In today's world, Whaley Lake has become a topic of great relevance and interest to a wide range of people. Whether due to its impact on society, its relevance in history, its importance in the scientific field, or its influence on culture, Whaley Lake has captured the attention of academics, scientists, enthusiasts, and the curious alike. In this article, we will explore different aspects of Whaley Lake, from its origins to its impact today, analyzing its implications and relevance in the current context. In addition, we will examine its relationship with other topics and its evolution over time, with the aim of providing a complete and enriching vision of Whaley Lake.
Whaley Lake | |
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![]() Whaley Lake near NY 292 | |
Location | Dutchess County, New York |
Coordinates | 41°33′30″N 73°39′45″W / 41.55833°N 73.66250°W |
Type | reservoir, natural lake |
Primary outflows | Whaley Lake Stream |
Catchment area | 3.7 square miles (9.6 km2) |
Basin countries | United States |
Surface area | 252 acres (102 ha) |
Surface elevation | 705 feet (215 m) |
Whaley Lake is located in the town of Pawling in southeastern Dutchess County in New York State, United States. It is the largest lake in Dutchess County.
The lake is partially man-made as it is controlled by a dam at its northern end. The lake feeds into the Fishkill Creek which empties into the Hudson River at Beacon, New York.
The lake is accessible via New York State Route 292, which runs along the south and west sides of the lake. The eastern shore of Whaley Lake is bordered by Metro-North Railroad's unused Beacon Line, and the Maybrook Trailway, which is a part of the Empire State Trail.