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The Catskill Aqueduct has an operational capacity of about 550 million US gallons (2,100,000 m 3) per day north of the Kensico Reservoir in Valhalla, New York. Capacity in the section of the aqueduct south of Kensico Reservoir to the Hillview Reservoir in Yonkers, New York is 880 million US gallons (3,300,000 m 3) per day. [7]
The Devonian Catskill Group or the Catskill Clastic wedge is a unit of mostly terrestrial sedimentary rock found in Pennsylvania and New York. Minor marine layers exist in this thick rock unit (up to 10,000 feet (3,000 m)). It is equivalent to the Hampshire Formation of Maryland, West Virginia, and Virginia.
The Catskill Mountains, also known as the Catskills, are a physiographic province and subrange of the larger Appalachian Mountains, located in southeastern New York.As a cultural and geographic region, the Catskills are generally defined as those areas close to or within the borders of the Catskill Park, a 700,000-acre (2,800 km 2) forest preserve protected from many forms of development under ...
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Fox Creek [1] is a 6.0-mile-long (9.7 km) [2] tributary of Catskill Creek in Albany County, New York. Via Catskill Creek, it is part of the Hudson River watershed. Fox Creek runs from the Rensselaerville State Forest in the town of Rensselaerville to Catskill Creek at Preston Hollow.
Balsam Lake Mountain is one of the Catskill Mountains, located in the Town of Hardenburgh, New York, United States.It is the westernmost of the range's 35 High Peaks.Its exact height has not been determined, but the highest contour line on topographic maps, 3,720 feet (1,130 m), is usually given as its elevation.
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Only part of it is in the state-owned Forest Preserve; the summit and the most common access route are owned by descendants of railroad magnate Jay Gould, a native of the region, who closed the peak to the public indefinitely in January 2021. Prior to then, a successful ascent was required for membership in the Catskill Mountain 3500 Club. [4]