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. 
