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0

Field Season 1907

I

E. M. Kindle

July 24

Livingston, Mont.

Ho. 9. Three and one-half miles south of Livingston, Mont . ,
the Yellowstone River merges from a narrow stretch of
valley - the Lower Canyon - about 2 miles long. The
river here cuts at right angles across strike of the
sedimentaries which dip to H. at 18 to 20. The granite
and gneiss at base of the section coxae in just above the
Lower Canyon or at upper end.

On west side, however, a fault interrupts the suc-
cession near base of the section and for some hundreds
of yards in vicinity cf this the exposures are imperfect
and rocks much broken up. The section as seen on W.side
of river follows.-

f Feet

a. (base) Light-gray limestone with minute oolitic
structure frequently developed, and some arena-
ceous bands 120

b. Mostly covered . . . .

2C0

o.

&.

Hard, buff
gray. Two
sils seen.

ague si an limestone mottled with dark-
corals of Zaphrentls type only fog-
Silurian?

• •

* ♦

Hard dark-gray limestone and some bands of drab
arenaceous rock with obscure bryoaoan corals and

Crthothetes cf . ohexaungensis common in one stratum
elsewhere barren . .

0 *

e. Light-gray to buffish limestone, fossils from

75 f

lower 60 feet .

•**»***#!«♦ a » 4 * « »

180

1100 •+

f. Light-buff qu&rtaito

£ * W

* * *

t 4*1

70 4

*

• Jr *

field Season 1907

• m. j£inule

July 26

Bozeman, Mont.

Ho. 10. Bridger Creek Canyon section, 4 miles E2. of Bozeman

a. Red shale and interhedded conglomerate and

quartzite

h. Buff-colored sandstone and quartzite. Ho fossils
except near top where they abound but rock does
not permit of extraction. (Garb. ? )

c. Massive to heavy-bedded light-gray limestone . . .

d. Thin-bedded, dark-gray limestone in 2-4 inch

strata separated by thin films of sandy shale.
Garb.? Foss.abt. ........

e. Gray limestone and sandy shale weathering huffish .

a-4. Brownish to gray quartzite with red jasper

pebbles in upper part

a-5. Greenish shales and covered

a- 2.. Gray, non-magne sian limestone , thin-bedded

feet

50

160

50 +■

100 +
200 4
220 ■'

a-1. Drab shale and limestone

80

BTb.p. 23

Field Season 1907

July 27
Logan , Mont .

So, 11. Section opposite Logan, I, aide of Gallatin River.

Feet

a. Black cr very cl a rk lino stone with seme shale at

base# * # • * * » * • » . » * » . . . • . , * 4 o 0

a JL

S 4k

©#**#■*

*•**«•< 4 * • *

b. Dark- colored to nearly black magnesian limestone.

Sometimes mottled huffish end blackish limestone.
Texture finely saocharoidal. ... . .120

o. Buff, sometimes reddish, sandy shale and shaly

yellow limestone near top 45

d. Gray limestone , huffish at base 10

e. Green argillaceous shale with limestone con-

cretions. Fossils abt. Bp. dis;j . etc. ..... 60

e~. Gray limestone and shale . 5

f. Buff or yellow cal care ous sandstone becoming a

shale in lower naif 30

f . Gray shaly crumbling limestone . 4

g. Hard, gray limestone in 1-4 inch strata (Garb. ) 300 *f

Beds show s pretty uniform dip of 45 to M’. and
strike of 1,28 B.

Fossils are extremely rare in a and b except a small
branching coral which is extremely abundant in certain
strata. A Favosites was found and a few brachiopods which
are pretty certainly Devonian. A piece of fishbone was
also found.

%

Sp. dlsjunotus and Lartlnia are common in the green
shale ; also small lame 11 ihranchs .

Fb.p. 27

Field Season 1907
&. 1 4 . Kindle

PWWjm n wi « m » » » ^n i n ~<i i y wa

KUg 1

Sixteen, liont.

10 . 13 .

Section from Canyon 3 miles below Sixteen st.
Sixteen.

Feet

a. Hass iv e light-grey lime stone (Canyon in this)

1000

b

Thin -bed dod , buif .gray , and red arenaceous lime-
stone, Fossils abt.in buff arenaceous beus .

Thin- be id a d , b? ui ah-gray a ome v/ha t argiliace ous
limestone with numerous fossils ......

d. Covered with t alius

e. Dirty mud- nolo rod or huffish- black magnesian

line stone ;saceharoidal texture

f. Gray limestone with 10-foot band of dark.nearly

black magnesian limestone near base ......

g. Yellow calcareous sandstone with Pro ductus . . . .

k. Green and red shale. So fossils ...

l. Yeyy hard black to gray limestone breaking with

glassy fracture . ,

140

80

60

80

120

25

50

Heddish shales and covered . 60

k. Thin- bedded dark-gray limestone. C ainb 100

l. Greenish shales 404-

The shales h seem rather local and appear to be

represented by the limestone series _i 1/4 mile above

Bolauger.

Kb. p» 34

Field Season 1907

B. 1:. Kindle

Aug . 14 . Mel rose, Mont *

So. 17. Camp Greek section E. of Melrose, Mont.

\

a. Mica schists . .

m * m

* * * 0 *

* *

c Shale and schists weathering brownish- buff

* * 0 *

c. Quartzite weathering brownish-buff

l **0~&0*9'0

d. Gray shale . .

*■•****.* m *

• »• 0 * «>

* • *

6 » Shale and tii m- b o dd&d fc rowni sh stind s t o hq ( wo a t ho red)

f & h o 1 a

«* * .LG* 00000m*

« *

&• ! Jignt-gray magnesian limestone with some dark bands
in lower half

h. Dark-red sandy shales . . .

♦ »

Buf fish-gray, non-magnesian limestone in 1-3 inch
laminae separated by thin wavy bands of shale si®,
ilar to Yegc limestone of fb.il lipsburg Quadrangle,
So fossils seen .

• *

9 9

*■9990

Buff-gray hard magnesian limestone, some shaly bands.

(There is quite clearly no break in sedimentation
between this and the following Jefferson limestone.
I'hin bands of j recur in lower 40 feet of the black
lime a to no above. )

'Jefferson limestone! Black magnesian limestone . . . ,
(A few bands of gray limestone occur through the
series bat they are of small importance with ref-
erence to the entire mass. Bo fossils seen ex-
cept the Byringo por a- like coral so common at Logan.
Also ho x el ,

Bluish gray argillaceous shale and huffish shale,
latter in lower half with some limestone bands
near middle

• *• * *

9 0 0 0 9

0*0

• 0

*00

a* Gray , non-raagne s ian limestone (Madison)

• *

0***0

Feet

600 '£■

6 .

ICO

500

20

25

3C

500

200

300

Tie section terminates on Carp Creek with the Madison. The
Quadrant quartzite however is wo 11 exposed near the railroad If. of
Melrose a mile or two.

The be da of above section dip at about 30 to 35 E. and Camp
Creek outs the strike at about right angles.

lib. p, 38

Field Season 1907

T3

J a Jl i'i I

indie

Aug . 19 Hyrum , Utah.

rovidence .

Ko.18. Fry Canyon, 4 miles S. of fiyrum and just E.of Prc

Lower limestones near end of canyon are thin-bedded.

nearly black. Dip 10

’-n

ri

Strike I. and S

Light-colored limestone appears above these

a.

Hear mouth of canyon two or three species of Spirife r and
Zaphrentis? occur abundantly in the limestone. They
seem to be Carboniferous forms.

Aug. 21.

Dip HE. 15 ; Strike H.50 W.

Kb. p. 39

Field Season 1907
E. M. Kindle

Aug. 21. By rum , Utah.

Ko,19. Section in K. fork of Blacksmith Fork Canyon, 10 miles

E. of Hyrum, Utah.

y fr'iX iT’ e e t

a. Bluish-gray, flaggy .hard, calcareous shale weathering

buff 50

b. Dark-blue limestone , finely crystalline to lithographic

in texture 400 4

c. White crystalline limestone (marble generally) in 1-3

beds and worthless from numerous joints .... 280 j*

d. Partly covered and limestone 150 j

e. Black magnesian limestone, with lighter beds rare

(Jefferson limestone) 1200

^ ' f. Gray limestone 1000 4-

* f-

I

lib. p. 42

Field Season 1907

Ur.

. i 0

*T ^

K

indie

ilo. 21.

In the canyon just north of hast iaradise Canyon
only dark-blue limestones ( Carb. ? )are exposed
below forks of the canyon.

Corals are extremely abundant in these
(the same as lower part of _e of Avon
secti on ) .

limestone s
,11. Iaradise

Fb.p.44

Field Season 1907
. M. Fin die

A ug . 2 2

Ho. 22 .

a.

b.

c.

d.

Green canyon (raradise of Weeks), 7 miles E
Paradise P. 0. .Utah.

of

Feet

'Shite to light-gray magnesian limestone, locally
altered to white quartz and sometimes with
chert hands. Sil. fossils IgO

Thin- he dded limestone , huff and brownish near top
with peculiar concretionary development resembling
finely brecciated limestone. Below this are thin-
banded blue-gray limestones. General aspect of
upper beds is suggestive of Yago limestone of
Phillipsburg quadrangle. This series mostly
covered 100

bark-blue limestone at base (lb feet) followed by
black and dark-gray magnesian limestone gen-'
erally with saccharoidal texture partly cov-
ered. Corals common in lower part 1100

Gray limestone partly covered (Garb.) 900

(

N ,

/ 4

• V*

A.

\a/

^ ViUa

\ v »«*

U

V

irb.P‘45

Field Season 1907

S. M. Kindle

Logan, Utah.

P'7,

Logan Canyon. The lower beds exposed at west end of
Canyon below the power-house are the black Jefferson
limestone and! dip strongly to S.

Crossing the E.& 3. axis of the syncline the following
section is seen some 8 miles above Logan.

Feet

a. (base) Lark bluish-gray hard magnesian limestone

b. Light-gray or white magnesian crystalline or sub-

crystalline limestone more or less massive.

Crinoid stems common, also Haly sites and other
Sil. fossils, but difficult to extract 275

c. Lark -gray to black magnesian limestones with

Haly sites common, also one sp. Pentamerus

oblongus 400

d. light to dark-gray , largely non-magnesian, frequent-

ly thin-bedded line stone , and interbedded gray

and some brownish shales. Limestone with

Martinia . 280

e.

f.

Dark-gray to black heavy-bedded magnesian
Cray, mostly non-magnesian limestone (Carb.

limestone 260

) . . . .1000

This Logan Canyon section differs from that of Green
Canyon in the absence of any separating formation be-
tween b and c.

The boundary between e_ anf f is not sharply marked
and is rather difficult to fix.