.* • • 51

Cleveland, Chios

contact of Cleveland and Chagrin at Doan

Brook...1*2

in section above railroad bridge on Big

Creek, South Brooklyn .. 3

Cleveland sh.: „

in contact of Cleveland and Chagrin - Doan

Brook, Cleveland, Ohio ..1,2

in section on Tinkers Creek, Bedford, Ohio • 17

Clinch River - in Devono-Uississippian section,

Cleveland to Dump Creek, Va. 51

Clintons

base of - in section at Cumberland Gap,Tenn# • 49
in section - elbow of wagon road to Blverton

and north to Dummy line - with Williard . . 29

top - in section at old woolen mills. South
Fork of Powell River, SW* side of Big Stone

Gap, Ya.39

in description of vicinity of Bast Big Stone
(Riverton).37

Clinton-Sneedville contact on Horth Fork of Powell
River above bridge at Big Stone Gap ,Va# -

with Williard • . ... 31

Clinton-Sneedville contact on South Fork of Powell
River 1 mile from schoolhouse at Big Stone
Gap, Va* - with Williard ••**•*♦***

Coral zone (?Onondaga.) - in section east side of

Powell River, Big Stone Gap,Va* • *»*** Zd

Corals: - in sketch and description at " Rock, Cut**,

above Wild Cat sink - like Ononuaga species * 38

Cumberland Gap, Tenn. - section at ••••••• ^

Cumberland Mt* - in section at Cumberland Gap * • 49

with Ulrich - section on Tinkers Creek, Bed¬
ford, Ohio • **•*••* • • • * * * ”4

with Ulrich - section at Slat© Guw, Ohio * * 60

Cushing and Hyde: ^ ^ q

with Ulrich - section on Dover Baj • • • • *

with Ulrich - section in Bagla Cluf* short

ravine beside W.E.lTussdorfer* s house * 13^

with Ulrich - section on Cahoon Creek • * 11 ? 12

Cuyahoga, east side of — in facts 1 earing on
^ Cn&grin-Ohio shale problem ••••••••

r'lnrnhno'A. «=» Grainier ss in Devono— Mississippi an sec
Cuya> 1?tn, cStveSandto Dump Creek, Va. . . • • - 51

? Cuyahoga - in section at Big Stone Gap, Va* ... 53

Devonian, base of - in section at Cumberland Gap,

Tenn.. • ..

Dev ono-Mississippian section - Cleveland to Dump

Creek, Va.. 51

Doan Bro ? )c ( , 1 Cl|^|l|nd M 0 ^o e;i 8 ection - ?ontact ^

in section, Kamms bridge over Rocky River - * 5

in facts bearing on Chagrin-Ohio shale problem
passing westward from Bedford to Beach ^

Park, Ohio ..* ' * ^

' D0V outcrop in west bank of creek east of — north

of H.Y.C.& St.L.R.R. • • • • . q

section on - with Cushing and Hyde. *

in facts bearing on Chagrin-Ohio shale problem,
passing westward from Bedford to Beach Park,

Ohio. 19

Dumry line at Big Stone Gap:

north to - elbow of wagon road to Riverton -

nea? 9 §!e$ # Iifl^°of a ?choahouse--%ke S pr i
of ...

51

13

19

37

Dump Greek, Va., Cleveland to - Devono-Mississip-

plan section ***** ..

Eagle Cliff - section at, in short ravine beside
Hussdorfer’s house - with Cushing and Hyde .

in facts bearing on Cleveland-Chagrin shale prob¬
lem passing westward from Bedford to Beach

Park, Ohio.

East Big Stone (Elverton) - description - with
Wixliard . . . . .

Eastwood Is* - in Silurian section in Jefferson
Co*, Ky. f according to Butts(1914) - verified
by Ulrich (1914) ***«*»«•*****♦♦ ^5*

Elverton:

elbow of wagon road to, and north to Dummy line -
Big Stone Gap, Va. - section - with Williard . 29
East Big Stone Gap (Elverton) - description -

with'Williard *««****•*•*•*** 6*

Euclid bluestone - in contact, Cleveland and Chagrin,
Doan Brook, Cleveland, Ohio • ••••••••• 1

Felseneck - section at John Goetz’s house — same as

at Hinz’s *.**»****«**«•*••* ^,14

Fern Glen or Keokuk - in generalized section of His-
sissippian of Louisville district — by Butts(1914),
verified by Ulrich (1914) ...**••♦•• ^

Fort Payne same as at head of Whit© Creek - in

section at Hidgetop, 'Term* ..

G on es ee*

or lower Portage - in Devono-Mississippia:
section - Cleveland to Dump Creek, va.

in section, east side of Powell Diver, Big

Stone Gap, 7a.

Goetz, John - home of - Felseneck - section near -

same as at Hinz’s ... 13,14

red ss. in section at Beach Park,Ohio (by Hyde)*

same as at*.

Grainger:

= Cuvahoga - in Devono-Mississippian section,

' Cleveland to Dump Creek, Va...

in section east side of Powell Diver, Big
Stone Gap, Va* ...

Grundv quadrangle — mentioned in Devono—Hississip—
pian section, Cleveland to Dump Creek, Va. • <

Hancock Is. - Sneedville and Helderbergian lime¬
stones mapped as — in description or vicinity

of East Big Stone (Elverton). .

(Harrodsburg) Warsaw - in generalized Llississippian
section of Louisville district, by Butts(-914)
verified by Ulrich (1914) •*••••

■ in

* e

43

ian

a « * *

51

Big

25

15

51

25

51

37

47

Helderbergian:

zone I of - New Scotland - section at Big
Stone Gap, elbow of wagon road to Elverton
and north to Dummy line - with Williard . . . 29

deposits - sequence of - at Big Stone Gap . . 36

apparently all Becraft - not Hew Scotland -
In sketch and description, hill at Hock
Cut, and above sink of Wild Cat Creek « . • 38

and Sneedville limestones - mapped as Hancock
limestone - in description of" vicinity of
East Big Stone (Elverton) • ••••••*• 37

Hinz, W*T* f home of - section in cliff near - same
measured and published by Prosser in 1903 west
of Nussdorfer’s house »«»«•***** 13,14

Huron to Sunbury - Chattanooga, above Chemung -
section at Big Stone Gap, va. - with Butts

and Mesler • •••.•*••••••«.. 53

Huron-0Imsted - possible boundary of - sketch * * 23
Huron River:

at Milan - sketch of - probable condition of
Chagrin-Ohio shale in vicinity of • • • • 21
exposure along west bank of, near Milan,

reported on by Xrosser - visited * . » . 23

Huron shale - in section at Slate Cut, Ohio -

with Gushing

Hyde

15

section by - Beach Park, Ohio

with Ulrich and Cushing:
section at Dover Bay .
section on Cahoon Creek

. 9

11,12

section in Eagle Cliff, short ravine beside
Nussdorfer Y s house

Jefferson County, Ky. - Silurian section in - ac-
cording to Butts(1914) - verified by Ulrich(

45

Kamms ,0hio:

bridge at, over Rocky River - section . . . 5

east bluff of Rocky River SW* of - section . 5

bridge at - mentioned in facts bearing on

Chagrin-Ohio shale problem ••••••••19

Kenwood ss« - in generalized Mississippian soction
of Louisville district by Butts(1914) - veri¬
fied by Ulrich (1914).47

Keokuk or Pern Glen - same as preceding .... 47

Kindle*s Onondaga - locality of - in section at

Big Stone Gap, Va.,east side of Powell River . 25

Kindle* s section(Db.l9iO,T>.39) at curve of Powell
Valley R.R. ,1JE. of Big' Stone Gap schoolhouse . 41

I

Lake Erie - in section at Cahoon Lake - with Hyde

and Cushing . ... 11

Laurel limestone - in section. Bakers Station to

Ridgetop, ..* * *

Louisville district - Uississippian generalized sec¬
tion of - hy Butts(1914) - verified by Ulrich

(1914) . . ..* 47

Maryville Is. - in Cambrian section at Cleveland,

Va.* *.* J

Mesler and Butts - with Ulrich - section at Big

Stone Gap, Va. *»*.*•••****••* 33

Hosier’s Nos®57,57a,b,an& 59 of collections — in

section at Big Stone Gap, Va. ••••••*♦ 53

Milan,Ohio - Huron River at - sketch of probable

condition of Chagrin-Ohio shale in vicinity of • 21

exposure near reported on by Prosser - visited^. • 23
Uississippian - generalised section - of Louisville
district ~ by Butts(1914) - verified by

Ulrich (1914) « *.. • • * * 4 ^

Mississippian-Devono section - Cleveland to Duinp

Creek, Va. *. ••••••••••• 51

Mont SiI^d i ?o M « s 8®fvgr^ n e 8 e °h on -". si

Newman Is.: „ , T

in section at Big Stone Cap, Va* * • • • *

— ste. Genevieve to Tribune = Monte Sana -
in I)evono-Mississippian section, Cleveland
to Pump Creek, Va. ..

New Providence: # ^

may be - section. Bakers Station to Ridgetop,

... • .. 43

cont ftiles It W B } rSok^ff- a ?n generi¥?z§|

Mlssissiprian section of Louisville dis¬
trict by Butts(1914) - verified by
. Ulrich '(1914). 47

New Scotland: ^_

or Becraft - in section. Big Stone Gap,Va.,

east side of Powell River.2o

=s Helderbergian zone I - in section at Big
Stone Gap, Va., elbow of wagon road to
Klverton and north to Pumny line .... 2?

in sketch and description — hill at Rock Cut

and above sink of Wild Cat Creek .... oo

New York Central and St.L.R.R. - section in west bank
of creek north of - east of Pover Bay.”

Nickle Plate R.R. : q

in section at Dover Bay. •••••*.?

in section at Cahoon Creek. .

*

Uussdorfer, W.H* s

section at Eagle Cliff, in short ravine beside

home of. xa

section in gliff west of horn? of -same measured
and published by Prosser in 1903 . 1»

Ohio Jn fii S sis8ipT>iaa generalized section of Louis¬
ville district by Butts(1914) - verified by

nlrich (1914) ............... 47

in section at Karams bridge over Rocky River . 5

Ohio shale-Chagrin problem - in sketch and facts bear-
inp* on in passing westward from Bedford to Beach
Park, Ohio ..13.21

Olmsted member and shale:

in section on Big Creek, South Brooklyn,

Cleveland, 0hi8 - above raixroad bridge * * 3

in section at Karams bridge over Rocky River * ® 5
in section at Gaboon Creek •••••••••11*12

in section at Sagle Cliff - short ravine be-

side W*H*Hussdorfer’ s house •••••• l* 5

in section in cliff near Hinz’s house - same
measured and published by Prosser in 1903 -

west of Hussdorfer’s house . .. 13

in section at John Goetz’s house (Felseneck) -

same as at Hinz’s •••••••••••• 13 f 14

Olmsted-Chagrin contact - in section at Beach
Park, Ohio, by Hyde. 15

in section at Tinkers Creek, Bedford, Ohio -

with Cushing. 1/

Olmsted-Huron - sketch of possible boundary

of*.*.*..

Onondaga:

of Kindle - locality of - in section at Big

Stone Gap, Va#, east side of Powell River * 25
? Onondaga coral zone - in section at Big

Stone Gap,Va#, east side Powell River . • 25

species - in sketch and description - hill
at Rock Cut and above sink of Wild Cat
Creek...08

Ordovician and Richmond fossils - in section.

Bakers Station to Ridgetop, Term.43

Osgood lft.and sh. - in Silurian section in Jeffer¬
son Co*,Ky., according to Butts(1914) - veri¬
fied by Ulrich(1914 ).45

Ostracoda: _

in section at Bakers Station to R i dge top, Tenu • 43

in Silurian section in Jefferson Co«,Ky«, accord¬
ing to Butts(1914) - verified by Ulrich
(1914).45

roimsyxvanian - m Devono-Mississippian section,

Cleveland to Dump Creek, Va#.; 51

Plants, like Milan, Ohio, species - in section.

Big Stone Cap, Va.... 53

Portage,lower, or Genesee - in Devono~Mississip~

pian section, Cleveland, to Dump Creek, Va# • . 51

Porter Creek - in section at Gaboon Creek « • • • 12

Porter Greek section:

beds in section at Eagle Cliff like.13

red ss# in section at John Goetz # s house
(Felseneck) cf* .............. 14

red ss* in section at Beach Park,Ohio (by

Hyde), same as at 15

Powell River:

in section at Big Eton© Gap f Ya# ....... 53

section east side of. Big Stone Gap ..... 25

South Fork of - in section at Big Stone Gap,
elbow of wagon road to Elverton and north

to Durany line.. 29

North Fork of, above bridge at Big Stone Gap -
contact of Clinton and Sneedville * . . . 31

South Fork of - Clintpn-Sneedvill© contact on -
1 mile from schoolhous© at Big Stone Gap • • 35

South Fork of, SF# side of Big Stone Gap,Va# -

section at old woolen mills *..39

Powell Valley R.R. , curve of, MS# Big Stone Gap
schoolhouse - Kindle f s section (XJd*1910,p#39)

Prosser:

section measured and published by
same as at Hinz f s nouse - west

in 1903 is
of Nussdor-

fer’s house . ....13,14

exposure reported by near Milan,Ohio - visited # 23
Prout Is# - in section at Slate Cut, Ohio .... 23

Ridgetop - Bakers Station, Term., to - section -

with Bassler.43

Ridgetop shales - in section. Bakers Station, Tenn#,

to Ridgetop. 43

Richmond and Ordovician fossils - in section.

Bakers Station, Tcnn#, to Ridgetop ...... 43

Rochester member - in Clinton-Sneadville contact,

bank of North Fork of Powell River, above bridge

at Big Stone Gap, Va.31

"Rock Cut" :

in description of East Big Stone (Elverton) . • 37
sketch and description of hill at, and above

sink of Fild Cat Creek.38

Rocky River:

section at Kamm3 bridge over •••• .5

section in east bluff of, SW# of Karans .... 5

Rocky River cont'd#:

boundary at Rocky Iiiver bluff same as at Big

Greek and Roan Brook sections ##•*«** 5

south of Kaiams bridge - in facts bearing on

Chagrin-Ohio shale problem #•*****• 19

Russell:

in Devono-Mississippian section, Cleveland to

Bump Greek, Va. .*...-•*•* 51

in Carribrian section at Cleveland, Va# . * ® . 51

Rutledge dol# - in Cambrian section at Cleveland,

51

Ste# Genevieve to Tribune — Monte Sana Hewman -
in Devoiio-Mississippian section, Cleveland to
Bump Creek, Va# «#•*•«..••••... 51

St# Louis Is# - in Bevono-Mississippian section,

Cleveland to Bump Creek, V a# •«'••••••• 51

St# Louis and H*Y.C#R.R# - in section, west bank

small creek east of Bover Bay and north of * • • 7

Saluda Is# - in Silurian section in Jefferson Co* f
Ky., according to Butts(1914) - verified by
Ulrich(1914).. • . . . 45

Scolithus ss# - in description of vicinity of East

Big Stone (Elverton)'•.. . 37

in section at Big Stone Gap, Va#. elbow of wagon
road to EXverton and north to Dumpy line . . 29

Silurian section in Jefferson Co#, Ky#, according

to Butts(1914) - verified by Ulrich(1914) . # 45

Slate Cut, Ohio - section at - with Cushing • * . 23

Sneedsville Is#:

in section at Big Stone Gap, Va# - elbow of wagon
road to Elverton and north to Bumny line • 29

in section at Big Stone Gap, Va# - east side

of Powell River . # . * !. 25

basal - in section at old woolen mills, SW#
side of Big Stone Gap, Va# - South Pork of
Powell River . 39

in sketch of He Id erb e rg i an zones at Big Stone
Gap - west ond of hill 1TB• of sehoolnouse . 35

and Helderbergian limestones - mapped as Han-
^Siver^onJ * n descr ^P^ i - on 0f East Big Stone ^

Sneedvilie-Clinton contact - on north Fork of Powell
River, above bridge at Big Stone Gap, Va# . • 31

on South Pork of Powell River, 1 mile from school-
house at Big Stone Cfap, Va#. 33

South Brooklyn, Cleveland, Ohio - section above rail¬
road bridge on Big Creek... 3

Spergen - in generalized Llississippian section of
Louisville district, according to Butts(1914) -
verified by Ulrich(1914).. . • 47

:

|r

v , AiULA UiA WU ~ Uilfci* Is UcAIlGOga ■“ IXi SOCtlOH Sr”v/ Big

S to ne & ap , Ya#*«**<*»* • ••••••••• 53

Tinkers Creek, Bedford, Ohio - section - with

Cushing . ... 17

Tribune, Ste. Genevieve.to — Monte Sana = Newman -
ih Devono-Mississippian section, Cleveland to
Dump Creek, Ya# 51

Waldron sh* - in Silurian section in Jefferson Co«,
Ky#, according to Butts (1914) - verified by

Ulrich (1914).* . . . 45

Warsaw - in section at Bidgetop, Tenn* •••••* 43

Warsaw (Harrodsburg) - in Ilississippian generalised
section of Louisville district, by Butts(1914] -

| verified by Ulrich(1914) .. 47

Whit© Creek - Port Payne same as at - in section.

Bakers Station, Tern** to Bidgetop **•««* 43

Wild Cat Creek - in description of East Big Stone

(Elvorton) - with Williard * • • ..37

in description and sketch of hill at Bock Cut and
above sink of •••••••• •••••••■• 38

Williards

and Butts - locality collected from by - in

section at Cumberland Gap, 'Term*. 49

with Ulrich - section at Big Stone Gap, elbow
of wagon road to Elverton and north to

Dummy line. 29

with Ulrich - Clinton-Sneedvilie contact on
North Pork of Powell Biver, above bridge at

Big Stone Gap, Ya« .. 31

with Ulrich - Clinton-Sneedvilie contact on
South Pork of Powell River, 1 mile from
schoolhous© at Big Stone Gap, Ya. . • . ♦ * 33

with Ulrich - description of East Big Stone

(elverton) «•♦••••••••••••• 37

with Ulrich - section at old woolen mills.

South Pork of Powell Biver, SV7. side.Big
Stone Gap, Ya. ..39

Woolen mills - section at - South Fork of Powell

Biver, SW^side Big Stone Gap, Va*. 39

Hi

* vs;

*