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Contributed by Yale Peabody Museum of Natural History.
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Transcription
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Section 17
Measured from the top of the intrusion up the south side
of Hill 5816, Hess ranch horst, to a point about three-quarters
of the way to the summit.
Top of measured sequence Thickness
(feet)
Lenoxhills Formation
18. Limestone, dark gray to light brown
weathering, dolomitic, 2 foot beds, coll.
17-18, Schwagerina tersa, Triticites
joensis (reworked) . . . . . . . . more than 12
17. Dolostone, brown-gray weathering, 6 inch
to 1 foot beds, granular texture, silty
throughout, fossil molds common,
chert pebbles common in upper portion . . . . 40
16. Sandstone, brown weathering, 6 inch to 2
foot beds, a few chert pebbles, well
sorted, medium to fine grained quartz
sand . . . . . . . . . . . . . . . . . . . . . 20
15. Conglomerate, like unit 13, but in 2 to
3 foot beds, upper portion is dominantly
gray quartz sandstone, coll. 17-15
(upper part), Parafusulina linearis,
Schwagerina nelsoni, S. diversiformis,
Pseudoschwagerina tumidosus, P. texana? . . 18