Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
| www.biodiversitylibrary.org
Transcription
547A includes some very friable gray to
grayish olive shale, the edge chipping
and in the slings. The shales are very splint-
ery, although not extremely so, they contain
an abundance of little round or elongate
nodules or nut balls indicating a local
formation & mud flats. Strike N. 18 deg W dp
40 deg N. 70 deg E. Fossils are scarce.
Orbiculoidae occasional
Camarotoechia
"Mediolopsis platyphyllus" rara
Otenodonta
(2) Loperdita (perhaps a mud ball?)
Hyolithes or a fish spine
- 547B. The 20 feet of shales of 5.4.7.B are less
friable than those of B and with a judson-
mannue of gray rather blue-gray olive color.
They agree in the thinness and in general
nature as well as in being splintery.
The last named character is rather vari-
able in places faintly discernable holes
in places the splinting develops almost
into flat cleavage. Typical network occurs
in spots in the shales, the development
of vertical replanturing, or of normal beds
while dependence appears to depend on the
proximity of the trap.
Fossils are frequently very scarce
in most places throughout the shale
except for a few linear seams, which
contain great numbers of fossil chiefly
little ostracods (Bumella? Beyrichia?) and
crink joints with a few tentaculites and
camarotoechia. And some contain great
numbers of Chonetes donysii but only a single
specimen was found in the shale situated this
seam after several hours search. A
sample of seams contains lamellibrancha
chiefly Grammysia ringulata or the
fauna is
Orbiculoidae occasional
Camarotoechia common
monocamps (possibly criniferopony)
Chonetes donysii rara (abundant in 1 seam)
Dalmanella yp.
Otenodonta? occaisional
Tentaculites
cornu/tes serpularius
Homalomus yp rare
Alcyones or Phacops (typical) occasional
Beyrichia 2ar 3 spp. abundant seams
Primitia
Crinoid segments
the fauna are distorted and elongated in
the direction of the dip and splintery.
A couple of calcareous seams or rather
linear causes contomi seams (not collected)
very large Astropoterella nearly 2 inches common?
Hyponites? one, 2 miles
Rynchonella (Camarotoechia?) uncommon
53.3 A
In the roadbed just S.W. of the middle
of 5.3.5 M., there near Mr Joseph E McAr's
farm some thin gray argileaceous shales and
thin sandy shale, striking north 75 W and
dipping about 40 deg N. 15 deg E. There is quite
a thickness of shale exposed, the edge of
the shale chipping out for a linear dis-
tance of 140 feet along the ground normal to
strike complete thickness (sin 60 x 140 ft.)
and this is only a small portion of the total
amount of shales which appears to be covered.
Fossils are very rare and include (5.3.5.2)
Chonetes donysii
C yp (small, coarser striae)
Grammysia unguia (small, smooth var.
Crinoid joints.