- Catskill Aqueduct
The Catskill Aqueduct, part of the
New York City water supply system , brings water from theCatskill Mountains to Yonkers where it connects to other parts of the sytem. It begins at theAshokan Reservoir inOlivebridge, New York , in Ulster County. It then heads south, flowing towardOrange County, New York , and then crosses underneath theHudson River toPutnam County, New York . Theaqueduct transports water from Ashokan as well as the Schoharie Reservoir, which feeds into Ashokan. From the Ashokan, the aqueduct traverses in a southeasterly direction through Ulster, Orange, and Putnam, counties. It crosses convert|1100|ft|m below the Hudson River bed at Storm King Mountain in Orange county. It crosses into Putnam county on the east side of the river at Breakneck Mountain. [ [http://books.google.com/books?id=KIkHuzvZTGYC&pg=RA1-PA190&lpg=RA1-PA190&dq=catskill+aqueduct+hudson+river+crossing&source=web&ots=ZSUd0eX9MN&sig=j_GpWaGRg34r1B8TRcllpi2oC88#PRA1-PA189,M1 The Hudson River Guidebook By Arthur G. Adams] ]The aqueduct then enters
Westchester County, New York , and flows to theKensico Reservoir , which also receives water from the City'sDelaware Aqueduct . It continues from the Kensico reservoir and terminates at theHillview Reservoir inYonkers . The Hillview Reservoir then feeds City Tunnels 1 and 2, which bring water to New York City. If necessary, water can be made to bypass both reservoirs.Construction commenced in 1907. The aqueduct proper was completed in 1916 and the entire Catskill Aqueduct system including three dams, and 67 shafts was completed in 1924. [ [http://www.dukelabs.com/Abstracts%20and%20Papers/CM2000c.htm Geology and history of the NYC water supply system - Merguerian, 2000c ] ] The total cost of the aqueduct system was $177 million. [ [http://books.google.com/books?id=s2MEAAAAMAAJ&pg=PA43&lpg=PA43&dq=bryn+mawr+siphon&source=web&ots=K3rf5VKOTH&sig=hxW9W7BNEZrBfSPc5EaPaBcmmJQ#PPA23,M1 Catskill Water Supply: A General Description and Brief History] ]
The convert|163|mi|km|sing=on aqueduct consists of convert|55|mi|km of
cut and cover aqueduct, over convert|28|mi|km of grade tunnel, convert|35|mi|km of pressure tunnel, six miles (10 km) of steel siphon, and convert|39|mi|km of conduit. The 67 shafts sunk for various purposes vary in depth from 174 to convert|1187|ft|m. [ [http://www.dukelabs.com/Abstracts%20and%20Papers/CM2000c.htm Geology and history of the NYC water supply system - Merguerian, 2000c ] ] Water flows by gravity through the aqueduct at a rate of about convert|4|ft/s|m/s. [ [http://www.greatachievements.org/?id=3610 Water Supply and Distribution Timeline - Greatest Engineering Achievements of the Twentieth Century ] ]The Catskill Aqueduct has an operational capacity of about 550 million gallons per day north of the
Kensico Reservoir inValhalla, New York . Capacity in the section of the aqueduct south of Kensico Reservoir to theHillview Reservoir inYonkers, New York is 880 million gallons per day. [ [http://www.eserc.stonybrook.edu/cen514/info/NYC/WaterSupply.html New York City water supply system ] ] The aqueduct normally operates well below capacity with daily averages around 350 - 400 million gallons of water per day.Trivia
* About 40% of New York City's water supply flows through the Catskill Aqueduct.
References
See also
*
Delaware Aqueduct
*New York City Water Supply System
*Frank E. Winsor the engineer in charge of construction of convert|32|mi|km of the Aqueduct.
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