Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
-158-
Section 11
Measured up a gully which heads in a slight reentrant
near the western end of Leonard Mountain. Units 1 and 2 dip
10° S and are truncated by higher units which dip about 7°
NW.
Top of ridge Thickness
(feet)
Leonard Formation
15. Limestone, medium to dark gray, thin
bedded, siliceous bands near top of
most units . . . . . . . . . . . . not measured
14. Siltstone, orange-brown weathering, many
limestone bands are completely replaced
by chert . . . . . . . . . . . . . . . . 32
13. Limestone, light gray, numerous chert
pebbles, 4 to 6 foot beds, but beds thicken
and thin along strike . . . . . . . . . . 46
12. Siltstone, orange to orange-brown weathering,
some beds of sandstone, many thin siliceous
bands . . . . . . . . . . . . . . . . . . 73
Lenox Hills Formation
11. Limestone, light gray, calcirudite near at
top, chert replacement common, 2 to 4
foot beds . . . . . . . . . . . . . . . 120
10. Covered, probably limestone and shale . . . . 41