Pennsylvania Geology Final Report Volume 1 1981

808 GEOLOaiCAL SURVEY OF PENNSYLVANIA.
poor fragment of an Orthoceras was found in
1000' N. of the tavern at Scherersville,
a loose rock
Fossils in Northampton county have been got from the
middle and upper limestones; thus—Maclurea (or Enom-
phalus) in Dech's quarry, IJ m. S. W. of Bath ; probably
of Chazy age. —Encrmal stems, not far N, E. of last;
Trenton. age\ also abundant in the upper beds of Krock's
quarry at Christian spring ; also, from there eastward to i
m. E. of Nazareth, wherever the limestones are weathered;
also, in Russ' quarry, just S. W. of Nazareth (here in company
with a few Orthis testudinaria); also, on Knecht's
farm close to Buslikill creek, ^ m, S. W. of Stockertown
(here in company with Clicetetes lycoperdon and 0. testudi-
naria)\ also, at quarry opposite Churchville church, in
upper weathered rocks (the lower beds affording LeptcBiia
sericea, 0. testudinarla, and O. pectinella)\ also \ m. E. of
Keller's tavern (two or three encrinal outcrops). All these
exhibitions prove that encr inal stems m.2LY^ iheTrenion outcrop.
— In the quarries on the Delaware just S. of Howell's
cotton mill are found Leptcena sericea, Orthis pectinella,
O. testudinaria., Strophomena alternata.^ Chcetetes lycoperdon.
and one or two other undetermined forms, lying in
colonies of from 20 to 200 individuals, and not scattered
through the rocks, which are evidently of Trenton age.