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John Boyd Thacher State Park

Coordinates: 42°39′21″N 74°01′09″W / 42.655833°N 74.019167°W / 42.655833; -74.019167
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John Boyd Thacher State Park
A panorama from the overlook on a mostly sunny summer day
View from the overlook
A map of New York showing the location of John Boyd Thacher State Park
A map of New York showing the location of John Boyd Thacher State Park
TypeState Park
LocationAlbany County, New York, United States
Coordinates42°39′21″N 74°01′09″W / 42.655833°N 74.019167°W / 42.655833; -74.019167
Area2,155 acres (872 ha)
Created1914
Operated byNew York State

John Boyd Thacher State Park is a state park located 15 miles (24 km) southwest of Albany, New York, near Voorheesville, in Albany County on State Route 157. Located mostly atop the Helderberg Escarpment, the park has several hiking trails that offer panoramic views of the Green Mountains in Vermont and the Taconic Mountains of the Hudson Valley.

Description

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Entrance sign
Tory cave sign

The Indian Ladder Trail is open from early summer to mid- November, 8:00 am until sunset, weather permitting. All other trails are open year-round. It is located on the Helderberg Escarpment, one of the best fossil-bearing formations in the US. There are over 12 miles (20 km) of trails in the park[1] including the famous Indian Ladder Trail. Volleyball courts, children’s play areas and numerous cooking/barbecue areas both open and covered.

Nearby at Thompson's Lake, is the Emma Treadwell Thacher Nature Center, which opened in July 2001[2] and has permanent and occasional displays for the public to view. The center also offers educational programs and visitor information.

From the top of the escarpment, which reaches 1300 ft (400 m), there are fine views of the Hudson and Mohawk Valleys as well as spectacular panoramas of the Adirondacks and Green Mountains of Vermont.

History

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The history of the park area dates back around 400 years to a time when the trail now known as the Indian Ladder Trail was used by the Mohawk Iroquois Indians to reach the trading post run by the Dutch.

Tory Cave sign

It was here that in 1777, at a spot known as Tory Cave, Jacob Salsbury found refuge from settlers during the Burgoyne Invasion.

The region is very well drained as all surface water runs into the limestone, making it an infertile area for farming. There are some fertile areas along the streams and Dutch settlers were brought in to the region by Patroons to whom they paid heavy rents until they freed themselves of the burden through the so-called Helderberg War (also called the Anti-Rent War) of 1839.[3]

The park is named after Albany mayor John Boyd Thacher whose widow, Emma Treadwell Thacher, donated the land in 1914.[4] Since its opening the area was designated as a State Park. The park soon became popular with the residents of Upstate New York and many amenities were added. The purchase of 500 acres (2 km2) of land in 2004 [5] with a State grant of $750.00 from the Environmental Protection Fund and a donation of land from the Nature Conservancy of 81 acres (320,000 m2) and the further purchase of 188 acres (0.76 km2) on 3 August 2006 [6] took the total area of the park to 2,155 acres (8.72 km2).

It is most likely that the most prominent feature of the park, the Helderberg Escarpment got its name from the Dutch Helder meaning bright or light and Berg meaning mountain.[3]

Park Faces Closure

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In early 2010 the Governor of New York, David Paterson, announced that due to the state's massive budget deficit certain areas of the budget would have to be trimmed in order for the state to maintain proper functions. In his budget cuts, Paterson listed the Department of Parks and Recreation as one of the areas that would have funding slashed, which meant that certain parks would either be completely shut down or operated at a minimum capacity.[7]

Upon learning Paterson's intentions, the people and local governments of New York began a collaborative effort to advocate for the budget to be amended to keep John Boyd Thacher State Park, as well as many other parks and historical sites open for the enjoyment of the people. They have used Facebook, Twitter, a website and petitions as tools to help them show their discontent and become more organized in their efforts to stop the park's closure.[8]

Pressure from the public and from some members of the State Legislature resulted in a reversal of the closure proposal. State Senate leaders held a press conference on March 24, 2010 at the capitol, where they said $11.5 million would be restored to the budget to keep parks open.[9]

Trails

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There are over 12 miles (20 km) of trails in the park, the most famous trail being the Indian Ladder Trail.

Indian Ladder Trail

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From the Indian Ladder parking lot, the visitor descends 60 ft (18 m) to the base of the escarpment via a metal staircase. From here the trail follows the base of the escarpment passing under the Minelot Falls and by the stream exiting from a small cave in the base of the rocks. This water is actually from Thompson Lake,[3] some two miles (3 km) away, which makes its way through the porous limestone until it exits here. At the end of the trail, a second set of metal staircases take the visitor back to the top of the escarpment. The trail then continues back to the parking lot, offering excellent panoramas.

  • Indian Ladder Trail, view from the path
    Indian Ladder Trail, view from the path
  • Indian Ladder Trail, the path through the wooded area
    Indian Ladder Trail, the path through the wooded area
  • Indian Ladder Trail, base of the cliff
    Indian Ladder Trail, base of the cliff
  • Indian Ladder Trail, Minelot Falls
    Indian Ladder Trail, Minelot Falls
  • Indian Ladder Trail, from above a staircase leading down over brush
    Indian Ladder Trail, from above a staircase leading down over brush
  • One of several underground springs at the park
    One of several underground springs at the park

Paint Mine Trail

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On the opposite side of the road to the Indian Ladder Trail, this trail is available all year except in the spring. Snow conditions may make hiking difficult. The trail is circular, about 6 miles (10 km) long through wooded areas.

The Long Path

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The Long Path proposed by Vincent Schaefer of Schenectady[10] is a long-distance hiking trail begun in the 1960s. The trail runs from the George Washington Bridge in New York City and ends at Thacher Park, a distance of 347.35 miles (559.01 km)

Natural history

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The park is designated as a wildlife preserve. There are strict regulations on the non-removal of fossils, rocks, plants, animals and birds from the park. There are also rules on the use of snowmobiles during winter and damage to the park. Breach of the regulations can lead to prosecution.

Birds

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Turkey vulture soaring above the park
Turkey vulture above the trees at the park

In April 2004,[5] the then New York State Governor George Pataki, announced that 1,800 acres (7.3 km2) of Thacher Park and nearby Thompson Lake were to be turned into a bird conservation area. This conservation area was modelled on the National Audubon Society's Important Bird Areas Program which was signed into law in 1997.[11]

There are some 171 species of bird to be seen in the park, many of which are in the "of concern" status. These include:[12]

Plants

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There is also a prolific variety of flowers, plants and trees within the park.[12] As the park is a preserve, all species are protected within the park boundaries. The area has some 1,400 acres (5.7 km2) of upland forest with mainly northern hardwoods predominating, but there are also

There are several habitat types preserved in the park, including 3,700 m of calcareous cliff, bur black oak swamp, red maple swamp and emergent marsh/scrub swamp.

Among flowers that can be seen are[13]

Ferns and their relations are also found in cool damp areas especially along Indian Ladder Trail.

Geology

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The Helderberg Plateau comprises a series of limestones of early Devonian age and is one of the most fossiliferous regions in the United States. The park is a window in to New York's geological history, as the rocks here take us back in time hundreds of millions of years. In the 1800s, some of the world's most renowned pioneering geologists, such as Charles Lyell and Amos Eaton, visited this location due to its robust fossil assemblage. During this time James Hall, New York's first state paleontologist, frequently visited the Heldeberg Escarpment, making observations and documenting the unique fossil assemblage. In the 1930s, Winifred Goldring, New York's state paleontologist and the first female state paleontologist in the nation, continued the work of pioneering geologists and in 1933 wrote a guide to Thacher State Park that is still in use to this day.

The escarpment features rocks of the Upper Silurian and Upper and Middle Ordovician ages resting below the Devonian rocks.[3] At the base of the escarpment, the Schenectady beds are visible. The Rondout "waterlime" or dolomite overlies the Schenectady beds and is most pronounced below Minelot Falls. The escarpment consists primarily of the Manlius Formation at the base, which is overlain by the Coeymans Formation. The Manlius Formation contains stromatoporoids and abundant desiccation features, notably prism cracks. The Coeymans Formation is a more massive limestone, appears bluish in color, and contains corals and brachiopods, notably gypidula coeymansensis. The gradational contact between the Manlius and Coeymans Formations represents a transgression, or rise in sea level. Overlying the Coeymans Formation, at the top of the escarpment, the Kalkberg Formation contains brachiopods and crinoids and is interpreted as even deeper marine deposits. The New Scotland Formation contains interbedded shale and sandstone; an exposure is found in Minelot Creek, up creek of the Paint Mine parking area. The Becraft Formation overlies the New Scotland Formation and is a coarse-grained limestone with abundant crinoid debris; it is best exposed in the northern section of the park near Carrick Road, where an unconformity separates the Becraft and overlying Oriskany Sandstone. Due to its predominant limestone bedrock, the park features karst topography which includes numerous disappearing streams, caves, sinkholes, and grikes. The park contains about 40 caves. The longest documented cave is Hailes Cave. This cave has 3,700 feet of mapped passages with about 2 miles of potentially unmapped passages. The park also contains glacial features, common to this region, in the form of striated bedrock and glacial erratics.

See also

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References

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  1. ^ Weather.com - NYSPJT
  2. ^ "New York State Parks Education". Archived from the original on September 24, 2006. Retrieved July 31, 2005.
  3. ^ a b c d Goldring, Winifred (1997) [1993]. Guide to the Geology of John Boyd Thacher Park. University of the State of New York. ISBN 1-55557-204-9. OCLC 42393004.
  4. ^ Stuberts Isle Archived 2013-02-03 at archive.today
  5. ^ a b Parsavand, Shirin (April 28, 2004). "1,800-acre (7.3 km2) bird area preserved". The Daily Gazette. Schenectady, N.Y.
  6. ^ State Governors Office press release Archived 2006-12-01 at the Wayback Machine
  7. ^ "New York Budget Proposals Would Close Many State Parks in 2010, End Land Acquisition". New York-New Jersey Trail Conference. February 2010.
  8. ^ "Save Thacher Park - FOX23 News - the 10 O'Clock News". Archived from the original on March 2, 2010. Retrieved February 20, 2010.
  9. ^ Post, Paul (March 25, 2010). "Senate Democrats say New York's state parks will stay open". The Saratogian.
  10. ^ The Long Path Trail Archived 2007-07-10 at the Wayback Machine
  11. ^ Duggan, Erin (April 28, 2004). "Feathered friends can nest easy at parks". Times Union. Albany, N.Y.
  12. ^ a b New York State Department of Environmental Conservation[permanent dead link‍]
  13. ^ House, Dr H. D. (2000). Handout. New York State Museum (Botany Department).
  14. ^ "Purple virgins-bower". Archived from the original on October 23, 2006. Retrieved March 1, 2007.
  15. ^ "Walking fern". Archived from the original on November 12, 2007. Retrieved March 1, 2007.
  16. ^ "Purple stemmed cliff brake". Archived from the original on February 4, 2007. Retrieved March 1, 2007.
  17. ^ "Slender cliff brake". Archived from the original on February 4, 2007. Retrieved March 1, 2007.

General references

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  • Able, K. P. (1996). Birding New York's Hudson-Mohawk Region. Delmar, N.Y.: Hudson-Mohawk Bird Club, Inc.
  • Van Driver, Bradford B. (2003) [1985]. Roadside Geology of New York. Missoula: Mountain Press Publishing Company. pp. 176, 185, 208–209. ISBN 0-87842-180-7.
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