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Contributed by Yale Peabody Museum of Natural History.
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Transcription
(150)
5V52) Ls, organic lag; light gray weathering
Products: crushed cobblews; upper 2"
rich in siliceous cement + fossils.
2 1/2'
53-54) Alternation of limestones like
52 and siltstones like 45; at least 4 alternati
intervais are poorly exposed; siltstones have silica
bands.
12'
# 55) Calcarenite - cobbles 3" to 6" diam; about
5% or less siliceous rocks in this unit.
8'
This seems to form the base of King's basal
Leonard Bt.
8/1/57/3, float found near bed 43. I believe
it has come down from either the lagging
bed 50 or in the Leonard above.
8/1/57/10 - NE q Section 20, 200 yds, from bed
#24 - one light colored block, gray
ones are in matrixy rock
afternoon (8/1/57) walked along Wolfcamp
central to the NE about 1 mile. The upper
whole of the Wolfcamp is poorly exposed along
here and even the basal conglomerate of the Wolfcamp
is incompletely exposed.
The Dimple is exposed in a window (?)
on the Dugout Creek Thrust sheet. A Dimple
is the apparent source for much of the
lower Wolfcamp Congl at this point.
Collection 8/1/57/8
Daymond ? is exposed just to the SW of
the Dugout; (8/1/57/9) is from sandsilt
in Daymond.
SW NE
Section 20
#24 +
Shale
conglo
Daymond / Dugout \
// in Wolfcamp.