Watkins Glen State Park
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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 park is a narrow gorge cut through rock by a stream—Glen Creek—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 ...
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List Of New York State Parks
This is a list of state parks in the U.S. state of New York (state), New York. Also listed are state golf courses, seasonal hunting areas, and ''former'' state parks. In New York, state parks are managed by the New York State Office of Parks, Recreation and Historic Preservation, Office of Parks, Recreation and Historic Preservation (OPRHP), with the exception of the Adirondack Park, Adirondack and Catskill Parks which are managed by the New York State Department of Environmental Conservation, Department of Environmental Conservation (DEC). Outside of the Adirondacks and the Catskills, the state parks department is organized into eleven regions: *Niagara *Allegany *Genesee *Finger Lakes *Central *Taconic *Palisades *Long Island *Thousand Islands *Saratoga/Capital District *New York City Forest preserve The largest parks in New York are the Adirondack Park, at ; and the Catskill Park, at . Together they comprise the New York Forest Preserve, properties that must be kept "Forever ...
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Watkins Glen, New York
Watkins Glen is a village and census-designated place in and the county seat of Schuyler County, New York, United States. As of the 2020 census, the population was 1,829. Watkins Glen lies within the towns of Dix and Reading. To the southwest of the village is the Watkins Glen International race track, which hosts annual NASCAR Cup Series and WeatherTech SportsCar Championship races, and formerly hosted the Formula One United States Grand Prix and various IndyCar races. History The settlement of the village began in 1791. First named "Jefferson" in 1842, the village was later renamed in 1852 to honor Dr. Samuel Watkins. Watkins' older brother John purchased property around the gorge in 1794 and constructed mills. After his brother's death, Samuel Watkins inherited the property and spent four decades building up the area with roads, shops and a hotel. Geography Watkins Glen is located at (42.380984, -76.871079). According to the United States Census Bureau, the village h ...
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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, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ...
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State Parks Of New York (state)
State may refer to: Arts, entertainment, and media Literature * ''State Magazine'', a monthly magazine published by the U.S. Department of State * ''The State'' (newspaper), a daily newspaper in Columbia, South Carolina, United States * ''Our State'', a monthly magazine published in North Carolina and formerly called ''The State'' * The State (Larry Niven), a fictional future government in three novels by Larry Niven Music Groups and labels * States Records, an American record label * The State (band), Australian band previously known as the Cutters Albums * ''State'' (album), a 2013 album by Todd Rundgren * ''States'' (album), a 2013 album by the Paper Kites * ''States'', a 1991 album by Klinik * ''The State'' (album), a 1999 album by Nickelback Television * ''The State'' (American TV series), 1993 * ''The State'' (British TV series), 2017 Other * The State (comedy troupe), an American comedy troupe Law and politics * State (polity), a centralized political organizatio ...
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Glens Of The United States
A glen is a valley, typically one that is long and bounded by gently sloped concave sides, unlike a ravine, which is deep and bounded by steep slopes. Whittow defines it as a "Scottish term for a deep valley in the Highlands" that is "narrower than a strath".. The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. The designation "glen" also occurs often in place names. Etymology The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. In Manx, ''glan'' is also to be found meaning glen. It is cognate with Welsh ''glyn''. Examples in Northern England, such as Glenridding, Westmorland, or Glendue, near Haltwhistle, Northumberland, are thought to derive from the aforementioned Cumbric cognate, or another Brythonic equivalent. This likely underlies some examples in Southern Scotland. As the name of a river, it is thought to derive from the Irish word ''glan'' meaning clean, or the Welsh word ''gleindid'' ...
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Watkins Glen International
Watkins Glen International, nicknamed "The Glen", is an automobile race track located in the town of Dix just southwest of the village of Watkins Glen, New York, at the southern tip of Seneca Lake. It was long known around the world as the home of the Formula One United States Grand Prix, which it hosted for twenty consecutive years (1961–1980). In addition, the site has also been home to road racing of nearly every class, including the World Sportscar Championship, Trans-Am, Can-Am, NASCAR Cup Series, the International Motor Sports Association and the IndyCar Series. The facility is currently owned by NASCAR. The course was opened in 1956 to host auto races previously held on public roads in and around the village. The circuit's current layout has more or less been the same since 1971, with minor modifications after the fatal crashes of François Cevert in 1973 and J.D. McDuffie in 1991. The circuit is a Mecca of North American road racing and is a popular venue among fa ...
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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 ago to the present. The last advance covered most of northern North America between c. 95,000 and c. 20,000 years before the present day and, among other geomorphological effects, gouged out the five Great Lakes and the hosts of smaller lakes of the Canadian Shield. These lakes extend from the eastern Northwest Territories, through most of northern Canada, and the upper Midwestern United States (Minnesota, Wisconsin, and Michigan) to the Finger Lakes, through Lake Champlain and Lake George areas of New York, across the northern Appalachians into and through all of New England and Nova Scotia. At times, the ice sheet's southern margin included the present-day sites of coastal towns of the Northeastern United States, and cities such as Bost ...
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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 finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ...
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Watkins Glen Spiral Gorge
Watkins may refer to: Boats * Watkins Yachts, an American sailboat builder, in business from 1973-1989 ** Watkins 32, an American sailboat design ** Watkins 33, an American sailboat design Places In the United States: * Watkins, Colorado * Watkins, Iowa * Watkins, Minnesota * Watkins, Missouri * Watkins, Ohio * Watkins, West Virginia * Watkins Glen, New York Organisations * Watkins Incorporated, a manufacturer of cosmetics, health remedies and baking products * Watkins Electric Music, a manufacturer of musical instruments * Watkins Books, a mind-body-spirit bookshop People * Watkins (surname) Watkins is an English and Welsh surname derived as a patronymic from Watkin, in turn a diminutive of the name Watt (also Wat), a popular Middle English given name itself derived as a pet form of the name Walter. Notable people with the surname ... Other * '' Watkins v. United States'' (1975), a U.S. Supreme Court decision * '' Watkins Biographical Dictionary'', a biographi ...
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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 primarily designated as a footpath only trail. The main trail (FLT) is 584 miles (939.9 km) long and extends from the New York-Pennsylvania border from Allegany State Park in southwestern New York to the Catskill Forest Preserve in eastern New York. There is an additional 400+ miles (643+ km) of branch and loop segments that branch off the main FLT—six branch trails and several loop and side trails. The FLT is part of the 4,600 mile North Country National Scenic Trail (NCNST) and affiliates with the North Country Trail Association as a partner organization. The NCNST uses approximately 424 miles of the FLT as it crosses New York from Allegany State Park and into Madison County. The Trail System passes over a mixture of public and private ...
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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 when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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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) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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