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Lake Gilead

Croton WatershedHudson Valley, New York geography stubsLakes of New York (state)Lakes of Putnam County, New YorkProtected areas of Putnam County, New York
Reservoirs in New York (state)Reservoirs in Putnam County, New YorkWater infrastructure of New York City

Lake Gilead is a 116-acre (0.47 km2) controlled lake located in Carmel Hamlet in Putnam County, New York. Originally known as Dean's Pond, it is 0.8 miles long, has a mean depth of 43 feet (13 m), and a maximum depth of approximately 120 feet (37 m). The lake is located within the lower Hudson River basin in the Croton River watershed. Lake Gilead is part of the Croton Watershed of the New York City water supply system. A dam and spillway are located on its southern end, with a 500' shore-to-shore set-back restricting boaters from the area.Recreational use of the controlled lakes falls under DEP regulations. Fishing and self-powered boating are allowed with a valid DEP permit and New York State Department of Environmental Conservation-issued fishing license. Swimming is prohibited. Ice fishing is allowed on Lake Gilead during the winter. Fish species present include (but are not limited to) largemouth bass, rainbow, lake and brown trout, chain pickerel, yellow perch, and panfish. In the 1990s a local fisherman illegally introduced northern pike, though they are rarely caught.

Excerpt from the Wikipedia article Lake Gilead (License: CC BY-SA 3.0, Authors).

Lake Gilead
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N 41.397777777778 ° E -73.675555555556 °
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Rock Road North 47
10512
New York, United States
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Croton Falls Reservoir

The Croton Falls Reservoir is a reservoir in the New York City water supply system in the Putnam County, New York townships of Carmel, and Southeast, roughly 50 miles (80 km) north of New York City. Part of the system's Croton Watershed, it was formed by impounding the West Branch and Middle Branch of the Croton River, tributaries of the Croton River, which flows into the Hudson River. Placed into service in 1911, the resulting reservoir has a drainage basin of 16 square miles (25.6 km²) and can hold 14.2 billion US gallons (54,000,000 m3) of water at full capacity. This includes all bodies of water that flow into the reservoir except for other reservoirs. Water sources in the basin include Michaels Brook, and Lake Gilead, one of three controlled lakes in the Croton Watershed. The reservoir is split into three portions by Putnam County Routes 35 and 38, which cross it with causeways and bridges. Water from the reservoir flows into Westchester County, New York, through the Muscoot Reservoir and New Croton Reservoir before entering the New Croton Aqueduct. Water in the Aqueduct flows through The Bronx into the Jerome Park Reservoir. In January 2007, the New York City Department of Environmental Protection reportedly began a $74 million project of improvements to the Croton Falls Reservoir and the Diverting Reservoir. The upgrading and rehabilitation is part of the city's effort to comply with state and federal dam safety regulations. At the Croton Falls Reservoir, the spillway - the structure that allows excess water to leave the reservoir - will be widened and deepened. The nearly 100-foot-tall (30 m) earthen and masonry dam will be resurfaced, a new bridge will be built over the redone spillway and various mechanical items, such as valves, will be replaced. In addition, cables anchoring the dam and spillway to the bedrock will be installed. The work will require the reservoir to be deepened 4 feet (1.2 m). The connecting channel between the two reservoirs will be emptied, inspected and dredged. Construction at both sites is expected to continue until Jan. 31, 2010.

West Branch Reservoir
West Branch Reservoir

The West Branch Reservoir is a reservoir in the New York City water supply system. Formed by impounding the upper reaches of the West Branch of the Croton River, it is located in the Putnam County, New York, towns of Kent, and Carmel, about 50 miles (80 km) north of New York City.Put into service in 1895, West Branch is one of 12 reservoirs in the system's Croton Watershed, and second northernmost. It receives the flow of the upstream Boyds Corner impoundment, and, when needed, of Lake Gleneida, a controlled lake in the City supply system. Primarily, however, it receives water from the much larger Rondout Reservoir in the Catskill Mountains on the west bank of the Hudson River via the Delaware Aqueduct. It serves as a supplementary settling basin for these waters before releasing its flow back into the aqueduct to be carried to the Kensico Reservoir in southern Westchester County.West Branch Reservoir has a 20 square mile (32 km²) drainage basin, and can hold up to 8 billion US gallons (30,000,000 m3) of water at full capacity. It consists of two basins, separated by State Route 301.During drought periods the West Branch also receives water pumped in from the Hudson River by the City's Chelsea Pumping Station near Beacon in Dutchess County, some 65 miles (105 km) from New York City. It was used for this purpose during the 1965–66 and 1985 droughts, as well as during May 1989. Water withdrawn from the West Branch ordinarily flows via the Delaware Aqueduct to the Kensico Reservoir in Westchester County for further settling. There it mixes with additional Catskill system water carried by the Catskill Aqueduct before entering tunnels that carry it to the Hillview Reservoir in Yonkers, at the City's northern boundary. There it enters the city's direct water supply distribution system, flowing via tunnels through the boroughs of The Bronx, Queens, and Brooklyn. The water finally stops at Staten Island. Water in excess of New York City's needs at the West Branch Reservoir goes over its spillway and into the West Branch Croton River, which is captured downstream by the Croton Falls Reservoir.

Tilly Foster Mine
Tilly Foster Mine

The Tilly Foster Mine was an iron mine in the Town of Southeast in Putnam County, New York, USA, two miles west of the village of Brewster along Route 6. The Tilly Foster Mine was named for Tilly Foster, who bought the land that the mine was on from George Beale. After Foster's death in 1842, the property passed through several hands before it came into the possession of Harvey Iron and Steel Company. The mine opened in 1853 and employed large numbers of Irish and Italian immigrants. The jobs available at the mine played a large part in bringing immigrants to the town of Southeast. Workers were known by numbers rather than names, because the names of immigrants were considered too difficult to pronounce. The mine reached its peak of production in the 1870s. It was 600 feet (180 meters) deep. There were 300 miners employed and they were producing 7,000 tons (14,000,000 pounds) of ore per month. The main minerals were magnetite and chondrodite. The iron ore was loaded onto a train to New York City. Large quantities of Bessemer ore were shipped to Scranton, Pennsylvania, and used to make steel rails for the Lackawanna Steel Company. From 1887 to 1889, the mine was made into an open pit. At one time, it was the largest open-pit operation in the world. In 1895, there was a major collapse that killed 13 miners. After the collapse it was flooded by a reservoir nearby. It was used by soldiers in World War II to test their diving equipment. A collection of minerals and artifacts from the mine is at the Southeast Museum in Brewster. On November 19, 2017, Robert Thomas, 48, went scuba diving at Tilly Foster Mine. He went down without a "buddy" to a depth of 171 feet, became entangled in wires and cables, and never resurfaced. His body was recovered at about 1:00 p.m. the day after he went missing. He and other divers had an agreement with owners of the property to dive at the mine.