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Lake Wononscopomuc
Lake Wononscopomuc is a lake located in the Lakeville section of Salisbury, Connecticut, United States The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territori .... It has the distinction of being the deepest natural lake in the state. Wononskopumuc is a Mahican name for "rocks at the bend in the lake." Also known as Wononskopomuc Lake or Lakeville Lake, Lake Wononscopomuc is a natural, marl lake that supports a diverse community of aquatic plants. The town beach and a boat launch, known collectively as the Salisbury Town Grove, are on the lake’s north shore. The boathouse and private beach of the Hotchkiss School are on the lake's south shore. Access to the lake is monitored because of fears that the invasive zebra mussel will be introduced on boats or trailers from nearby Twin Lakes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lakeville, Connecticut
Lakeville is a census-designated place (CDP) in Litchfield County, Connecticut, United States, close to Dutchess County, New York. It is within the town of Salisbury, but has its own ZIP Code (06039). As of the 2010 census, the population of Lakeville was 928, out of 3,741 in the entire town of Salisbury. The Hotchkiss School is located in Lakeville, and the Indian Mountain School is nearby. Geography Lakeville is in the southwest part of the town of Salisbury, on U.S. Route 44 southwest of the Salisbury town center. US 44 leads northeast to Canaan village and west to Millerton, New York. According to the U.S. Census Bureau, the Lakeville CDP has a total area of , of which are land and , or 14.8%, are water. Most of the water area is part of Lake Wononscopomuc, the deepest natural lake in the state. History Until 1846, Lakeville was called "Furnace Village", due to the location there of one of the early blast furnaces of the historic Salisbury iron industry (one of whic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salisbury, Connecticut
Salisbury () is a town situated in Litchfield County, Connecticut, United States. The town is the northwesternmost in the state of Connecticut; the Massachusetts-New York-Connecticut tri-state marker is located at the northwest corner of the town. The population was 4,194 at the 2020 census. History Salisbury was established and incorporated in 1741, and contains several historic homes, though some were replaced by larger modern structures in the late 20th century. Salisbury was named for Salisbury, a city in England. Historian Ed Kirby tells that traces of iron were discovered in what was to become Salisbury in 1728, with the discovery of the large deposit at Old Hill (later Ore Hill) in 1731 by John Pell and Ezekiel Ashley. From before the American Revolution, through the Federal Period of the nation, and until around 1920, Salisbury was the seat of an important iron industry. Additional iron mines were opened, mostly in the western end of the town, although historian Dian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States
The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territories, nine Minor Outlying Islands, and 326 Indian reservations. The United States is also in free association with three Pacific Island sovereign states: the Federated States of Micronesia, the Marshall Islands, and the Republic of Palau. It is the world's third-largest country by both land and total area. It shares land borders with Canada to its north and with Mexico to its south and has maritime borders with the Bahamas, Cuba, Russia, and other nations. With a population of over 333 million, it is the most populous country in the Americas and the third most populous in the world. The national capital of the United States is Washington, D.C. and its most populous city and principal financial center is New York City. Paleo-Americ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marl Lake
A marl lake is a type of alkaline lake whose bottom sediments include large deposits of marl, a mixture of clay and carbonate minerals. The term is particularly applied to lakes that have been dredged or mined for marl, often for manufacturing Portland cement. Marl lakes are found around the Great Lakes of North America, in Britain, and in other areas that were once glaciated. They support distinctive ecological communities that are vulnerable to damage from silting, nutrient pollution, drainage, and invasive species. Description Marl lakes typically are found in areas that were recently glaciated, and they often fill kettle depressions left behind by melting glaciers. Their most distinctive characteristic is that they deposit sediments rich in calcium carbonate. More precisely, a marl lake is a lake in which calcium carbonate makes up at least 50% of the dry weight of the inorganic fraction of the surface sediments. In some lakes, the sediments are almost pure calcium carbo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hotchkiss School
The Hotchkiss School is a coeducational preparatory school in Lakeville, Connecticut, United States. Hotchkiss is a member of the Eight Schools Association and Ten Schools Admissions Organization. It is also a former member of the G30 Schools group. History In 1891, Maria Harrison Bissell Hotchkiss, with guidance from Yale President Timothy Dwight V, founded the school to prepare young men for Yale University. In 1892, The Hotchkiss School opened its doors to 50 male boarding students for $600. Hotchkiss's endowment also precipitated scholarship aid to deserving students. In 1974, the school became coeducational. *a "With the guidance of then President of Yale University Timothy Dwight, Maria Hotchkiss established the School in 1891 to prepare young men for Yale...Hotchkiss offers a classical education, finding strength in a traditional approach that has worked well and stood the test of time." — ¶ 2 (Strengthened by Time) *b "The week leading up to and including “Taft ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Twin Lakes (Connecticut)
The Twin Lakes are adjacent Lakes Washining and Washinee, commonly referred to as East Twin Lake and West Twin Lake, in Salisbury amidst Connecticut's Northwest Hills. Geography Lake Washinee is about 1.6 miles (2.6 km) long, and under a quarter mile (0.4 km) wide of except for its squarish roughly 0.5 by 0.6 mile (0.8 by 1.0 km) southernmost section. Its deepest part is around . Lake Washining is much rounder, and roughly 0.9 by 1.3 miles (1.5 by 2 km). It has a maximum depth of . Much of the shore is wetland, but there are some private residences. There is a thermocline that forms around . The Twin Lakes are located in Salisbury, Connecticut, roughly five miles away from both the Massachusetts and New York borders. The two lakes are separated by an isthmus under 300 feet (100 m) wide, and they maintain the same water level. They are located in the Housatonic Valley in northwestern Connecticut. Near the 'Between the Lakes Road' is located a series of lim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lakes Of Connecticut
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
