1st -23d Report of the State Geologist Volume a - 21.cNew York State Geological Survey
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Author: New York State Geological Survey
Page Count: 30 pages
Published Date: 01 May 2012
Publisher: Rarebooksclub.com
Publication Country: Miami Fl, United States
Language: English
Type: PDF
ISBN: 9781231376652
File size: 39 Mb
File Name: 1st.-23d.Report.of.the.State.Geologist.Volume.a.-.21.pdf
Download Link: 1st -23d Report of the State Geologist Volume a - 21
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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1903 Excerpt: ...channel quite certainly added its waters to the flood which cut the blulfs at Hanlius Center and those south and east of Kirkville. The waters which occupied the huge channels at Syracuse may possibly have cut the banks on the two hills east and southeast of East Syracuse, and at the last probably poured directly into the early Lake Iroquois. The Verona-Greenway channels were probably cut at the same time as these at Oneida and Canastota. These carried for a long time the glacially impounded waters held in the valleys of Oneida, Cowaselon, Chittenango and possibly Limestone creeks. It is not certain whether the low channels between Oneida and Chittenango carried any waters derived from the west of Limestone and Butternut creeks. It is probable however that the low channels west of Chittenango carried in addition to the local waters the eastward drainage of the vast Lake Warren, which then occupied as much of the basins of Ontario, Erie and Huron as the ice sheet had then deserted. Work in completion of channel investigation The channel phenomena in the extreme limits of the territory, east and west, remain unstudied. In the area between Rome, . Utica and Clinton must lie the easternmost scourways of the entire series. These must have carried to their destination in the Mohawk the waters which cut the channels on Eaton hill, and at least the higher ones on West Stockbridge, Cranson and Eagle hills.1 West of Syracuse and reaching past Rochester to the west side of the Genesee valley are capacious channels which are probably later in time than those already described. It is the intention of the writer to make these two sets of undescribed channels the subject of another paper. Thereafter it will be in order to make a summation of all the data in a single writi...
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