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Tioughnioga River
The Tioughnioga River () is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed August 8, 2011 tributary of the Chenango River in central New York in the United States. It drains a dissected plateau area east of the Finger Lakes at the northernmost edge of the watershed of the Susquehanna River. The name comes from a native word for "forks of the river" or "meeting of waters". The river was also called "Tiohujodha" by the Moravian Indians. At one time it was called the Onondaga, as leading to that town, and Teyoghagoga was another early form. It rises in two branches in upstate New York southeast of the city of Syracuse, with the East Branch sometimes regarded as the main branch. The West Branch, long, issues from Tully Lake, approximately south of Tully on the Onondaga- Cortland county line, and flows south. The Tully Valley is a preglacial valley of a northward flowing river that flowed into the Ontarian River (pr ...
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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 ...
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Tully (town), New York
Tully is a town in Onondaga County, New York, United States. The population of the town was 951 at the 2019 census. The name of the town is derived from the Roman orator Marcus Tullius Cicero. The town is on the county's southern border, south of Syracuse. History Tully was within the former Central New York Military Tract, an area which the federal government reserved to use for granting plots of land as bounty and pay to soldiers and veterans for their service during the American Revolution. The surveyors were responsible for naming the areas. One of the assistant surveyors, being a classical scholar and professor at Kings College (Columbia), assigned names from Roman generals and statesmen, and Greek men of letters. Tully is derived from the middle name of Marcus Tullius Cicero. This area had been occupied for centuries by the Onondaga people, one of the first Five Nations of the Iroquois Confederacy, or ''Haudenosaunee''. As four of the six nations were allied with th ...
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Binghamton, New York
Binghamton () is a city in the U.S. state of New York, and serves as the county seat of Broome County. Surrounded by rolling hills, it lies in the state's Southern Tier region near the Pennsylvania border, in a bowl-shaped valley at the confluence of the Susquehanna and Chenango Rivers. Binghamton is the principal city and cultural center of the Binghamton metropolitan area (also known as Greater Binghamton, or historically the Triple Cities, including Endicott and Johnson City), home to a quarter million people. The city's population, according to the 2020 census, is 47,969. From the days of the railroad, Binghamton was a transportation crossroads and a manufacturing center, and has been known at different times for the production of cigars, shoes, and computers. IBM was founded nearby, and the flight simulator was invented in the city, leading to a notable concentration of electronics- and defense-oriented firms. This sustained economic prosperity earned Binghamton the m ...
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Whitney Point, New York
Whitney Point is a village in Broome County, New York, United States. The population was 964 at the 2010 census. It is part of the Binghamton Metropolitan Statistical Area. The name comes from Thomas and William Whitney, early developers. The village is in the southwestern corner of the town of Triangle and is north of Binghamton. History The village area was first settled around 1791 and began to flourish after the arrival of the Whitney family around 1800. The Village of Whitney Point (originally called "Whitney's Point") was incorporated in 1871. A catastrophic fire almost destroyed the village in 1897. After serious flooding in 1935 and 1936, work began on a dam north of the village on the Otselic River. It was completed in 1942 and — after decisions were later made to impound water on a year-round basis for recreational purposes — formed the Whitney Point Lake (Reservoir). The village has been the site of the Broome County Fair since 1874. The Whitney Automobile was b ...
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Otselic River
The Otselic River (aht-SEEL-ik), formerly known as Otselic Creek, is a tributary of the Tioughnioga River in central New York in the United States. It drains a hilly area, mostly forested and agricultural, east of the Finger Lakes at the northern edge of the Susquehanna River watershed. Originally the Otselic Creek began at Hatch Lake in the Town of Eaton. When Hatch Lake was dammed in the 1830s to supply the Chenango Canal, all the lake water was diverted to the Chenango Valley to the east. The Otselic River now rises in Torpy Pond in southwestern Madison County, northeast of Georgetown, and meanders southwest through rich river bottom farmland. The Otselic Valley runs through Georgetown, Otselic, Pitcher, Cincinnatus, Willet, Lisle, and Whitney Point, where it is impounded to form Whitney Point Reservoir. Below the Whitney Point Dam, the Otselic River joins the Tioughnioga River from the northeast. Formerly, several "mill ditches" diverted the river water to mi ...
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Kettle (landform)
A kettle (also known as a kettle lake, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are fluvi ...
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Interstate 81
Interstate 81 (I-81) is a north–south (physically northeast–southwest) Interstate Highway in the eastern part of the United States. Its southern terminus is at I-40 in Dandridge, Tennessee; its northern terminus is on Wellesley Island, New York at the Canadian border, where the Thousand Islands Bridge connects it to Highway 137 and ultimately to Highway 401, the main Ontario freeway connecting Detroit via Toronto to Montreal. The major metropolitan areas along the route of I-81 include the Tri-Cities of Tennessee; Roanoke in Virginia; Harrisburg and the Wyoming Valley in Pennsylvania; and Syracuse in New York. I-81 largely traces the paths created down the length of the Appalachian Mountains through the Great Appalachian Valley by migrating animals, indigenous peoples, and early settlers. It also follows a major corridor for troop movements during the Civil War. These trails and roadways gradually evolved into US Route 11 (US 11); I-81 para ...
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Sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural class of soil or soil type; i.e., a soil containing more than 85 percent sand-sized particles by mass. The composition of sand varies, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non- tropical coastal settings is silica (silicon dioxide, or SiO2), usually in the form of quartz. Calcium carbonate is the second most common type of sand, for example, aragonite, which has mostly been created, over the past 500million years, by various forms of life, like coral and shellfish. For example, it is the primary form of sand apparent in areas where reefs have dominated the ecosystem for millions of years like the Caribbean. Somewhat more rarely, sand may be composed of ...
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Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ...
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Rock (geology)
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of exis ...
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Lake Ontario
Lake Ontario is one of the five Great Lakes of North America. It is bounded on the north, west, and southwest by the Canadian province of Ontario, and on the south and east by the U.S. state of New York. The Canada–United States border spans the centre of the lake. The Canadian cities of Toronto, Kingston, Mississauga, and Hamilton are located on the lake's northern and western shorelines, while the American city of Rochester is located on the south shore. In the Huron language, the name means "great lake". Its primary inlet is the Niagara River from Lake Erie. The last in the Great Lakes chain, Lake Ontario serves as the outlet to the Atlantic Ocean via the Saint Lawrence River, comprising the eastern end of the Saint Lawrence Seaway. The Moses-Saunders Power Dam regulates the water level of the lake. Geography Lake Ontario is the easternmost of the Great Lakes and the smallest in surface area (7,340 sq mi, 18,960 km2), although it exceeds ...
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Ontarian River
{{Unreferenced, date=December 2009 The Ontarian River is the term used for the pre-glacial river that began the creation of the valley in Silurian age shales and limestones now occupied by Lake Ontario. The valley was greatly deepened by glacial action during the Ice age. The original flow is thought to have been westward beginning from the Laurentian shield in the present area of the St. Lawrence River to eventually join the Mississippi River The Mississippi River is the second-longest river and chief river of the second-largest drainage system in North America, second only to the Hudson Bay drainage system. From its traditional source of Lake Itasca in northern Minnesota, it fl ... drainage system. During continental glaciation, the tremendous weight of the glacier depressed the area of the St. Lawrence so much that a lower point of drainage was established eastward through the present river system. The area is still rebounding, however, and the rise could further rearr ...
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