Croton Aqueduct

The Croton Aqueduct or Old Croton Aqueduct was a large and complex water distribution system constructed as part of the New York City water supply system between 1837 and 1842. The aqueducts, which were among the first in the United States, carried water by gravity 41 miles (66 km) from the Croton River in Westchester County to reservoirs in Manhattan. It was built because local water resources had become polluted and inadequate for the growing population of New York City. Although the aqueduct was largely superseded by the New Croton Aqueduct, which was built in 1885-1890, the Old Croton Aqueduct remained in service until 1955.

Background

The island of Manhattan, surrounded by brackish rivers, had a limited supply of freshwater available. It dwindled as the city grew rapidly after the American Revolutionary War, and freshwater sources became polluted by effluent. Before the aqueduct was constructed, residents of New York obtained water from cisterns, wells, natural springs, and other bodies of water. Rapid population growth in the 19th century and encroachment on these areas as Manhattan moved further north of Wall Street, led to the pollution of many local fresh water sources. Below Grand Street, a small number of well-off customers of the Manhattan Company had fresh water delivered to them, but that company was actually more focused on banking—it eventually became Chase Manhattan—and only paid as much attention to its water activities as it needed to avoid losing the state charter that allowed it to bank. The poor and the rest of the city were forced to rely on well water, often made palatable by adding alcoholic spirits, prompting temperance campaigners to call for the municipal provision of water.