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Contributed by Yale Peabody Museum of Natural History.
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Transcription
140
[see p.137 + p.107 of Nb #1]
40
Bed 5, Sect. 16 - the lower rubble + shale have
joints which run to the W and become
massive and the upper part become
shaly at the base and shale gradually
replaces most of the bs. in a distance.
300 yds. (to the point from which sect 39
starts)
40
Bed 5, Sect 16 - final grades fall off
into beddinging bs. in 1'-2' beds about
400 yds W of Bed 7. Then at ca
end by a NNE trending fault
which has drop the cliff sect.
down ca out 15' stratigraphically.
Coll. 8/23/58/8 until bed 21 type
calcium sidedy fault.
38
West of Sect. 30 - the upper portion of King's 3rd limestone (bed 11, Sect. 30) becomes
massive in 2'-3' beds - mineral flag -
forms little back-en valley. Dips on this
outcrop are from 25°-75°N
39
Bed 7, Sect. 32 is equivalent to bed 24, Sect.
30. Bed 9, Sect. 32 = Bed 12, Sect. 30
38
37
39
(8/23/58)
141
Bed 11 & 12, Sect. 32 = ± to bed 23, Sect. 16
"Keez" erosion has removed much of this
interval.
Bed 7, Sec 32 = Bed 7, Sec 31 - (it must!) +
8/23/58/1 from "gap tank gum" about
200 yds NW of King's cemetery locality
about 2 miles SE of Arnold Ranch.
8/23/58/2 - some general area as above
about 150 yds SW of cemetery locality.
weren't able to find accounts bed however.