Bulletin 5
Bulletin 5
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Survey, 188:*, p. 356.
t Third Ann. Rep. U. S. Geol. Survey, 1883. p. 356.
X Johnnon : Tran>«. N. Y. Acad. Nat. Sci., vol. i, 1882, pp. 77-80.
^ Third Ann. Rep. U. S. Geol. Survey, 1883, p. 3ij5.
NORTHWARD FLOW OP CAYUGA RIVER. 3o3 * ' It haB been a somewhat current assumption that this valley, in common with tVie adjacent ones, is an old river trough that discharged southward through the SuBqiiehanna. If this be true, and no allowance \ye made, on the one hand, for drift06 ...it8 in the bottom of the lake, nor, on the other, for glacial corrasion, the total tiepth of the drift under the crest of the moraine nmst exceed 1,000 feet, and this «lei>th, approximately, must continue Car down the Chemung-Susquehanna valley/' Now that much of the depth of the lake is proved to be due to ice t^rosion this loses some of its force, but even now th^ depth of drift must needs be nearly 600 feet, which of itself is almost incredible. There are, l:io^'ever, abundant and sufficient reasons to show that the river course was north and not south.
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You can find similar books in the "Read Also" column, or choose other free books by Geological Society of America to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Survey, 188:*, p. 356.
t Third Ann. Rep. U. S. Geol. Survey, 1883. p. 356.
X Johnnon : Tran>«. N. Y. Acad. Nat. Sci., vol. i, 1882, pp. 77-80.
^ Third Ann. Rep. U. S. Geol. Survey, 1883, p. 3ij5.
NORTHWARD FLOW OP CAYUGA RIVER. 3o3 * ' It haB been a somewhat current assumption that this valley, in common with tVie adjacent ones, is an old river trough that discharged southward through the SuBqiiehanna. If this be true, and no allowance \ye made, on the one hand, for drift
What to read after Bulletin 5?
You can find similar books in the "Read Also" column, or choose other free books by Geological Society of America to read onlineMoreLess
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