Stark's Knob
Stark's Knob is a basaltic pillow lava formation near Schuylerville, New York, United States. It formed about 460 to 440 million years ago in relatively shallow sea water. It is often mistakenly referred to as a volcano, probably because early investigators described it as a volcano or volcanic plug.[1]
It was here during the
Geology
Stark's Knob formed in the
History
Revolutionary War
During the
Modern History
In 1916, the property was deeded to the state. This was partly to prevent the mining of the formation for use in road building. After many years of virtual neglect and a number of proposals to sell the property, the state finally decided to take action to prevent the site's further decay as well as curb vandalism and maintain trails.[2][5] In 2005, the site was incorporated into the master plan of Hudson Crossing Park, a bi-county park centered on Champlain Canal Lock 5 Island.[2]
References
- ^ a b "Stark's Knob: Geological Origins". Office of Cultural Education, New York State Education Department. Retrieved 6 November 2010.
- ^ a b c d "Master Plan". Hudson Crossing Park. Retrieved 4 October 2014.
- ^ "Stark's Knob: Historical Background". Office of Cultural Education, New York State Education Department. Retrieved 6 November 2010.
- ^ Parks and Recreation, Village of Schuylerville website, accessed November 6, 2010
- ^ "Stark's Knob: 1914-1999". Office of Cultural Education, New York State Education Department. Retrieved 6 November 2010.
External links
- Stark's Knob Scientific Reservation
- 1949 USGS Map of the Knob and the surrounding area
- Stark's Knob, Cornell University website