Related Research Articles
The Hudson River is a 315-mile (507 km) river that flows from north to south primarily through eastern New York in the United States. The river originates in the Adirondack Mountains of Upstate New York, flows southward through the Hudson Valley to the Upper New York Bay between New York City and Jersey City. It eventually drains into the Atlantic Ocean at New York Harbor. The river serves as a political boundary between the states of New Jersey and New York at its southern end. Further north, it marks local boundaries between several New York counties. The lower half of the river is a tidal estuary, deeper than the body of water into which it flows, occupying the Hudson Fjord, an inlet which formed during the most recent period of North American glaciation, estimated at 26,000 to 13,300 years ago. Tidal waters influence the Hudson's flow from as far north as the city of Troy.
The Allegheny River is a 325-mile (523 km) long headwater stream of the Ohio River in western Pennsylvania and New York, United States. The Allegheny River runs from its headwaters just below the middle of Pennsylvania's northern border northwesterly into New York then in a zigzag southwesterly across the border and through Western Pennsylvania to join the Monongahela River at the Forks of the Ohio on the "Point" of Point State Park in Downtown Pittsburgh, Pennsylvania. The Allegheny River is, by volume, the main headstream of both the Ohio and Mississippi Rivers. Historically, the Allegheny was considered to be the upper Ohio River by both Native Americans and European settlers.
The Mohawk River is a 149-mile-long (240 km) river in the U.S. state of New York. It is the largest tributary of the Hudson River. The Mohawk flows into the Hudson in Cohoes, New York, a few miles north of the city of Albany. The river is named for the Mohawk Nation of the Iroquois Confederacy. It is a major waterway in north-central New York. The largest tributary, the Schoharie Creek, accounts for over one quarter (26.83%) of the Mohawk River's watershed. Another main tributary is the West Canada Creek which makes up for 16.33% of the Mohawk's watershed.
The Hoosic River, also known as the Hoosac, the Hoosick and the Hoosuck, is a 76.3-mile-long (122.8 km) tributary of the Hudson River in the northeastern United States. The different spellings are the result of varying transliterations of the river's original Algonquian name. It can be translated either as "the beyond place" or as "the stony place".
Brandywine Creek is a tributary of the Christina River in southeastern Pennsylvania and northern Delaware in the United States. The Lower Brandywine is 20.4 miles (32.8 km) long and is a designated Pennsylvania Scenic River with several tributary streams. The East Branch and West Branch of the creek originate within 2 miles (3 km) of each other on the slopes of Welsh Mountain in Honey Brook Township, Pennsylvania, about 20 miles (32 km) northwest of their confluence.
Schoharie Creek in New York, flows north 93 miles (150 km) from the foot of Indian Head Mountain in the Catskills through the Schoharie Valley to the Mohawk River. It is twice impounded north of Prattsville to create New York City's Schoharie Reservoir and the Blenheim-Gilboa Power Project.
Alplaus is a hamlet located in Schenectady County, New York, United States. Its name is derived from the Dutch Aal Plaats, or "Place of the Eels."
A stream is a body of water with surface water flowing within the bed and banks of a channel. The flow of a stream is controlled by three inputs - surface water, subsurface water and groundwater. The surface and subsurface water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls.
The Poesten Kill is a 26.2-mile-long (42.2 km) creek in upstate New York located entirely in Rensselaer County, which flows westerly from its source at Dyken Pond in the town of Berlin to its mouth at the Hudson River in the city of Troy. It has been used historically as a source of water for local inhabitants and farmers and became even more important as a source of water power during the Industrial Revolution, during which many mills and factories sprung up along its banks.
Glacial Lake Albany was a prehistoric North American proglacial lake that formed during the end of the Wisconsinan glaciation. It existed between 15,000 and 12,600 years ago and was created when meltwater from a retreating glacier, along with water from rivers such as the Iromohawk, became ice dammed in the Hudson Valley. Organic materials in Lake Albany deposits have been carbon dated to approximately 11,700 years ago. The lake spanned approximately 160 miles (260 km) from present-day Newburgh to Glens Falls.
Kinderhook Creek is a 49.0-mile-long (78.9 km) tributary to Stockport Creek, an inlet of the Hudson River in the United States. From its source in Hancock, Massachusetts, the creek runs southwest through the Taconic Mountains into Rensselaer County, New York, and then into Columbia County. It flows through the towns of Stephentown, New Lebanon, Nassau, Chatham, Kinderhook and Stuyvesant to its mouth at Stockport Creek in the town of Stockport.
The Verkeerder Kill, sometimes Verkeerderkill and locally shortened to Kaidy Kill is an 8-mile-long (13 km) stream in Ulster County, New York, United States. It rises on the Shawangunk Ridge, in the town of Wawarsing, and flows southwards through the town of Shawangunk, toward the Shawangunk Kill, itself a major tributary of the Wallkill River. Ultimately it is a part of the Hudson River's watershed.
The Canajoharie Creek is a river that flows into the Mohawk River in the Village of Canajoharie in the U.S. State of New York. The name "Canajoharie" is a Mohawk language term meaning "the pot that washes itself", referring to the "Canajoharie Boiling Pot", a 20-foot (6.1 m) wide and 10-foot (3.0 m) deep pothole in the Canajoharie Creek, just south of the village of Canajoharie. Bowmans Creek is one main tributary that enters the creek east of the Hamlet of Sprout Brook. The other main tributary is Brimstone Creek which enters the creek north-northwest of the Village of Ames.
Lisha Kill flows through Lisha Kill, New York before emptying into the Mohawk River in Niskayuna, New York. The stream is also referred to as Lisha's Kill and received its name from a local legend about a Native American woman who is buried along its banks.
Lansing Kill flows into the Mohawk River in Hillside, New York. Pixley Falls is a waterfall located on Lansing Kill by Hurlbutville, New York. Lansing Kill flows through Pixley Falls State Park and it flows parallel to the old Black River Canal for much of its course.
Verf Kill flows into the Mohawk River near Pattersonville, New York.
Mount Moses is a mountain in the Central New York region of New York. It is located west of Riverside and north of Sidney. The Unadilla River converges with the Susquehanna River southwest of Mount Moses. Hutchinson Hill is located north-northeast.
The Saw Kill is a 14.3-mile-long (23.0 km) tributary of the Hudson River, called the Metambesem by the Algonquin people of the area and sometimes called Sawkill Creek today. It rises in the town of Milan and drains a 22-square-mile (57 km2) area of northwestern Dutchess County, New York, that includes most of the town of Red Hook to the west and part of Rhinebeck to Red Hook's south.
References
- ↑ "Alplaus Kill". Geographic Names Information System . United States Geological Survey . Retrieved 2017-10-12.
- ↑ "Alplaus Kill". usgs.gov. usgs. 1972. Retrieved 13 October 2017.
data
- ↑ University of the State of New York Bulletin. University of the State of New York. 1914. p. 56.