Located in the Labrador Hollow Unique Area is the beautiful main 50 foot Tinker Falls with its impressive natural rock amphitheater above a 30 foot rocky cascade. The falls are most spectacular during the spring thaw and after a major rainstorm. 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.
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