Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
(836-5 to 840) interval chiefly a dirty
clay silicious to (illegible?) claystone with
one streak of dirty flint clay. (GC-166)
Flint is fragmental - appears about
half way between reworking while soft
and reworking while hard.
(565-4 to 571) interval chiefly silicious
to silty semihard clay with considerable
Fe and minor lump inclusions.
specimen (GC 16.12)
16/12 shows contact of
homogenous silicious semihard and
overlying fragmental zone.
* GC G11 is at base of fragmental zone + shows
large fragments of silty claystone and/or fracture
filling it down.