D. P. Penhallow—Herbage of Permanent Meadow. 395. . 
S. 15° to 25° W. Unstratified drift, striated loose stones and er- 
_ TYatics are uncommon; the most notable of the latter was found 
on the line of the West Shore railroad about one mile below the 
their deep quarries along the river, especially the quarry near 
the town showing the unconformity ; second, the complication 
of synclinal and anticlinal on the line of the West Shore rail- 
Toad ; third, the new channel at Eddyville and the limestone 
Synclinal Opposite to it. A large quarry is opened on the river 
bluff a mile north of the ma , and several others in a very 
interesting region between Whiteport and Rosendale south- 
West of our limits. ‘Two railroads and the river boats afford 
fasy access to the town; local tuys are constantly running up 
and down the creek between Rondout and Eddyville; and th 
Wallkill Valley railroad serves for longer excursions. 
Cambridge, May, 1883. 
ArT. XLVI.— Notice of Agricultural, Botanical and Chemical 
Results of Expervments on the Mixed Herbage of Permanent 
Meadow, conducted jor more than twenty years in succession on 
the same land; by D. P. Pennantow. Phil. Trans. Roy. 
Soc., Part IV, 1882. to. 
e entire volume will well repay careful 
