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Transcription
702 Bridge level across Gunst creek, 9th
G. M.
Section at Gunst creek,
6 ft up to lowest Stagh. mayrillensis
13 ft up to bridge level, face of Nott's prs.
9½ft to top of heavy l, with D. emacrata.
Gunst creek level abundant.
.690 Base of not l type at Gunst bridge.
722 Bridge over Gunst creek at 10,15
770 S V S head. First house Ey bridges
740 At bridge over branch of Gunst creek,
4 mi E of Shelbyville.
726 To top of heavy rock, 2ft thick, like
that considered at base of not l type
section at Bridge over Gunst creek,
but good strag. mayrillensis
occurs beneath, with high occurence.
850 Plat. lyng abundant up to this level.
860 Camparatively impsiliforms sec-
tion since last record, a and,
appearing, up to R. A jamison,
about 1 mi. West of Clay village, west
of deep valley of branch of Tick creek,
43½mi East of Shelbyville.
847, Just before Machinery southend
of sharp turn in road, 3¼mi Ws
of Clay village.
805 Bridge east fork up bend.
815 ft Plat. lyng, very few, but large
17½ft up to bridge, ½ mi W of Clayville,
creek level at bridge, with Strag.
mayrillensis 5 ft above creek,
in lumps full of hygrymae and
few Strags. mayrillensis. Mr.
Dolanmella noticed but my
short stretch made here.
This cannot be near upper part of
Farm but where Plat. lyng and
Strag. mayrillensis come close
together.
875 road corner in Clayville at 12,15
888. Platysta? sp. plat. lyng layers,
Planchartrema dentatum, What lens-
you is this. Followed by layer of
nodular saddle.
945. Apparently the same flat lyng layers
as at 888. There appears to be a
north and dip equal to that of the
road between here and bottoming hill,
Then there is rocks crossing the road
with strike N 25 E, And dip 20 east.
This strike cutting Stiglephmena
mayrillensis.
985. Strag. splacated thick layer of
limestone full of Dolanmella
emacrata resembles the heavy
bed here recorded above and at
first considered as face of not
l type bed.
1015. Sandy Garrend looking rock with
limestone layers with Del. emacrata
= ½th of first size