Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
| www.biodiversitylibrary.org
Transcription
South East of Church at next comer
is Cliver Black shale, this black
shale is exposed also N of church
corner.
From house N of church, going
up the road,
While on E side of road, white
clay on left. From middle
part of rise hill is Cliver
black shale on both sides of
road, presumably dipping NW.
House rooms at top of hill on W
side of road. No exposure here
but cherty rock occurs where road
turns off to east. Rock dips strongly
W. That is very thin strips
x 2 chains wide. Dissected to be
Lower West Union.
Further up down the hill
along upper third of hill
above, is sand rock with
small celled foraminifera,
East of the road junction the
Lower West Union rock ascends
the hill and at the same time
slopes northward.
At some 5 feet below the level
the strong bend of the road
northward, there is a white
clay, as yet unexamined.
Just before reaching strong bend in
road towards east, white clay
film from west which shows up,
fronting strong bend in road to mi
where road descends the hill, there
is Lower West Union dipping
strongly NNW, undulated at lower
part of built by White Clay
arch formation partially.
Hill runs N of roads along edge of
this hill bounding the road
occurs white creek chalk and clay
at scheme SE and runs back
limbering, very slightly lower
West Union.
Then runs rises eastward along
long hill slope exposing Bellport
near base with Bransfield debris
begin up and Cincinnati rocks
seen top but not actually in site,
Some Cincinnati rocks
show up on that part of road
which as Cline's hill SE in direction.
When road runs E there are no
opposes until bend of road is
reached where it turns at right
angle northward. Here very
strongly tilted Cincinnati
rocks near,
Road turns NNE, then ENE.
Cincinnati debris occurs at bend,