62 J. D. Dana—Hudson River Age of the Taconic Schists. 
of Willow Brook, S. side of oy od pea , schist N. 16° E., 
dip 60° E., and $m. N.E, of last, N. 14° E., dip 50°-60° EK. At Stan- 
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layer of grayish Sevag in the schist, 25 to 30 feet ‘thick, trike 
of slate and quartzyte, N. 16° E.; dip 60° E; ; just north of river — 
4m. W. of Bangall, schist N. 28° E., dip 75° E., and here a fault 
the limestone adjoining being n nearly horizontal. Between Pine 
Plains and Stissingville, much of the limestone nearly horizontal, 
with small eastward dip, et aa to westerly. So : Stissingville 
near railroad, limestone N. 12° me E., di ° 'W., and 
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50° E. (average); 3 m. S. of Furnace, adjoining Taconic Mtn., 
limestone asp schist N. 15° E., dip 50° EL 
Shekomeko Limestone area.—The area  ceuies the valley 
between Husted station and Pulver’s Corners. Thence it extends 
the road from Bangall enters the Mori In a cut just northeast 
of Husted station, limestone N. 25° E ay! 35° E.; 3 re in next 
‘ so 
of the limestone area, slate, near road to Ban ngall, 'N. 20°-32° K., 
Sag in aim gan", 10°-50°W. , but $m. to the west, it is 40°-50° E. 
. Fis “Millerton belt 
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E., dip 70° to 80° Lae fine-grained, fissile rock, of little 
luster, fusing B. B. to a slightly magnetic age, and oe 
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atteawan, at junction of schist and limestone, N. 52° E., dip 
70° E.; $m. of Matteawan, Panag mag N, 42° E., 70° -80° E.; 
