Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
"Our work indicates that the base limestone series had best be divided into
three zones with distinct names. The upper
lagers beds 8 can be termed the
Brandy Grove series because they are
well shown and are most fossiliferous at
Brandy Grove to Indian Cove.
The middle series, Lagers beds 3-7
are practically unfossiliferous and may be
called the St. Albans series because
all these beds are seen in St. Albans
Cliff down to the shore on the road to
Coke Springs Lytt house.
The lower series includes Lagers beds
1 and 2 and may be called Rosed Cove beds.
These lower beds make a good contrast to upper
lagers. Beds 3 are soft and break down while
the balance of the series again stand in
vertical cliffs.