210 
The American Geologist, 
October, 189^ 
Musconetcong mountain on the south, it is possible to trace a 
well connected series of glacial deposits, embracing all those 
which I would refer to the first group. This covers the localities 
of Oxford Furnace, Oxford church, Little York, Brass Castle, 
Washington, Pleasant Valley, probably Mt. Bethel, though this 
place was not visited, Roxburgh, Harmony, Lower Harmony, the 
country northeast and east of Phillipsburg, and also southeast 
ij O-nfida Vmed Sand.st I I Elf»a.t 
II I I ll H.RShaleVSlaU refer to 
JLSilai" LcmeiIor.es | Tide m-ate 
"L_V-j Gnec&toid RocKs 
to Springtown, Hughesville and Musconetcong mountain at a 
point two miles south of Bloomsbury. 
Avoiding as far as possible the stream valleys, the higher 
divides were explored. These deposits were found at the follow- 
ing levels: 
Oxford Furnace 520 ft. Little York 850 ft. 
Brass Castle 700 " Washington ...500 " 
Harmony 560 " Phillipsburg, N. E. . . 375 to 460 " 
Musconetcong mountain, for a distance of three miles, at 700 
to im feet. 
