Watkins Glen State Park is in the village of Watkins Glen, south of Seneca Lake in Schuyler County in

New York New York most commonly refers to: * New York City, the most populous city in the United States, located in the state of New York * New York (state), a state in the northeastern United States New York may also refer to: Film and television * '' ...

Finger Lakes The Finger Lakes are a group of eleven long, narrow, roughly north–south lakes located south of Lake Ontario in an area called the ''Finger Lakes region'' in New York, in the United States. This region straddles the northern and transitional ...

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 The American Scenic and Historic Preservation Society was created in 1895 as New York’s first organized preservation lobby. The Society operated as a national organization to protect the natural scenery and the preservation of historic landmark ...

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 New York State Office of Parks, Recreation and Historic Preservation (NYS OPRHP) is a state agency within the New York State Executive Department Parks, Recreation and Historic Preservation Law § 3.03. "The office of parks, recreation a ...

The centerpiece of the park is a narrow

gorge A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tenden ...

cut through rock by a stream—Glen Creek—that was left

hanging Hanging is the suspension of a person by a noose or ligature around the neck.Oxford English Dictionary, 2nd ed. Hanging as method of execution is unknown, as method of suicide from 1325. The ''Oxford English Dictionary'' states that hanging i ...

when

glacier A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires dis ...

s of the

Ice age An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and gree ...

deepened the Seneca valley, increasing the tributary

stream gradient Stream gradient (or stream slope) is the grade (or slope) of a stream measured by the ratio of drop in elevation per unit horizontal distance, usually expressed as meters per kilometer or feet per mile. Hydrology and geology A high gradient indicat ...

to create

rapids Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Rapids are hydrological features between a ''run'' (a smoothly flowing part of a stream) and a ''cascade''. ...

and

waterfall A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several wa ...

s wherever there were layers of hard rock. The area's rocks are

sedimentary Sedimentary rocks are types of rock (geology), rock that are formed by the accumulation or deposition of mineral or organic matter, organic particles at Earth#Surface, Earth's surface, followed by cementation (geology), cementation. Sedimentati ...

Devonian The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, whe ...

age, part of a

dissected plateau A dissected plateau is a plateau area that has been severely eroded such that the relief is sharp. Such an area may be referred to as mountainous, but dissected plateaus are distinguishable from orogenic mountain belts by the lack of folding, me ...

that was uplifted with little faulting or distortion. They consist mostly of soft

shale Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especial ...

s, with some layers of harder

sandstone Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) ...

and

limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...

. 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 The Finger Lakes Trail consists of a network of trails in New York. The trail system is administered by thFinger Lakes Trail Conference(FLTC), a non-profit 501(c)(3) organization, composed primarily of volunteers. Description The FLT is primaril ...

, an system of trails within New York state."Watkins Glen State Park", visitor's guide, New York State Office of Parks, Recreation, and Historic Preservation, Finger Lakes Region (2012)

Activities and services

The park has comfortable camping sites, as well as picnic tables and pavilions, food, playground, a gift shop, pool, dump stations, showers, recreation programs, tent and trailer sites, fishing, hiking, hunting and cross-country skiing. The entrance fee for a day picnic is $8 per car. The park is open year-round, but not all facilities are available at all times.

Geology

During the

Pleistocene The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fina ...

era, a vast area was covered by ice during the maximum extent of glacial ice in the north polar area. The movement of glaciers from the

Laurentide The Laurentide Ice Sheet was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States, multiple times during the Quaternary glacial epochs, from 2.58 million years a ...

and Wisconsin ice sheets shaped the

region. The lakes originated as a series of northward-flowing streams. Around two million years ago the first of many continental glaciers of the Laurentide Ice Sheet moved southward from the Hudson Bay area, initiating the Pleistocene glaciation. These glaciers widened, deepened and accentuated the existing river valleys. Glacial debris, possibly including terminal moraines, left behind by the receding ice acted as dams, allowing lakes to form. Despite the deep erosion of the valleys, the surrounding uplands show little evidence of glaciation, suggesting that the ice was thin, or at least unable to cause much erosion at these higher altitudes. The deep cutting of the valleys by the ice left some tributaries hanging high above the lakes: both Seneca and Cayuga have tributaries hanging as much as above the valley floors. One such hanging valley, overlooking the south end of the Seneca Lake valley, evolved into the deep gorge of Watkins Glen. The steep drop of Glen Creek into Seneca Valley created a powerful torrent that eroded the underlying rock, cutting further and further back towards the stream's headwaters. This erosion was not a uniform process: the rock here includes

, and

, and these types of rock erode at different rates, leaving behind a staircase of waterfalls, cascades, plunge pools, and potholes. Watkins Glen State Park now encompasses nineteen waterfalls spaced along a trail roughly long."Watkins Glen State Park"
Finger Lakes Tourism Alliance, n.d. Retrieved: February 20, 2014

References

External links

New York State Parks: Watkins Glen State Park
* {{authority control Glens of the United States State parks of New York (state) Campgrounds in New York (state) Parks in Schuyler County, New York

Activities and services

Geology

See also

References

External links