Cazenovia Creek Ice-Control Structure

Cazenovia Creek, in Western New York, the largest tributary of the Buffalo River. Breakup ice jams form along the lower basin nearly every year during mid-winter or spring thaws, and ice-jam flooding occurs in the City of Buffalo and the Town of West Seneca about every 2-3 years. This report describ...

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Bibliographic Details
Main Authors: Lever, James H., Gooch, Gordon, Daly, Steven F.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
Format: Text
Language:English
Published: 2000
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA382170
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA382170