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Contributed by Yale Peabody Museum of Natural History.
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Transcription
(50)
100 yds to the east the 8,9 and maybe the 7
beds are gouged out & and a chert quartzite
Conglo fills a 40 to 45' depth channel. I
take this to be an old river channel. It
has the appearance of the typical meandering
conglo of the western party, the later.
This channel is about 130 yds wide in
outcrops.
(12) Dolostone, Brown weathering, 6" to 1'
beds, Locality the Beds on small road
Ese. 36' 5/19/57/13
(13) Sandstone; light brown to tan weathering.
grease of chert+quartzite conglo pebbles.
3'-1'-beds, 6'
(14) Conglo; 5" cobbles, mainly very limited,
with sandstone lines of it's mostly
chert + quartzite near base, seems to be
near top ; 16'; This is like conglom
erate channel; little no. 6s formed part.
(15) Covered, 15' red soil.
(31)
(16) Conglo; mostly dark gray & light
gravelly; sandy clay matrix as well.
(mostly a pebble conglo.)
2'
(17) Covered, 15', red soil.
(18) Calcarenite, chalky tan weathering,
2' to 8' beds, 3'; 12" Cobbles
(19) Covered, Red soil, 12'
(20) Calcarenite; 5', 10" Cobbles, light to
tan/gray, no cobbles.
Top of Beds found Conglomerate
I named draw the top of the Waycamp (based
on Geology) at the top of the Calcostone
unit, and the base of the waycamp at the
base of unit 7. The 2' conglo (#15) is
dead to claim but it seemed to have
only ls of the 8 & 9 types in it. The
rest of the conglom has a great deal of chert.
W E
not is pebbles, except
main edges