Labrador Hollow's topography is responsible for its unique character. The area is located in the middle of a valley running north to south that was dug out by glacial movement that occurred during the Pleistocene Epoch. Massive ice sheets from the last glaciation episode (Wisconsinan glaciation episode) retreated from the area approximately ten thousand years ago. They left behind numerous sedimentary deposits and superficial features, some of which filled with water and are now called the Finger Lakes, while others became known as valleys. The floor of Labrador Hollow's valley is only about one-half mile wide, but its walls rise abruptly for several hundred feet. Today, this unique and attractive area provides diverse ecological, economic, and recreational services for many New York residents and visitors alike. Lone fisherman finds peace, solitude and tranquility while paddling around the pond.

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拍攝者： Mccrainemercantile