J. D. Dana—Taconice Rocks and Stratigraphy. 218 
er nestone, nearly east-and-west in direction, indicat- 
= ANA ines of faulting, transverse to the preceding. Fig. 5 
a iy? a section across the beds from south to north, 
ough the two belts. The southern belt has the overlying 
ee mile north of Gallows Hill, at 4, there is the south 
a thin hea er schist ridge. In the view from the southward 
fisk: 5 atum of schist having the eastward pitch of the sur- 
» OVerlies, like a blanket, a bed of white limestone, as repre- 
Wertical ¢ g. 7. The limestone directly below the schist has a 
ront with some schist-capped recesses; but south of 
8. 
e Whine, £. : 
thi : 7 
dlopin, luff portion it spreads widely as the rock beneath the 
of ¢ 8 fields, showing itself in occasional visi e zz 
i i ° to the 
show *E., the strike being N. 19° W. The section does not 
: “lee the ridge is synclinal, anticlinal, or monoclinal 
ault 
is a small ridge 
© the northwest of the last locality at 5, § 
i fourth of a mile 
OF wal. 
schist, named Turnip Rock. lt is about a 
