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Montour Falls, New York

Montour Falls, New YorkUse mdy dates from May 2024Villages in New York (state)Villages in Schuyler County, New York
Montour Falls from Mill Street
Montour Falls from Mill Street

Montour Falls is a village located in Schuyler County, New York, United States. The population was 2,714 at the time of the 2020 census. A waterfall at the end of West Main Street gives the village its name. The name "Montour" is derived from Queen Catharine Montour, a prominent Native American woman of Seneca Indian heritage who lived at the village site in the 18th century. The boundaries defining the Village of Montour Falls occur mostly within the Town of Montour, but a small part lies within the Town of Dix. The village is located approximately twenty miles north of Elmira, New York and three miles south of Watkins Glen, New York. The New York State Academy of Fire Science is located in the village.

Excerpt from the Wikipedia article Montour Falls, New York (License: CC BY-SA 3.0, Authors, Images).

Montour Falls, New York
Clinton Street,

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Wikipedia: Montour Falls, New YorkContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 42.349166666667 ° E -76.846388888889 °
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Address

Clinton Street 109
14865
New York, United States
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Montour Falls from Mill Street
Montour Falls from Mill Street
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Nearby Places

Watkins Glen State Park
Watkins Glen State Park

Watkins Glen State Park is in the village of Watkins Glen, south of Seneca Lake in Schuyler County in New York's Finger Lakes region. The park's lower part is near the village, while the upper part is open woodland. It was opened to the public in 1863 and was privately run as a tourist resort until 1906, when it was purchased by New York State. Initially known as Watkins Glen State Reservation, the park was first managed by the American Scenic and Historic Preservation Society before being turned over to full state control in 1911. Since 1924, it has been managed by the Finger Lakes Region of the New York State Office of Parks, Recreation and Historic Preservation. The centerpiece of the 778-acre (3.15 km2) park is a 400-foot-deep (120 m) narrow gorge cut through rock by Glen Creek, a stream that was left hanging when glaciers of the Ice age deepened the Seneca valley, increasing the tributary stream gradient to create rapids and waterfalls wherever there were layers of hard rock. The area's rocks are sedimentary of Devonian age, part of a dissected plateau that was uplifted with little faulting or distortion. They consist mostly of soft shales, with some layers of harder sandstone and limestone. The park features three trails, open from mid-May to early November, by which one can climb or descend the gorge. The Southern Rim and Indian Trails run along the gorge's wooded rim, while the Gorge Trail is closest to the stream and runs over, under and along the park's 19 waterfalls by way of stone bridges and more than 800 stone steps. The trails connect to the Finger Lakes Trail, an 800-mile (1,300 km) system of trails within New York state.