query: which states does the connecticut river flow through?

title: Black River (Connecticut River tributary)

text: Black River (Connecticut River tributary) The Black River is a river in the U.S. state of Vermont, and a tributary of the Connecticut River. The watershed, or drainage basin, consists of some in southeastern Vermont, almost all of which lies in Windsor County. The Black River begins in a small body of water called Black Pond, in Plymouth, Vermont. Winding its way toward the town of Ludlow, its narrow flow picks up a variety of small brooks and streams and is cooled by overhanging branches. Passing through Amherst Lake, Echo Lake, Lake Rescue, and Lake Pauline, the Black River picks

title: Connecticut River

text: Connecticut River The Connecticut River is the longest river in the New England region of the United States, flowing roughly southward for through four states. It rises at the U.S. border with Quebec, Canada, and discharges at Long Island Sound. Its watershed encompasses five U.S. states and one Canadian province, via 148 tributaries, 38 of which are major rivers. It produces 70% of Long Island Sound's fresh water, discharging at per second. The Connecticut River Valley is home to some of the northeastern United States' most productive farmland, as well as a metropolitan region of approximately two million people surrounding

title: Connecticut River

text: from south to north by location of mouth: The Connecticut River is a barrier to travel between western and eastern New England. Several major transportation corridors cross the river including Amtrak's Northeast Corridor, Interstate 95 (Connecticut Turnpike), Interstate 90 (Massachusetts Turnpike), Interstate 89, Interstate 93, and Interstate 84. In addition, Interstate 91, whose route largely follows the river north-south, crosses it twice – once in Connecticut and once in Massachusetts. Connecticut River The Connecticut River is the longest river in the New England region of the United States, flowing roughly southward for through four states. It rises at the U.S.

title: Connecticut River

text: of the Western Hemisphere's "40 Last Great Places", while the Ramsar Convention on Wetlands listed its estuary and tidal wetlands complex as one of 1,759 wetlands of international importance. In 1997, the Connecticut River was designated one of only 14 American Heritage Rivers, which recognized its "distinctive natural, economic, agricultural, scenic, historic, cultural and recreational qualities." In May 2012, the Connecticut River was designated America's first National Blueway, in recognition of the restoration and preservation efforts on the river. The Connecticut River's flow is slowed by main stem dams, which create a series of slow-flowing basins from Lake Francis Dam

title: Connecticut River

text: New England, the Connecticut River watershed spans five of the six New England states – New Hampshire, Vermont, Massachusetts, Connecticut, as well as small portions of Maine and the Canadian province of Quebec. The Connecticut River rises from Fourth Connecticut Lake, a small pond that sits south of the Canada–United States border in the town of Pittsburg, New Hampshire, at an elevation of above sea level. It flows through the remaining Connecticut Lakes and Lake Francis for , all within the town of Pittsburg, and then widens as it delineates of the border between New Hampshire and Vermont. The river

title: Mad River (Connecticut)

text: in New England. The fish was illegally introduced to the reservoir in the 1970s and has since become naturalized. Mad River (Connecticut) The Mad River is a river that flows through northern New Haven County, Connecticut in the United States. Rising at the outlet of Cedar Lake just south of Bristol, it courses roughly 11 miles through Wolcott and Waterbury before emptying into the Naugatuck River. Prior to settlement by the Connecticut Colony, the broad region encompassing the Mad River was a hunting ground frequented by native Algonquian people of the Mattabesec and Tunxis tribes. The territory was known to

title: Mad River (Connecticut)

text: Mad River (Connecticut) The Mad River is a river that flows through northern New Haven County, Connecticut in the United States. Rising at the outlet of Cedar Lake just south of Bristol, it courses roughly 11 miles through Wolcott and Waterbury before emptying into the Naugatuck River. Prior to settlement by the Connecticut Colony, the broad region encompassing the Mad River was a hunting ground frequented by native Algonquian people of the Mattabesec and Tunxis tribes. The territory was known to these inhabitants as "Mattatuckoke", believed to translate to "place without trees", and it correlated roughly to what is today

title: Connecticut River

text: in Pittsburg, New Hampshire, to the Holyoke Dam at South Hadley Falls in Massachusetts. Among the most extensively dammed rivers in the United States, the Connecticut may soon flow at a more natural pace, according to scientists at the University of Massachusetts at Amherst, who have devised a computer that – "in an effort to balance human and natural needs" – coordinates the holding and releasing of water between the river's 54 largest dams. The Connecticut River watershed encompasses , connecting 148 tributaries, including 38 major rivers and numerous lakes and ponds. Major tributaries include (from north to south) the

title: Thames River (Connecticut)

text: Thames River (Connecticut) The Thames River () is a short river and tidal estuary in the state of Connecticut. It flows south for through eastern Connecticut from the junction of the Yantic River and Shetucket River at Norwich, Connecticut, to New London and Groton, Connecticut which flank its mouth at Long Island Sound. The Thames River watershed includes a number of smaller basins and the 80-mile-long Quinebaug River, which rises in southern Massachusetts and joins the Shetucket River about four miles northeast of Norwich. The river has provided important harbors since the mid-17th century. It was originally known as the

title: Oxoboxo River, Connecticut

text: Oxoboxo River, Connecticut Oxoboxo River is a census-designated place (CDP) in the town of Montville in New London County, Connecticut, United States. The population was 2,938 at the 2000 census and 3,165 at the 2010 census. The statistical area encompasses the town center of Montville, as well as the adjacent villages of Palmertown and Uncasville. The name of the statistical area is from the river of the same name running through the CDP. The U.S. Postal Service includes the entire area of the CDP in ZIP code 06382, for which the USPS uses "Uncasville" as the place name. The Uncasville

title: Cold River (Connecticut River tributary)

text: Cold River (Connecticut River tributary) The Cold River is a 22.6-mile-long (36.5 km) river located in western New Hampshire in the United States. It is a tributary of the Connecticut River, which flows to Long Island Sound. The Cold River begins at the outlet of Crescent Lake in the northeastern corner of the town of Acworth. The river flows east into the town of Lempster, then turns south and reenters Acworth. When Dodge Brook joins the river, it turns west and makes its way to the Connecticut River, passing the villages of South Acworth, Alstead, and Drewsville. The river reaches

text: the Connecticut just south of the communities of Bellows Falls, Vermont, and North Walpole, New Hampshire. In October 2005, flooding on the Cold River and its tributaries caused severe damage in the towns of Alstead, Acworth, and Walpole. Cold River (Connecticut River tributary) The Cold River is a 22.6-mile-long (36.5 km) river located in western New Hampshire in the United States. It is a tributary of the Connecticut River, which flows to Long Island Sound. The Cold River begins at the outlet of Crescent Lake in the northeastern corner of the town of Acworth. The river flows east into the

title: The Oxbow (Connecticut River)

text: masters rowing clubs in western Massachusetts. The Oxbow (Connecticut River) The Oxbow (also known as the Ox-Bow) is an extension of the Connecticut River, located in Northampton, Massachusetts. It is famous for its appearance in the 1836 painting "The Oxbow" by Thomas Cole. Historically, the Oxbow was connected directly to the Connecticut river as a large U-shaped bend. In 1840, flood waters cut through the narrow section, separating the Oxbow from the main river and the current. In the early 1900s, the Oxbow was used extensively for logging operations, as a holding area for logs sent down river. The northern

title: The Oxbow (Connecticut River)

text: The Oxbow (Connecticut River) The Oxbow (also known as the Ox-Bow) is an extension of the Connecticut River, located in Northampton, Massachusetts. It is famous for its appearance in the 1836 painting "The Oxbow" by Thomas Cole. Historically, the Oxbow was connected directly to the Connecticut river as a large U-shaped bend. In 1840, flood waters cut through the narrow section, separating the Oxbow from the main river and the current. In the early 1900s, the Oxbow was used extensively for logging operations, as a holding area for logs sent down river. The northern end was later cut off to

title: Thames River (Connecticut)

text: the world's first nuclear-powered submarine. Two historic forts overlook the mouth of the river at New London harbor, now Connecticut State Parks: Fort Griswold on the eastern Groton Heights, and Fort Trumbull on the New London side. The Yale-Harvard Boat Race is held annually in New London. New London's Sailfest is an annual event which includes OpSail, a gathering of large sailing vessels, including the U.S. Coast Guard training ship "Eagle". Thames River (Connecticut) The Thames River () is a short river and tidal estuary in the state of Connecticut. It flows south for through eastern Connecticut from the junction

title: Mill River (Connecticut)

text: Mill River (Connecticut) The Mill River is a river in the U.S. state of Connecticut. The river starts in the town of Cheshire, flows through Hamden and New Haven, and discharges into New Haven Harbor on Long Island Sound. The river's length is . The river is dammed in southern Hamden to form Lake Whitney, which is operated as a reservoir by the South Central Connecticut Regional Water Authority. A mill for grinding corn was built on a Quinnipiack ford near East Rock in 1642. By 1780 there were eight mills. In time the river provided power for Eli Whitney's

title: Connecticut River

text: Hartford, the Connecticut River's second largest city and only state capital, is located at the southern end of this region on an ancient floodplain that stretches to Middletown. south of Hartford, at Middletown, the Lower Connecticut River section begins with a narrowing of the river, and then a sharp turn southeast. Throughout southern Connecticut, the Connecticut passes through a thinly populated, hilly, wooded region before again widening and discharging into Long Island Sound between Old Saybrook and Old Lyme. Due to the presence of large, shifting sandbars at its mouth, the Connecticut is the only major river in the Northeastern

title: Deep River, Connecticut

text: Deep River, Connecticut Deep River is a town in Middlesex County, Connecticut, United States. The population was 4,629 at the 2010 census. The town center is also designated by the U.S. Census Bureau as a census-designated place (CDP). Deep River is part of what the locals call the "Tri-town Area" made up of Deep River, Chester, and Essex, Connecticut. Every year on the third Saturday in July, Deep River hosts the Deep River Ancient Muster, the largest one day gathering of fife and drum corps in the world. According to the United States Census Bureau, the town has a total

title: Connecticut River

text: United States without a port at its mouth. The Connecticut River carries a heavy amount of silt, especially during the spring snow melt, from as far north as Quebec. This heavy silt concentration manifests in a large sandbar near the Connecticut's mouth, which has, historically, provided a formidable obstacle to navigation. Due to the difficulty it presents to ships, the Connecticut is one of the few major rivers in the United States without a major city at its mouth. The Connecticut's major cities – Hartford and Springfield – lie upriver, respectively. The Nature Conservancy named the Connecticut River's tidelands one

title: Connecticut River

text: Special Concern in one or more of the states in the watershed. The mouth of the river up to Essex is thought to be one of the busiest stretches of waterway in Connecticut. Some local police departments and the state Environmental Conservation Police patrol the area a few times a week. Some towns keep boats available if needed. In Massachusetts, the most active stretch of the Connecticut River is centered on the Oxbow, north of Springfield in the college town of Northampton. Camping is available along much of the river, for non-motorized boats, via the Connecticut River Paddlers' Trail. The

title: Farmington River

text: its course to form the Barkhamsted Reservoir and Lake McDonough; it does not assume a particularly river-like appearance until it exits Lake McDonough in New Hartford, Connecticut. The East Branch and West Branch join in New Hartford, Connecticut just about one mile south of Lake McDonough. Upper reaches of the river flow mostly southward, but the river turns northward in Farmington, Connecticut and then runs mostly north and east until it flows into the Connecticut River in Windsor, Connecticut. There are several whitewater sections. One of these, the so-called "Upper Farmington" section of the West Branch in New Boston, Massachusetts,

title: Connecticut River

text: Springfield, Massachusetts and Hartford, Connecticut. The word "Connecticut" is a French corruption of the Mohegan word "quinetucket", which means "beside the long, tidal river". The word came into English during the early 1600s to name the river, which was also called simply "The Great River". Prior to Dutch exploration beginning in 1614, numerous indigenous tribes lived throughout the fertile Connecticut River valley. Information concerning how these tribes lived and interacted stems mostly from English accounts written during the 1630s. The Pequots dominated a territory in the southernmost region of the Connecticut River valley, stretching roughly from the river's mouth at

title: Falls River (Connecticut River tributary)

text: Falls River (Connecticut River tributary) The Falls River is a river located in Essex, Connecticut. It begins in the Pond Meadow area of Ivoryton and runs for about through Essex. Its beginnings are visible from Comstock Field at the end of Park Road in Ivoryton. Before that it runs to a small pond behind the L.C. Doane Company near Pond Meadow Road. It runs along the old Sohmer Piano Factory, under Walnut Street, and along Main Street. It continues to run along Main Street, being very visible near the Lutheran Church. It eventually winds its way to the Connecticut River,

title: Deep River, Connecticut

text: include connections to the Old Saybrook Train Station, served by Amtrak and Shoreline East railroads. Deep River, Connecticut Deep River is a town in Middlesex County, Connecticut, United States. The population was 4,629 at the 2010 census. The town center is also designated by the U.S. Census Bureau as a census-designated place (CDP). Deep River is part of what the locals call the "Tri-town Area" made up of Deep River, Chester, and Essex, Connecticut. Every year on the third Saturday in July, Deep River hosts the Deep River Ancient Muster, the largest one day gathering of fife and drum corps

title: Mill River (Connecticut)

text: gun factory, now the Eli Whitney Museum. Mill River passes through Sleeping Giant State Park in northern Hamden and East Rock Park below Lake Whitney in Hamden. These are among the river's reaches that remain undeveloped and are popular spots for fishing and hiking. English Station, an abandoned power plant, lies on Ball Island in the New Haven terminus of the river. Mill River (Connecticut) The Mill River is a river in the U.S. state of Connecticut. The river starts in the town of Cheshire, flows through Hamden and New Haven, and discharges into New Haven Harbor on Long Island

title: Connecticut River Walk Park

text: Connecticut River Walk Park The Connecticut River Walk is partially constructed park and bikeway in Springfield, Massachusetts, United States, along the banks of New England's largest river, the Connecticut River. Currently, Springfield's section of this park is 3.7 miles long, running from Chicopee, Massachusetts to the South End Bridge in Springfield, Massachusetts. Unique features of the trail include its path alongside an active - and soon-to-be the United States' first high-speed - train line, making it a "rail-with-trail," and its passing in very close proximity to the Naismith Memorial Basketball Hall of Fame. The longest river in New England, the

title: Park River (Connecticut)

text: Trout Brook watershed. Sections of Trout Brook are impaired. Piper Brook starts in St. Mary's Cemetery in New Britain, has an 11.5 square mile watershed, and also has impaired sections. Bass Brook is the other brook in the watershed, with a 10.4 square mile watershed, which starts near Farmington Ave. and flows into Piper Brook near CT Rt. 9 in New Britain. Other towns in the South Branch watershed are Newington, Farmington and Wethersfield. Park River (Connecticut) The Park River, sometimes called the Hog River, flows through and under the city of Hartford, Connecticut. Between 1940 and the 1980s, the

title: West River (Connecticut)

text: West River (Connecticut) The West River is a freshwater stream in southern Connecticut. It flows through the towns of Bethany, Woodbridge, and New Haven before discharging into New Haven Harbor. Within the city of New Haven, the river is surrounded by Edgewood Park and the West River Memorial Park along much of its length. While the river's natural channel winds along the western edge of the West River Memorial Park, a very straight channel (a former rowing course) cuts through its middle and terminates at the park's northern edge (Derby Avenue). There is a public canoe launch, maintained by the

title: West River (Connecticut)

text: anecdotal evidence of increased fish passage has been reported. West River (Connecticut) The West River is a freshwater stream in southern Connecticut. It flows through the towns of Bethany, Woodbridge, and New Haven before discharging into New Haven Harbor. Within the city of New Haven, the river is surrounded by Edgewood Park and the West River Memorial Park along much of its length. While the river's natural channel winds along the western edge of the West River Memorial Park, a very straight channel (a former rowing course) cuts through its middle and terminates at the park's northern edge (Derby Avenue).

title: North Branch Sugar River

text: North Branch Sugar River The North Branch of the Sugar River is a river located in western New Hampshire in the United States. It is a tributary of the Sugar River, which flows to the Connecticut River, which flows to Long Island Sound. The North Branch of the Sugar River begins at the confluence of Sawyer Brook and Stocker Brook in the town of Grantham, New Hampshire. The river flows south through the town of Croydon, reaching the Sugar River in the town of Newport. In Croydon, the river's flow is interrupted by Spectacle Pond, a two-lobed lake. New Hampshire

title: Connecticut River Walk Park

text: planned to run for 20 miles, through city-owned floodplain alongside the Connecticut River. Since the 1960s, Springfielders have been cut off from the economic and recreational development opportunities of the Connecticut River by Interstate 91. Connecticut River Walk & Bikeway was conceived to revitalize the Connecticut Riverfront, restoring it as a focus of life in the region. Unfortunately, Interstate 91 and its tangential developments - for example, above-grade parking lots built underneath it; tall, earthen, grassy mounds constructed beside it; and even double-sided, 20-foot limestone walls between the city and the river- pose formidable barriers to pedestrians reaching the Connecticut

title: Park River (Connecticut)

text: Park River (Connecticut) The Park River, sometimes called the Hog River, flows through and under the city of Hartford, Connecticut. Between 1940 and the 1980s, the river was buried by the Army Corps of Engineers to prevent the spring floods regularly caused by increased surface runoff from urban development. Before European settlement, the Suckiaug people (their name derived from the word "sucki-auke", meaning "black earth") lived on the fertile banks of the Connecticut and Park rivers. In 1633, fur traders from the Dutch West India Company set up Fort Goede Hoop at the rivers' confluence. The Dutch referred to today's

title: Connecticut River Museum

text: Connecticut River Museum The Connecticut River Museum is a U.S. educational and cultural institution based at Steamboat Dock in Essex, Connecticut that focuses on the marine environment and maritime heritage of the Connecticut River Valley. The three-story Connecticut River Museum is located in a restored 1878 steamboat warehouse, which is now the only one of its type remaining on the river, and has been listed on the National Register of Historic Places. The museum opened to the public in 1975, with Connecticut Governor Ella Grasso as its first paid member and "ex officio" patron. The core of its collection came

title: Connecticut River

text: town of Pittsburg is occupied by the Connecticut Lakes, which contain lake trout and landlocked salmon. Landlocked salmon make their way into the river during spring spawning runs of bait fish and during their fall spawn. The river has fly-fishing-only regulations on of river. Most of the river from Lake Francis south is open to lure and bait as well. Two tail-water dams provide cold river water for miles downstream, making for bountiful summer fishing on the Connecticut. After the first major dam was built near Turners Falls, Massachusetts, thirteen additional dams have ended the Connecticut River's great anadromous fish

title: Norwich, Connecticut

text: Norwich, Connecticut Norwich, known as 'The Rose of New England', is a city in New London County, Connecticut, United States. The population was 40,493 at the 2010 United States Census. Three rivers, the Yantic, the Shetucket, and the Quinebaug, flow into the city and form its harbor, from which the Thames River flows south to Long Island Sound. Norwichtown was founded in 1659, by settlers from Old Saybrook led by Major John Mason and Reverend James Fitch. They purchased the land "nine miles square" that would become Norwich from the local Native Mohegan Sachem Uncas. In 1668, a wharf was

title: Deerfield River

text: of the river flow and allow selectible trout fishing through the year. Deerfield River Deerfield River is a river that runs for from southern Vermont through northwestern Massachusetts to the Connecticut River. The Deerfield was historically influential in the settlement of western Franklin County, Massachusetts, and its namesake town. The Deerfield River is the Connecticut River's second longest tributary in Massachusetts, shorter than the Metropolitan Springfield's Westfield River. The river's confluence with the Connecticut is in Greenfield, Massachusetts, downstream of Turners Falls. () The Deerfield is one of the most heavily used rivers in the country with, on average, a

title: Connecticut River

text: Connecticut Colony and New Netherland Colony to a point near Greenwich, Connecticut. The treaty allowed the Dutch to maintain their trading post at Foot Huys de Hoop, which they did until the 1664 British takeover of New Netherland. The Connecticut River Valley's central location, fertile soil, and abundant natural resources made it the target of centuries of border disputes, beginning with Springfield's defection from the Connecticut Colony in 1641, which brought the Massachusetts Bay Colony to the river. Conflicting royal treaties of 1764 sparked the river's east-siders to unite with Ethan Allen and the west-siders against New York and the

title: Still River (Housatonic River tributary)

text: Still River (Housatonic River tributary) The Still River is a tributary to the Housatonic River in Western Connecticut. The river headwaters emanate from Farringtons Pond () at the New York border with Danbury, Connecticut. It meanders through Sanfords Pond () and Lake Kenosia () before entering a concrete aqueduct near downtown Danbury. It then turns north and becomes a more conventional river as it cuts through Brookfield and southern New Milford before joining with the Housatonic (). It has a drainage area of 85 square miles, and a mean flow of 377 cubic feet per second. Mercury nitrate was discharged

title: Connecticut River

text: River; however, the region is best known for its numerous college towns, such as Northampton, South Hadley, and Amherst, as well as the river's most populous city, Springfield. The city sits atop bluffs beside the Connecticut's confluence with two major tributaries, the Chicopee River to the east and Westfield River to the west. The Connecticut River is influenced by the tides as far north as Enfield Rapids in Windsor Locks, Connecticut, approximately north of the river's mouth. Two million residents live in the densely populated Hartford-Springfield region, which stretches roughly between the college towns of Amherst, Massachusetts, and Middletown, Connecticut.

title: Connecticut River

text: the 1930s diverted the Swift River, which feeds the Chicopee River, a tributary of the Connecticut. This resulted in an unsuccessful lawsuit by the state of Connecticut against the diversion of its riparian waters. Demand for drinking water in eastern Massachusetts passed the sustainable supply from the existing system in 1969. Diverting water from the Connecticut River was considered several times, but in 1986 the Massachusetts Water Resources Authority instead undertook a campaign of water conservation. Demand was reduced to sustainable levels by 1989, reaching approximately a 25% margin of safety by 2009. By far the largest river ecosystem in

text: near a parcel of conserved land called Osage Trails. Falls River (Connecticut River tributary) The Falls River is a river located in Essex, Connecticut. It begins in the Pond Meadow area of Ivoryton and runs for about through Essex. Its beginnings are visible from Comstock Field at the end of Park Road in Ivoryton. Before that it runs to a small pond behind the L.C. Doane Company near Pond Meadow Road. It runs along the old Sohmer Piano Factory, under Walnut Street, and along Main Street. It continues to run along Main Street, being very visible near the Lutheran Church.

title: Connecticut River

text: of roads isolated the city for a time. When the water receded, it left behind silt-caused mud which in places was thick; the recovery effort in Springfield, at the height of the American Great Depression, took approximately a decade. Overall, the flood caused 171 deaths and US$500 million (US$ with inflation) in damages. Across the northeast, over 430,000 people were made homeless or destitute by flooding that year. The Connecticut River Flood Control Compact between the states of Connecticut, Massachusetts, New Hampshire, and Vermont was established in 1953 to help prevent serious flooding. The creation of the Quabbin Reservoir in

title: Connecticut River Academy

text: much of the negative effects caused by this. Connecticut River Academy The Connecticut River Academy is a magnet high school for grades 9 - 12, located in East Hartford, Hartford County, Connecticut. It is co-located with Goodwin College, a small 4-year college which moved to the site in 2005. Connecticut River Academy opened in 2010 and graduated its first 4-year class in 2014. The school's themes are environmental sciences and manufacturing, and it focuses on preparing kids for college life and adulthood. One such method is the senior capstone project, in which students must shadow a mentor for a minimum

title: Connecticut River Academy

text: Connecticut River Academy The Connecticut River Academy is a magnet high school for grades 9 - 12, located in East Hartford, Hartford County, Connecticut. It is co-located with Goodwin College, a small 4-year college which moved to the site in 2005. Connecticut River Academy opened in 2010 and graduated its first 4-year class in 2014. The school's themes are environmental sciences and manufacturing, and it focuses on preparing kids for college life and adulthood. One such method is the senior capstone project, in which students must shadow a mentor for a minimum of 15 hours, and write a lengthy reflection

title: Connecticut River

text: the Connecticut River until the end of the French and Indian War in 1763. Abenaki Indians resisted British attempts at colonization, but Colonists began settling north of Brattleboro, Vermont following the war. Settlement of the Upper Connecticut River Valley increased quickly, with population assessments of 36,000 by 1790. The area that is now Vermont was claimed by both New Hampshire and New York, and was settled primarily through the issuance of land grants by New Hampshire Governor Benning Wentworth beginning in the 1740s. New York protested these grants, and King George III decided in 1764 that the border between the

title: Connecticut River

text: to move logs through Perry Falls in Pittsburg. Teams of men would wait at Canaan, Vermont, to protect the bridges from log jams. Men guided logs through a drop along the length of Fifteen-Mile Falls (now submerged under Moore and Comerford reservoirs), and through Logan's Rips at Fitzdale, Mulligan's Lower Pitch, and Seven Islands. The White River from Vermont and Ammonoosuc River from New Hampshire brought more logs into the Connecticut. A log boom was built between Wells River, Vermont, and Woodsville, New Hampshire, to hold the logs briefly and release them gradually to avoid jams in the Ox Bow.

title: Connecticut River Line

text: was discontinued in 1987 due to poor track conditions on the line. Service resumed in 1989 after Amtrak seized control of the line in Vermont from the Boston and Maine Railroad, but the train was rerouted over the Central Vermont Railway through Massachusetts and Connecticut to avoid the still-dilapidated Conn River Line, because Guilford Rail System refused to improve poor track conditions. A stop was added at to replace Northampton. The "Montrealer" was replaced by the daytime "Vermonter" in 1995, using the original route through Connecticut but still avoiding the Conn River Line in Massachusetts. Freight service along the Conn

title: Connecticut River Walk Park

text: as of 2011, Interstate 91 remains a physical barrier between Springfield, the Connecticut River, and the Basketball Hall of Fame. It remains to be seen whether Interstate 91 will be re-routed to its originally planned route along West Springfield's Riverdale Road, (the original highway construction for I-91,) freeing up Springfield's most valuable land; or whether officials will demolish large portions of the highway's tangential developments, making it easier to access the riverfront; or whether some compromise will be reached. Connecticut River Walk Park The Connecticut River Walk is partially constructed park and bikeway in Springfield, Massachusetts, United States, along the

title: Oyster River (Connecticut)

text: Oyster River (Connecticut) The Oyster River is a stream located in the state of Connecticut in New Haven County. It flows south through Orange and forms the boundary of West Haven and Orange and further downstream the boundary of West Haven and Milford. It empties into Long Island Sound, just south of Route 162 at Oyster River Point. Swans, box turtles and many other animals call this area home. In colonial times the area was also known as Clarke’s Point. About 1840, Peter Aims purchased the land from the Clark family and the area become Aimes Point. The Aimes’ family

title: The Oxbow (Connecticut River)

text: build Interstate 91, which runs between the Oxbow and the Connecticut River. The Connecticut River is still accessible by a channel made under the Interstate 91 and U.S. Route 5 bridges. The Oxbow captured the imagination and attention of a broad set of artists over time. Thomas Cole described the scene as "well known" in 1836 as he began his large painting of The Oxbow. A depiction of what was called "Hockanum Bend" had appeared in 1826 in "The northern traveller; containing the routes to Niagara, Quebec, and the Springs," by Theodore Dwight. In 1835 an illustration was created by

title: Connecticut River

text: settlement severing ties with the Connecticut Colony. As this controversy was heating up, the Massachusetts Bay Colony saw an opportunity to gain a foothold along the fertile Connecticut River Valley. In 1640, Boston asserted a claim to jurisdiction over lands surrounding the river; however, Springfield remained politically independent until tensions with the Connecticut Colony were exacerbated by a final confrontation later that year. Hartford kept a fort at the mouth of the Connecticut River at Old Saybrook for protection against the Pequots, Wampanoags, Mohegans, and the New Netherland Colony. After Springfield broke ties with the Colony, the remaining Connecticut settlements

title: Connecticut River Museum

text: research library. In December 1995, the museum was given a triangular waterfront property, valued at US$910,000, in the neighboring village of Old Saybrook, Connecticut, by Bill and Victoria Winterer, who were among the museums co-founders. The property is used as a waterfront park managed by the museum. In 2011 the museum caught fire. They had to rebuild part of it. Connecticut River Museum The Connecticut River Museum is a U.S. educational and cultural institution based at Steamboat Dock in Essex, Connecticut that focuses on the marine environment and maritime heritage of the Connecticut River Valley. The three-story Connecticut River Museum

title: Oxoboxo River, Connecticut

text: median income for a family was $51,987. Males had a median income of $37,775 versus $29,028 for females. The per capita income for the CDP was $23,310. About 5.3% of families and 6.4% of the population were below the poverty line, including 10.5% of those under age 18 and 6.6% of those age 65 or over. Oxoboxo River, Connecticut Oxoboxo River is a census-designated place (CDP) in the town of Montville in New London County, Connecticut, United States. The population was 2,938 at the 2000 census and 3,165 at the 2010 census. The statistical area encompasses the town center of

title: Fall River (Connecticut River tributary)

text: Fall River (Connecticut River tributary) The Fall River is a river in southern Vermont and northern Massachusetts, joining the Connecticut River just downstream from Turners Falls, Massachusetts. The river rises on the eastern slopes of East Mountain in Guilford, Vermont, and flows southward into Bernardston, Massachusetts. For nearly its entire length in Bernardston it is followed by U.S. Route 5 and Interstate 91, flowing for most of that distance between the two highways. South of Bernardston the river forms the boundary between the town of Gill and the city of Greenfield. The Fall River enters the Connecticut River directly across

title: Salmon River (Connecticut)

text: Salmon River (Connecticut) The Salmon River is formed at the confluence of the Blackledge and Jeremy rivers about one mile west of North Westchester, Connecticut. It drains 96,000 acres and courses for to Salmon Cove near Moodus where it flows into the Connecticut River. The Salmon River is probably the largest stream and watershed whose sources and mouth are entirely within the limits of Connecticut. There is a popular paddling route along the Salmon River varying in difficulty from quickwater to Class II whitewater. It begins along River Road about 1/10 of a mile south of the river's formation and

title: New Milford, Connecticut

text: River flow through the town. According to the United States Census Bureau, the town has a total area of , making it the largest town in Connecticut. of it is land and of it (3.31%) is water. The CDP corresponding to the town center has a total area of . of it is land and of it (0.88%) is water. New Milford has a humid continental climate, with mild to warm humid summers and cold to very cold winters. The highest recorded temperature was 103 °F (39 °C) in July 1966, while the lowest recorded temperature was -15 °F (-26

title: Connecticut River

text: state line is now inundated by the impoundments of dams built after this time. The Treaty of Paris (1783) that ended the American Revolutionary War created a new international border between New Hampshire and the Province of Canada at "northwesternmost headwaters of the Connecticut". Several streams fit this description, and thus a boundary dispute led to the short-lived Indian Stream Republic, which existed from 1832 to 1835. The broad, fertile Connecticut River Valley attracted agricultural settlers and colonial traders to Hartford, Springfield, and the surrounding region. The high volume and numerous falls of the river led to the rise of

title: Thames River (Connecticut)

text: Pequot River after the Pequot Indians who dominated the area. Other early names for the river have included Frisius, Great, Great River of Pequot, Little Fresh, Mohegan, New London, and Pequod. The town was officially named New London in 1658 and the estuary river was renamed Thames after the River Thames in London, England. The United States Coast Guard Academy, Connecticut College, a U.S. Navy submarine base, and the Electric Boat submarine shipyard are located on the river at New London and Groton. The USS "Nautilus" (SSN-571) was launched into the river on January 21, 1954 from Electric Boat, becoming

title: Connecticut River Railroad

text: Connecticut River Railroad The Connecticut River Railroad was a railroad located along the Connecticut River in western Massachusetts, formed in 1845 from the merger of two unfinished railroads. Its main line from Springfield to East Northfield, Massachusetts, opened in stages between 1845 and 1849. It built several branches and over the years acquired additional lines in Vermont. The railroad was acquired by the Boston and Maine Railroad in 1893. The Connecticut River Railroad (CRRR) was formed in 1845 by the merger of the Northampton and Springfield Railroad (chartered in 1842) with the Greenfield and Northampton Railroad. The CRRR first line

title: Fort River

text: has a wide variety of wildlife due to it being the longest free-flowing tributary (having no dams or other man made changes made to the rivers shape or flow) of the Connecticut River. Because of this there is a lot of wildlife making it one of the 3 most diverse rivers in the state. Mussels, Eastern Pearlfish, Sea Lampreys, and American Eel's. Fort River The Fort River is a river in Western Massachusetts and is a tributary of the Connecticut River and runs through the towns of, Amherst, Massachusetts, and ends in Hadley, Massachusetts. The Fort technically begins as Adams

title: Connecticut River

text: provinces should be the western bank of the Connecticut River. Ethan Allen, the Green Mountain Boys, and other residents of the disputed area resisted attempts by New York to exercise authority over the area, which resulted in the establishment of the independent Vermont Republic in 1777 and its eventual accession to the United States in 1791 as the fourteenth state. Boundary disputes between Vermont and New Hampshire lasted for nearly 150 years and were finally settled in 1933, when the U.S. Supreme Court reaffirmed King George's boundary as the ordinary low-water mark on the Vermont shore. In some places, the

title: Mystic River (Connecticut)

text: according to the Mystic River Historical Society. The Pequot Indians built a village called Siccanemos overlooking the western bank of the Mystic River, but it was destroyed during the Pequot War on May 26, 1637, the day of the Mystic massacre. Mystic River (Connecticut) The Mystic River is a estuary in the southeast corner of the U.S. state of Connecticut. Its main tributary is Whitford Brook. It empties into Fishers Island Sound, dividing the village of Mystic, Connecticut between the towns of Groton and Stonington. Much of the river is tidal. The Mystic River was the location of three large

title: Salmon River (Connecticut)

text: character of the Salmon River watershed. Land trusts hold numerous, smaller nature preserves and conservation easements throughout the Salmon River basin such as Pine Brook Preserve in Haddam, Keech Preserve and Salmon Cove Preserve in East Haddam and the Gateway Property and Palakewitz Easement in Colchester. Salmon River (Connecticut) The Salmon River is formed at the confluence of the Blackledge and Jeremy rivers about one mile west of North Westchester, Connecticut. It drains 96,000 acres and courses for to Salmon Cove near Moodus where it flows into the Connecticut River. The Salmon River is probably the largest stream and watershed

title: Scantic River

text: Scantic River The Scantic River (pronounced SKAN-tik) is a river that flows through the states of Massachusetts and Connecticut and is tributary to the Connecticut River. The Scantic River's tributaries rise in the towns of Hampden, Wilbraham, East Longmeadow and Monson in Massachusetts, and in Stafford and Somers, Connecticut, forming the river in the town of Hampden, Massachusetts southeast of Springfield. The Scantic flows southwest for through the towns and communities of Hampden, Massachusetts; Somers, Somersville, Scitico, Hazardville, Enfield, East Windsor, Broad Brook, Scantic, South Windsor, and East Windsor Hill, Connecticut, until joining the Connecticut River () near the East

title: Bridge Street Bridge (Connecticut River)

text: Bridge Street Bridge (Connecticut River) The Bridge Street Bridge is a crossing for Route 140 over the Connecticut River, connecting the towns of Windsor Locks and East Windsor. The current bridge was completed in 1992. The previous bridge at this location was a 7-span through Pratt truss built in 1921. Before that there was a suspension bridge built in 1886. Originally, there was a ferry secured to a mid-river pier. Starting in 1855, there was a ferry tied to a pier in the river to prevent it from being washed downstream. This was succeeded in 1886 with a suspension bridge

title: Pawcatuck River

text: and Hopkinton and Westerly. It turns briefly northwest and west before resuming a southward course to flow past Potter Hill, Rhode Island and between the towns of Westerly, Rhode Island and the Pawcatuck section of Stonington, Connecticut; its mouth is on Little Narragansett Bay on Long Island Sound (). Below is a list of all crossings over the Pawcatuck River. The list starts at the headwaters and goes downstream. In addition to many unnamed tributaries, the following brooks and rivers feed the Pawcatuck: Pawcatuck River The Pawcatuck River is a river in the US states of Rhode Island and Connecticut

title: Chicopee River

text: comparison, the meandering Connecticut River drops just 50 feet from Chicopee to Old Saybrook, Connecticut, where it empties into the Long Island Sound. For this reason, numerous mills were built along the Chicopee River; today, many of them can be found in various states of repurposing, with a particularly famous mill in Springfield Indian Orchard serving as artists' space. Due in part to its precipitous drop, as of 2011, there are six hydropower dams on the Chicopee River. The average flow of the Chicopee River is 900 cubic feet per second, or about 581,644,800 gallons per day. Historical texts often

title: Connecticut River

text: the site of Hartford, Connecticut called the "Fort Huys de Hoop" ("Fort House of Hope"). Four separate Puritan-led groups also settled the fertile Connecticut River Valley, and they founded the two large cities that continue to dominate the Valley today: Hartford (est. 1635) and Springfield (est. 1636). The first group of pioneers left the Plymouth Colony in 1632 and ultimately founded the village of Matianuck (which became Windsor, Connecticut) several miles north of the Dutch fort. A group left the Massachusetts Bay Colony from Watertown, seeking a site where they could practice their religion more freely. With this in mind,

title: Connecticut River

text: Paddlers' Trail currently includes campsites on over of the river. The Water Quality Act of 1965 had a major impact on controlling water pollution in the Connecticut River and its tributaries. Since then, the river has been restored from Class D to Class B (fishable and swimmable). Many towns along the Lower Connecticut River have enacted a cap on further development along the banks, so that no buildings may be constructed except on existing foundations. Currently, a website provides water quality reports twice a week, indicating whether various portions of the river are safe for swimming, boating and fishing. Listed

title: Connecticut River

text: Connecticut River. From the late 1800s until today, it has functioned largely as a center of wildlife and recreation. Starting about 1865, the river was used for massive logging drives from Third Connecticut Lake to initially water powered sawmills near Enfield Falls. Trees cut adjacent to tributary streams including Perry Stream and Indian Stream in Pittsburg, New Hampshire, Halls Stream on the Quebec–New Hampshire border, Simms Stream, the Mohawk River, and the Nulhegan River basin in Essex County, Vermont, would be flushed into the main river by the release of water impounded behind splash dams. Several log drivers died trying

title: Watching the River Flow

text: composing protest songs. For Shelton, who noted the promotional photo for "Watching the River Flow" depicting Dylan looking through a camera, the track expressed Dylan's wish just to be an observer, and not a political activist. Author Seth Rogovoy similarly interpreted the song as Dylan's desire to ignore politics and avoid getting involved in people's disputes. The line "[This ol' river] keeps on rollin', though/No matter ... which way the wind does blow" has been heard by writers Peter Vernezze and Carl J. Porter as evidence of Dylan's conviction that "the river of time, the flow of facts, in reality

title: Flow-through entity

text: Transactions. According to a report published by Brookings in May 2017, in the early 1980s almost all business income in the United States was generated by C corporations. In terms of Income tax in the United States C corporations are taxed separately from their owners. In December 2004 the "Financial Asset Securitization Investment" (FASIT) which was a flow-through entity formed in the United States, was repealed. FASIT was an investment instrument in "non-mortgage receivable pools such as credit card receivables, automobile loans, construction loans, and finance leases." FASITS in existence on October 24, 2004 were exempted from the repeal. By

title: Watching the River Flow

text: Watching the River Flow "Watching the River Flow" is a blues rock song by American singer Bob Dylan. Produced by Leon Russell, it was written and recorded during a session in March 1971 at Blue Rock Studios in New York City. The collaboration with Russell formed in part through Dylan's desire for a new sound—after a period of immersion in country rock music—and for a change from his previous producer. The song was praised by critics for its energy and distinctive vocals, guitar, and piano. It has been interpreted as Dylan's account of his writer's block in the early 1970s,

title: Flow-through entity

text: Flow-through entity A flow-through entity (FTE) is a legal entity where income "flows through" to investors or owners; that is, the income of the entity is treated as the income of the investors or owners. Flow-through entities are also known as pass-through entities or fiscally-transparent entities. Depending on the local tax regulations, this structure can avoid dividend tax and double taxation because only owners or investors are taxed on the revenue. Technically, for tax purposes, flow-through entities are considered "non-entities" because they are not taxed; rather, taxation "flows-through" to another tax return. Common types of FTEs are general partnerships, limited

title: Flow-through test

text: reagent. If the analyte was present in the original sample, then by the end of this process it should be bound to the membrane, with the signal reagent bound to it, revealing (usually visually) the presence of the analyte on the membrane. Flow-through tests can be performed more quickly than lateral flow tests. They exhibit good sensitivity to antibodies, but their detection of antigens is generally less sensitive than lateral flow tests. Flow-through test Flow-through tests or immunoconcentration assays are a type of diagnostic assay that allows users to test for the presence of a biomarker, usually a specific antibody,

title: Flow-through share

text: this service in Canada including Oberon Capital Corporation which is thought to be the largest provider of this unique structure that promotes mineral exploration in Canada and encourages charitable gifting. Flow-through share A flow-through share (FTS) is a tax-based financing incentive that is available to, among others, the mining sector. A FTS is a type of share issued by a corporation to a taxpayer, pursuant to an agreement with the corporation under which the issuing corporation agrees to incur eligible exploration expenses in an amount up to the consideration paid by the taxpayer for the shares. The corporation “renounces” to

title: Flow-through entity

text: opposed to labor. Approximately the largest 2% of pass-through businesses represent 40% of pass-through income and today are taxed at 39.6%, the top individual rate." Flow-through entity A flow-through entity (FTE) is a legal entity where income "flows through" to investors or owners; that is, the income of the entity is treated as the income of the investors or owners. Flow-through entities are also known as pass-through entities or fiscally-transparent entities. Depending on the local tax regulations, this structure can avoid dividend tax and double taxation because only owners or investors are taxed on the revenue. Technically, for tax purposes,

title: Flow-through entity

text: partnerships and limited liability partnerships. In the United States, additional types of FTE include S corporations, income trusts and limited liability companies. Most countries require an FTE (or its owners) to file an annual return reporting the shares of income allocated to owners, and to provide each owner with a statement of allocated income to enable owners to report their shares of income on their own tax returns. In the United States, the statement of allocated income is known as form K-1 (or Schedule K-1). According to International Bureau of Fiscal Documentation (IBFD) a pass-through entity or flow-through entity (FTE)

title: Flow-through test

text: type of immunostrip to be developed, although lateral flow tests have subsequently become the dominant immunostrip point of care device. The first flow-through test was developed in 1985 to test for the presence of beta-human chorionic gonadotropin in urine. Flow-through assays are by principle binding assays. In practice they are mostly applied to detect the interaction of an antibody, as from a sample of the test subject's blood, with immobilized antigens, resulting in the formation of an antigen-antibody complex. However, other types of capture-assays are technically feasible, including small molecule capture-assays or antigen tests. Flow-through assays for the detection of

title: Flow-through entity

text: on their "pro rata shares of income" based on their shareholdings in the S corporation which is not itself taxed. FTEs included in the 2009 "IBFD International Tax Glossary" included the "Bond and Bond Option Sales Strategy" (BOSS) transaction] referring to an "investment strategy developed in the United States to generate tax losses without a corresponding economic loss. The transaction involves the use of a partnership or other flow-through entity that makes an investment in a foreign corporation that is capitalized for the purpose of carrying out the transaction. Variants of Boss Transactions are referred to as Son of Boss

title: Fluid flow through porous media

text: where formula_27. Fluid flow through porous media In fluid mechanics, fluid flow through porous media is the manner in which fluids behave when flowing through a porous medium, for example sponge or wood, or when filtering water using sand or another porous material. As commonly observed, some fluid flows through the media while some mass of the fluid is stored in the pores present in the media. The basic law governing the flow of fluids through porous media is Darcy's Law, which was formulated by the French civil engineer Henry Darcy in 1856 on the basis of his experiments on

title: Fluid flow through porous media

text: Fluid flow through porous media In fluid mechanics, fluid flow through porous media is the manner in which fluids behave when flowing through a porous medium, for example sponge or wood, or when filtering water using sand or another porous material. As commonly observed, some fluid flows through the media while some mass of the fluid is stored in the pores present in the media. The basic law governing the flow of fluids through porous media is Darcy's Law, which was formulated by the French civil engineer Henry Darcy in 1856 on the basis of his experiments on vertical water

title: Watching the River Flow

text: reviews; Dylan's next album that year, "New Morning", was viewed much more favorably by critics, and Ralph Gleason declared "We've got Dylan back again!" For Heylin, Dylan's assertion in the song that he does not have any particular message to express, is an attempt to subvert critics like Gleason. Heylin wrote that both "Watching the River Flow" and "When I Paint My Masterpiece" discuss Dylan's professed lack of inspiration at the time in an honest and satisfying way. Pointing to the fact that Dylan made no attempt to record either a single or an album in the following year of

title: Flow-through share

text: Flow-through share A flow-through share (FTS) is a tax-based financing incentive that is available to, among others, the mining sector. A FTS is a type of share issued by a corporation to a taxpayer, pursuant to an agreement with the corporation under which the issuing corporation agrees to incur eligible exploration expenses in an amount up to the consideration paid by the taxpayer for the shares. The corporation “renounces” to the taxpayer an amount in respect of the expenditures so that the exploration and development expenses are considered to be the taxpayer’s expenses for tax purposes. As a result of

title: Flow-through share

text: corporation to transfer the resource expenses to the investor. A junior resource corporation, in particular, benefits greatly from FTS financing. “The FTS program provides tax incentives to investors who acquire FTSs by allowing: • deductions for resource expenses renounced by eligible corporations; and • investment tax credits for individuals (excluding trusts) on resource expenses in the mining sector that qualify as flow-through mining expenditures. “The Canada Revenue Agency (CRA) reviews all FTS arrangements. Audits are carried out to monitor the program.” When flow-through shares are donated, a lower after-tax cost of giving is achieved. The flow through donation financing structure

title: Flow-through test

text: Flow-through test Flow-through tests or immunoconcentration assays are a type of diagnostic assay that allows users to test for the presence of a biomarker, usually a specific antibody, in a sample such as blood. They are a type of point of care test, a test designed to be used by a healthcare provider at patient contact. Point of care tests often allow for rapid detection of a specific biomarker without specialized lab equipment and training; this aids in diagnosis and allows therapeutic action to be initiated more quickly. Flow-through tests began development in the early 1980s and were the first

title: Potential flow

text: Potential flow does not include all the characteristics of flows that are encountered in the real world. Potential flow theory cannot be applied for viscous internal flows. Richard Feynman considered potential flow to be so unphysical that the only fluid to obey the assumptions was "dry water" (quoting John von Neumann). Incompressible potential flow also makes a number of invalid predictions, such as d'Alembert's paradox, which states that the drag on any object moving through an infinite fluid otherwise at rest is zero. More precisely, potential flow cannot account for the behaviour of flows that include a boundary layer. Nevertheless,

title: Cedar River Flow

text: a trail from the Northville-Lake Placid Trail on the west shore. No motors are allowed on the Cedar River Flow. Cedar River Flow The Cedar River Flow is a remote 640-acre (2.6 km2) shallow lake, created by the Wakely Dam on the Cedar River, where there are a number of campsites accessible via a gravel road, 14 miles (23 km) from Indian Lake or 23 miles (37 km) from Inlet. More campsites are accessible via canoe, around the Flow. It lies on the border between the Moose River Plains Wild Forest and the West Canada Lake Wilderness Area. Fish species

title: Watching the River Flow

text: two years earlier, Dylan claimed he was content to watch while "The river flows, flows to the sea/Wherever it flows, that's where I want to be"; by contrast, in "Watching the River Flow", Dylan writes that he wants to be moving, wishing he was "back in the city/Instead of this old bank of sand". Ricks found Dylan's unsettledness at odds with the implied bucolic notion of watching the river flow. For Ricks, the vocal phrasing and the musical arrangements clash with the lyrics; the "choppy" rhythms and "stroppy stomping" of the backing track, disrupt the theme of contentedly watching the

title: Watching the River Flow

text: to the late Rolling Stones pianist Ian Stewart, including a version of "Watching the River Flow" featuring the Rolling Stones' Mick Jagger, Keith Richards, Charlie Watts, and Ronnie Wood, as well as former member Bill Wyman. The five Rolling Stones recorded their contributions separately, in different studios at different times, but the track constituted the first time since 1992 that Wyman had recorded on the same song as his former bandmates. The choice of the song was based on Ian Stewart's judgment that "Watching the River Flow" was "the only decent thing Bob Dylan ever did". The song has been

title: Watching the River Flow

text: Davis on guitar, and Jim Keltner on drums. Dylan recorded several covers, among them "That Lucky Old Sun" and "Spanish Harlem", as well as two originals: "When I Paint My Masterpiece" and "Watching the River Flow"—the final song recorded at the session. "Watching the River Flow" was based on studio jams done at Blue Rock, and uses a chord progression in the key of F major. Russell recalled that when developing the song, the basic track was formed, and that Dylan then wrote the lyrics in several minutes. Jim Keltner has also reported that Dylan wrote the songs at the

title: Watching the River Flow

text: his fans. Marcus argued that the reason the single was not a hit in the US was because "the time has passed when people are interested in hearing Bob Dylan say he'll just sit there and watch the river flow ... even though that's not quite what he's saying". For Marcus, "Watching the River Flow" is a compelling work, but the subtlety of the song may have prevented it from reaching a wide audience. Clinton Heylin and writer Christopher Ricks discussed Dylan's restlessness in the song. Heylin said that in "Ballad of Easy Rider", co-written by Dylan and Roger McGuinn

title: New River (Mexico–United States)

text: New River (Mexico–United States) The New River () flows north from near Cerro Prieto, through the city of Mexicali, Baja California, Mexico, into the United States through the city of Calexico, California, towards the Salton Sea. The river channel has existed since pre-historic times; however, the river as known today was formed from a levee failure that resulted in massive flooding that re-created the Salton Sea. Today, the river flow is not natural, mostly consisting of agricultural runoff, municipal discharge and industrial dumping. The river has been referred to as the most severely polluted river of its size within the

title: Watching the River Flow

text: covered by numerous artists, including Seatrain (1973), the Earl Scruggs Revue (1976), Steve Gibbons (1977), Joe Cocker (1978), Steve Forbert in the I-10 Chronicles (2001), Ken Saydak (2001), Colin James (2005), Asylum Street Spankers (2006), and Steve Gadd (2010). Leon Russell released his own version in 1999 on the compilation "Tangled Up in Blues". Watching the River Flow "Watching the River Flow" is a blues rock song by American singer Bob Dylan. Produced by Leon Russell, it was written and recorded during a session in March 1971 at Blue Rock Studios in New York City. The collaboration with Russell formed

title: Watching the River Flow

text: 1972, he commented that "Dylan had now concluded that he must simply sit by that bank of sand and await [his muse's] return." Ian Bell, in his critical biography of Dylan, wrote that it was "no accident" that both "Watching The River Flow" and "When I Paint My Masterpiece" made much the same statement. Bell argued that "When I Paint My Masterpiece" is the better song as it is the funnier of the two. Bell heard Dylan mocking both his admirers and his own reputation in this composition, while he detected in "Watching The River Flow" an admission that "If

title: Eel River (California)

text: discharge of any California river in recorded history, and one of the largest peaks recorded in the world relative to the size of its drainage basin. In contrast, during the dry months of July through September, the river achieves nearly zero flow. The lowermost United States Geological Survey (USGS) streamgage on the Eel where flow volume is measured is at Scotia, where an annual mean of , or per year, was recorded between 1910 and 2012. This station measures runoff from an area of , or 85 percent of the basin; however it does not include the flow of the

title: River Calder, West Yorkshire

text: River Calder, West Yorkshire The River Calder is in West Yorkshire, in Northern England. The Calder rises on the eastern slopes of the Pennines and flows through green countryside, former woollen-mill villages, and large and small towns before joining the River Aire near Castleford. The river's valley is generally known as the Calder Valley. The name Calderdale usually refers to the large urban and rural borough (centred on Halifax) through which the upper river flows. The lower reaches flow through the boroughs of Kirklees (based on Huddersfield) and Wakefield. However, the river does not flow through the centres of Halifax

title: Cedar River Flow

text: Cedar River Flow The Cedar River Flow is a remote 640-acre (2.6 km2) shallow lake, created by the Wakely Dam on the Cedar River, where there are a number of campsites accessible via a gravel road, 14 miles (23 km) from Indian Lake or 23 miles (37 km) from Inlet. More campsites are accessible via canoe, around the Flow. It lies on the border between the Moose River Plains Wild Forest and the West Canada Lake Wilderness Area. Fish species present in the lake include brook trout, brown trout, and white sucker. There is a carry down boat access via

title: River Idle

text: pass through urban areas, and there are significant discharges to the rivers from sewage treatment works. The average flow in the River Maun is around 13 Mld (megalitres per day) in dry weather, which is supplemented by Mansfield sewage treatment works, which discharges nearly 23 Mld. Water quality does not improve in the Idle, and remains at 'C' on the GQA scale all the way to the Trent. The Environment Agency maintain gauging stations to measure the flow in the river near the junction with the River Poulter, and to the east of Mattersey. Until the 17th century, the river

title: Flow-through entity

text: is a "non-taxable entity, such as a partnership, under which the income or expense is generally regarded as income or expense of the participants under the transparency principle." FTEs are based on conduit theory or pipeline theory which is defined as a "method of integrating the taxation at the entity and participator level under which income or deductions flow through from the entity to its participators. The entity is in effect regarded as an extension of the participators. A partnership is generally taxed according to the conduit system. The conduit system may be contrasted with the classical system." In the