Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
AIN-49-04 Mossey Creek - Dutch Cri hogback
1 clay bed comes in here - about 2' of good clay and
some argill. siltstone & sandstone at base. Bed
pinched out about 40 ft N & 15 ft south.
Identity? no bessel bentonite but its low in section
2 platy beds, underlain by irreg. bedded, rusty weather
ss with flinty, bentonite like layer capping it.
3 main clay bed in here, bentonitic-clay at base, for
short distance. Between 2 & 3 this horizon marked by
wt zone in coalesced overlying & underlying ss. Local
clay pebble cgl also marks it, but to of this type
zone and relations of upper obscure.
4 Platy beds - in place. First clay bed in here, swings
over rim and causes swale. In and out S of
here about halfway to 3.
Bdga. platy beds thin ledge ss (typ 2nd?) then
slope, with platy ss ledgy at base (3rd), the
2nd bentonitic layer of 3rd shale crops
short distance up slope above it.
Below 3rd ss slope that includes discont.
Then ledge cgl. Lytle with Fe-stone cap,
about 10', then slope of lb. ss & redclsh
then 40' ledge cgl. ss, red wash at
base. This massive ledge is local.
North of swale the main clay bed pinches
in and out between a thin(?) 1st Glacierzrn
and thin overlying Dakota. These 2 ss.
make up the rim. Clay bed locally
represented by siltst & silty clay.
10.