Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
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material. These do not appear to be
true concretions but consist of a
more or less spongy mass of radiating
fibrous crystals of -? (maybe aragonite)
May have concretionary nodule in
center.
(170F + 180F) 10'10" Grey brown sandy shale
becoming glauconitic & somewhat
more sandy at top.
(190F) 5'5" Grey brown sandy shale
decidedly glauconitic.
(200F) 5'5" Lower part grey brown
sandy shale. Upper 3'
considerably sandier & browner
weathering buff, it is a loosey
sand. This split in lithology
taken as base of true Fox Hills.
(210F + 220F) 10'10" Light brown sand, rather