Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
5) 8.2
Interbedded clayey, blocky silt, silty shale,
minor clay shale and a few layers
OB stained sandy silt or VFG sand.
Blocky laminated clayey gray silts
predominate. At top is thin OB stained
VFG sand+silt with liquidite silt
assoc.
6) 16.7
Interbedded clayey silt, gray to dkgray shale +
silty shale and scattered thin beds of
'silty VFG sand that are commonly
weathered OB. In this interval shale
layers more numerous, clayey silt layers
thinner + aggregate less than 50% prob.
7) 8.0
Sand, fq to vfg locally silty with some
interbeds of gray clay shale in lower
1.5. Weathers yellowish gray and
has, locally, large calc.concretionary
masses, generally flattened in plane
bedding but locally more spheroidal.
Long clasts, up to 12.0, thicknesses
locally up to 3.0. Typical "calcrete type"
greywacke.
8) 17.6
Sandy-clay grading upward to clayey sand, gray,
weathers yellowish gray some OB stain,
has somewhat larger plant frags than
most of section below.
9) 15.5 - ?
Sand, fq to vfg gray, graywacke, local
light orange stain. In upper 5-7' keep
and north cone masses holding rim.
locally coalesce to form rim rock but
commonly single up to 15'+ across
and 8' high.
Top of S end of bluff.
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