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70-1040: It drains a rural area of the northern Green Mountains along the Canada–US border northeast of Lake Champlain, and an area of Quebec's Eastern Townships . The South Branch rises in Vermont and runs generally from southeast to northwest; the North Branch rises in Lake d'Argent in Eastman, Quebec , and runs from north to south. The North Branch and the South Branch join at Highwater, Quebec , just downriver from North Troy, Vermont . The river then runs in Quebec for approximately 15 miles (24 km), re-entering Vermont at Richford and thence to Lake Champlain's Missisquoi Bay . According to US Natural Resources Conservation Service, Missisquoi Soil – Missisquoi

140-499: A physiographic section of the larger New England province , which in turn is part of the larger Appalachian physiographic division. [REDACTED] Green Mountains travel guide from Wikivoyage 44°47′30″N 72°34′58″W  /  44.79167°N 72.58278°W  / 44.79167; -72.58278 Lake Champlain Lake Champlain ( / ʃ æ m ˈ p l eɪ n / sham- PLAYN ; French : Lac Champlain )

210-693: A direct invasion route to British Canada. However, had the British controlled the lake, they could have divided the colonies of New England and further depleted the Continental Army . The Continental Army's first offensive action took place in May 1775, three weeks after the Battles of Lexington and Concord . Ethan Allen , accompanied by 200 Green Mountain Boys , was ordered to capture Fort Ticonderoga and retrieve supplies for

280-475: A discharge of pollution into Lake Champlain. Agricultural and urban runoff from the watershed or drainage basin is the primary source of excess phosphorus, which exacerbates algae blooms in Lake Champlain. The most problematic blooms have been cyanobacteria , commonly called blue-green algae, in the northeastern part of the lake: primarily Missisquoi Bay . To reduce phosphorus runoff to this part of

350-575: A dooryard garden, typical of mid-19th century New England village homes, and his experience settling in the Champlain Valley depicts the industries and lifestyles surrounding Lake Champlain following the Revolutionary War. Similar to the experience of Salmon Dutton, former colonial militia Major General Hezekiah Barnes settled in Charlotte, Vermont , in 1787. Following the war, Barnes worked as

420-919: A large area of marsh located on a peninsula (stretching over 4.2 kilometres (2.6 mi)) westwards and having a width of 7.2 kilometres (4.5 mi)). Named tributaries in Vermont are: Taft Brook in Westfield , Beetle Brook in Troy , Jay Brook in Jay , Stanhope Brook in Richford , the Trout River in Montgomery , Tyler Branch in Enosburg , Black Creek in Sheldon and Fairfield , and Hungerford Brook in Swanton and Highgate . The Abenaki people used

490-451: A natural defensive position. The British and American vessels engaged in combat for much of the day, only stopping due to impending nightfall. After a long day of combat, the American fleet was in worse shape than the experienced British Navy. Upon ceasefire, Arnold called a council of war with his fellow officers, proposing to escape the British fleet via rowboats under the cover of night. As

560-639: A road surveyor; he also established an inn and trading post in Charlotte, along the main trade route from Montreal down Lake Champlain. Barnes' stagecoach inn was built in traditional Georgian style, with 10 fireplaces, a ballroom on the interior and a wraparound porch on the outside. In 1800, Continental Army Captain Benjamin Harrington established a distillery business in Shelburne, Vermont , which supplied his nearby inn. These individual accounts shed light on

630-521: A row, or flocks of blackbirds flying close to the water". In 2022, it was reported that a feature dramatic film, Lucy and the Lake Monster , was in the works about a young orphan girl and her grandfather looking for Champ. A pollution prevention, control and restoration plan for Lake Champlain was first endorsed in October 1996 by the governors of New York and Vermont and the regional administrators of

700-606: A small uproar, the Great Lake status was rescinded on March 24 (although New York and Vermont universities continue to receive funds to monitor and study the lake). In 1609, Samuel de Champlain wrote that he saw a lake monster 5 ft (1.5 m) long, as thick as a man's thigh, with silver-gray scales a dagger could not penetrate. The alleged monster had 2.5 ft (0.76 m) jaws with sharp and dangerous teeth. Native Americans claimed to have seen similar monsters 8 to 10 ft (2.4 to 3.0 m) long. This mysterious creature

770-606: A souvenir plaque affixed at each end of the bridge, the manufacturer of the metal superstructure of the Vallée bridge is the American company Pittsburg Des Moines Steel Co. The substructure was built by Cenedella & Compagny, from Milford to Massachusetts. Construction contracts had been awarded in 1929. This bridge has been listed since 1990 in the National Register of Historic Places in the United States. This metal bridge replaces

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840-455: A successful siege of Quebec. In May 1776, with the arrival of a British convoy carrying 10,000 British and Hessian troops to Canada, the Continental forces retreated back down the Champlain Valley to reevaluate their strategy. "I know of no better method than to secure the important posts of Ticonderoga and Crown Point, and by building a number of armed vessels to command the lakes, otherwise

910-523: Is Kaniatarakwà:ronte , meaning "a bulged lake" or "lake with a bulge in it". An alternate name is Kaniá:tare tsi kahnhokà:ronte (phonetic English spelling Caniaderi Guarunte ), meaning "door of the country" or "lake to the country". The lake is an important eastern gateway to Iroquois Confederacy lands. The lake was named after the French explorer Samuel de Champlain , who encountered it in July 1609. While

980-475: Is "Wazowategok", meaning "to the river that turns around". The toponym "Rivière Missisquoi" was formalized on December 5, 1968, at the Commission de toponymie du Québec . The Missisquoi River rises in western Orleans County, Vermont , northwest of Lowell , Vermont, at an altitude of 247 metres (810 ft). This source is located next to Route 58 and adjacent to Belvidere Mountain . This source proves to be

1050-470: Is 23 miles (37 km) north of Glens Falls on the Hudson River and 70 miles (110 km) north of Albany, New York . Forts were built at Ticonderoga and Crown Point ( Fort St. Frederic ) to control passage on the lake in colonial times. Important battles were fought at Ticonderoga in 1758 and 1775. During the Revolutionary War, the British and Americans conducted a frenetic shipbuilding race through

1120-614: Is a natural freshwater lake in North America . It mostly lies between the US states of New York and Vermont , but also extends north into the Canadian province of Quebec . The New York portion of the Champlain Valley includes the eastern parts of Clinton County and Essex County . Most of this area is part of the Adirondack Park . There are recreational facilities in the park and along

1190-465: Is an extensive Ordovician carbonate rock formation that extends from Tennessee to Quebec and Newfoundland . The oldest reefs are around "The Head" of the south end of Isle La Motte ; slightly younger reefs are found at the Fisk Quarry, and the youngest (the famous coral reefs) are in fields to the north. The lake has long acted as a border between indigenous nations, much as it is today between

1260-612: Is derived from the Abenaki word masipskoik, which means "where there is flint" or "where flint is". The name originates from an Abenaki chert quarry located near Missisquoi Bay on Lake Champlain. However, according to the Commission de toponymie du Québec (Quebec board of place names), the term missisquoi in Abenaki means "multitudes of water birds", which takes on this river all its meaning. The traditional indigenous variant of this toponym

1330-695: Is fed by the Ausable , Boquet , Great Chazy , La Chute , Little Ausable, Little Chazy , Salmon and Saranac rivers, along with Putnam Creek. In Quebec, it is fed by the Pike River . It is connected to the Hudson River by the Champlain Canal . Parts of the lake freeze each winter, and in some winters the entire lake surface freezes, referred to as "closing". In July and August, the lake temperature reaches an average of 70 °F (21 °C). The Chazy Reef

1400-691: Is in the Lake Champlain Valley between the Green Mountains of Vermont and the Adirondack Mountains of New York , drained northward by the 106 mi-long (171 km) Richelieu River into the St. Lawrence River at Sorel-Tracy, Quebec , northeast and downstream of Montreal . The Champlain basin collects waters from the northwestern slopes of the Green Mountains and the eastern portion of

1470-467: Is likely the original Lake Champlain monster. The monster has been memorialized in sports teams' names and mascots, e.g., the Vermont Lake Monsters and Champ, the mascot of the state's minor league baseball team. A Vermont Historical Society publication recounts the story and offers possible explanations for accounts of the so-called monster: "floating logs, schools of large sturgeon diving in

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1540-435: Is located in the town of Sutton, near the hamlet of Glen Sutton, in Quebec. The other end of the bridge is located in the municipality of Richford, in the state of Vermont in the United States, near the hamlet of East Richford. This bridge serves sector residents and vacationers transiting between Canada and the United States. This triangular metal beam bridge has two spans: one of 16 m and the other of 46.5 meters. According to

1610-621: The Appalachian Mountains , a range that stretches from Quebec in the north to Alabama in the south. The Green Mountains are part of the New England/Acadian forests ecoregion . Three peaks—Mount Mansfield, Camel's Hump, and Mount Abraham—support alpine vegetation . Some of the mountains are developed for skiing and other snow-related activities. Others have hiking trails for use in summer. Mansfield, Killington, Pico, and Ellen have downhill ski resorts on their slopes. All of

1680-658: The Champlain Canal connected Lake Champlain to the Hudson River system, allowing north–south commerce by water from New York City to Montreal and Atlantic Canada . In 1909, 65,000 people celebrated the 300th anniversary of the French discovery of the lake. Attending dignitaries included President William Howard Taft , along with representatives from France, Canada and the United Kingdom. In 1929, then-New York Governor Franklin Roosevelt and Vermont Governor John Weeks dedicated

1750-579: The Great Appalachian Valley , which stretches between Quebec , Canada, to the north, and Alabama , US, to the south. The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley , which in turn is part of the larger Appalachian physiographic division. Lake Champlain is one of numerous large lakes scattered in an arc through Labrador , in Canada, the northern United States, and

1820-501: The National Wild and Scenic Rivers System . River sections being considered for Wild and Scenic designation are as follows: A Study Committee composed of local appointees and partner organizations has been evaluating the Wild and Scenic Designation of the upper Missisquoi and Trout rivers. The group's mission is to facilitate the transfer of information among the ten communities through which

1890-546: The Northwest Territories of Canada. It is the thirteenth-largest lake by area in the US. Approximately 490 sq mi (1,269 km ) in area, the lake is 107 mi (172 km) long and 14 mi (23 km) across at its widest point, and has a maximum depth of approximately 400 ft (120 m). The lake varies seasonally from about 95 to 100 ft (29 to 30 m) above mean sea level . Lake Champlain

1960-591: The United States Environmental Protection Agency (EPA). In April 2003, the plan was updated, and Quebec signed on to it. The plan is being implemented by the Lake Champlain Basin Program and its partners at the state, provincial, federal and local levels. Renowned as a model for interstate and international cooperation, its primary goals are to reduce phosphorus inputs to Lake Champlain, reduce toxic contamination, minimize

2030-525: The Webster–Ashburton Treaty of 1842, the Canada–U.S. border was adjusted northward to include the strategically important site of "Fort Blunder" on the US side. In 1844, work was begun to replace the remains of the 1812-era fort with a massive new Third System masonry fortification, known as Fort Montgomery . Portions of this fort are still standing. In the early 19th century, the construction of

2100-627: The "Green Mountains". However, other ranges within Vermont, including the Taconic Mountains in southwestern Vermont and the Northeastern Highlands , are not geologically part of the Green Mountains. The best-known mountains—for reasons such as high elevation, ease of public access by road or trail (especially the Long Trail and Appalachian Trail ), or with ski resorts or towns nearby—in the range include: The Green Mountains are part of

2170-467: The 1796 Jay Treaty . Eager to take back control of Lake Champlain following the end of the Revolutionary War, Americans flocked to settle the Champlain Valley . Many individuals emigrated from Massachusetts and other New England colonies, such as Salmon Dutton , a settler of Cavendish, Vermont . Dutton emigrated in 1782 and worked as a surveyor, town official and toll-road owner. His home had

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2240-582: The Adirondack Mountains, reaching as far south as the 32 mi-long (51 km) Lake George in New York. Lake Champlain drains nearly half of Vermont, and approximately 250,000 people get their drinking water from the lake. The lake is fed in Vermont by the LaPlatte, Lamoille , Missisquoi , Poultney and Winooski rivers, along with Lewis Creek, Little Otter Creek and Otter Creek . In New York, it

2310-614: The American victory denied the British any leverage to demand exclusive control over the Great Lakes or territorial gains against the New England states. Three US Naval ships have been named after this battle: USS  Lake Champlain  (CV-39) , USS  Lake Champlain  (CG-57) and a cargo ship used during World War I . Following the War of 1812, the U.S. Army began construction on " Fort Blunder ": an unnamed fortification built at

2380-781: The British burned Arnold's flagship, the Royal Savage , to the east, the Americans rowed past the British lines. The following morning, the British learned of the Americans' escape and set out after the fleeing Continental vessels. On October 13, the British fleet caught up to the struggling American ships near Split Rock Mountain . With no hope of fighting off the powerful British navy, Arnold ordered his men to run their five vessels aground in Ferris Bay, Panton, Vermont . The depleted Continental army escaped on land back to Fort Ticonderoga and Mount Independence ; however, they no longer controlled

2450-402: The British fleet on Lake Champlain. By the end of the summer of 1776, the opposing armies were prepared to battle over the strategic advantage of controlling Lake Champlain. On October 11, 1776, the British and American naval fleets met on the western side of Valcour Island , on Lake Champlain. American General Benedict Arnold established the location, as it provided the Continental fleet with

2520-534: The British took control of the fort. However, Burgoyne's southern campaign did not go uncontested. On October 7, 1777, American General Horatio Gates , who occupied Bemis Heights , met Burgoyne's army at the Second Battle of Freeman's Farm . At Freeman's Farm, Burgoyne's army suffered its final defeat and ended its invasion south into the colonies. Ten days later, on October 17, 1777, British General Burgoyne surrendered his army at Saratoga . This defeat

2590-481: The British. Thus, the colonial militias devised a plan to take control of the two forts and bring the guns back to the fight in Boston. The necessity of controlling the two forts at Ticonderoga and Crown Point placed Lake Champlain as a strategic arena during the Revolutionary War. By taking control of these forts, Americans not only gained heavy artillery, but control of a vast water highway as well: Lake Champlain provided

2660-444: The Champlain Valley from 1778 to 1780, and Lake Champlain permitted direct transportation of supplies from the British posts at the northern end of the lake. With the end of the Revolutionary War in 1783, the British naval fleet on Lake Champlain retreated up to St. John's. However, British troops garrisoned at Fort Dutchman's Point ( North Hero, Vermont ) and Fort au Fer ( Champlain, New York ), on Lake Champlain, did not leave until

2730-520: The Champlain Valley. The goal of this invasion was to divide the New England colonies, thus forcing the Continental Army into a separated fight on multiple fronts. Lake Champlain provided Burgoyne with protected passage deep into the American colonies . Burgoyne's army reached Fort Ticonderoga and Mount Independence in late June, 1777. During the night of July 5, the American forces fled Ticonderoga as

2800-421: The Lake Champlain waterway. The approaching winter of 1776–1777 restricted British movement along the recently controlled Lake Champlain. As the British abandoned Crown Point and returned to Canada for the winter, the Americans reduced their garrisons in the Champlain Valley from 13,000 to 2,500 soldiers. In early 1777, British General John Burgoyne led 8,000 troops from Canada, down Lake Champlain and into

2870-512: The October 1776, the Continental Army had 16 operating naval vessels on Lake Champlain: a great increase to the four small ships they had at the beginning of the summer. General Benedict Arnold commanded the American naval fleet on Lake Champlain, which was composed of volunteers and soldiers drafted from the Northern Army. With great contrast to the Continental navy, experienced Royal Navy officers, British seamen and Hessian artillerymen manned

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2940-818: The border with Massachusetts to the border with Quebec , Canada . The part of the same range that is in Massachusetts and Connecticut is known as The Berkshires or the Berkshire Hills (with the Connecticut portion, mostly in Litchfield County , locally called the Northwest Hills or Litchfield Hills) and the Quebec portion is called the Sutton Mountains, or Monts Sutton  [ fr ] in French. All mountains in Vermont are often referred to as

3010-620: The continuity of the Burgess Branch (coming from the southwest). From its source, the Missisquoi River flows over 117.3 kilometres (72.9 mi), with a drop of 218 metres (715 ft), according to the following segments: Upper course (in Vermont) (segment of 34.7 kilometres (21.6 mi), with a drop of 87 metres (285 ft)) In upper course, Missisquoi River flows north past Troy and North Troy , crosses Big Falls State Park and

3080-443: The fight in Boston. Benedict Arnold shared the command with Allen, and, in early May 1775, they captured Fort Ticonderoga, Crown Point and the southern Loyalist settlement of Skenesborough . As a result of Allen's offensive attack on the Champlain Valley in 1775, the American forces controlled the Lake Champlain waterway. The Continental Army realized the strategic advantage of controlling Lake Champlain, as it leads directly to

3150-454: The first bridge to span the lake, built from Crown Point to Chimney Point . This bridge lasted until December 2009. Severe deterioration was found, and the bridge was demolished and replaced with the Lake Champlain Bridge , which opened in November 2011. On February 19, 1932, boats were able to sail on Lake Champlain. It was the first time that the lake was known to be free of ice during the winter at that time. Lake Champlain briefly became

3220-611: The following year. In this period, the Continental Army gained strength and was victorious at Saratoga . At the start of the Revolutionary War , British forces occupied the Champlain Valley . However, it did not take long for rebel leaders to realize the importance of controlling Lake Champlain. Early in the war, the colonial militias attempted to expel the British from Boston ; however, this undertaking could not be achieved without heavy artillery. The British forts at Ticonderoga and Crown Point , on Lake Champlain, were known to have ample supplies of artillery and were weakly-manned by

3290-429: The forces now in Canada will be brought down upon us as quick as possible, having nothing to oppose them...They will doubtless try to construct some armed vessels and then endeavor to penetrate the country toward New York." (Brigadier General John Sullivan to George Washington , June 24, 1776). Both British and American forces spent the summer of 1776 building their naval fleets, at opposite ends of Lake Champlain. By

3360-431: The heart of Quebec. Immediately after taking Forts Ticonderoga and Crown Point, the Americans began planning an attack on British Canada. The American siege of Quebec was a two-pronged assault and occurred throughout the winter of 1775–1776. Brigadier General Richard Montgomery led the first assault up the Champlain Valley into Canada, while Benedict Arnold led a second army to Quebec via the Maine wilderness. Despite

3430-411: The largest include Grand Isle , Isle La Motte and North Hero : all part of Grand Isle County, Vermont . Because of Lake Champlain's connections both to the St. Lawrence Seaway via the Richelieu River , and to the Hudson River via the Champlain Canal , Lake Champlain is sometimes referred to as "The Sixth Great Lake". The Champlain Valley is the northernmost unit of a landform system known as

3500-449: The major peaks are traversed by the Long Trail , a wilderness hiking trail that runs from the southern to northern borders of the state and is overlapped by the Appalachian Trail for roughly 1 ⁄ 3 of its length. The Vermont Republic , also known as the Green Mountain Republic, existed from 1777 to 1791, at which time Vermont became the 14th state. Vermont not only takes its state nickname ("The Green Mountain State") from

3570-435: The mountains, it is named after them. The French Monts Verts or Verts Monts is literally translated as "Green Mountains". This name was suggested in 1777 by Dr. Thomas Young , an American revolutionary and Boston Tea Party participant. The University of Vermont and State Agricultural College is referred to as UVM, after the Latin Universitas Viridis Montis (University of the Green Mountains). The Green Mountains are

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3640-441: The nation's sixth Great Lake on March 6, 1998, when President Clinton signed Senate Bill 927. This bill, which was led by U.S. Senator Patrick Leahy of Vermont and reauthorized the National Sea Grant Program , contained a line declaring Lake Champlain to be a Great Lake. This status enabled its neighboring states to apply for additional federal research and education funds allocated to these national resources. However, following

3710-447: The northernmost end of Lake Champlain to protect against attacks from British Canada. Its nickname came from a surveying error: the initial phase of construction on the fort turned out to be taking place on a point 3 ⁄ 4  mi (1.2 km) north of the Canada–U.S. border. Once this error was spotted, construction was abandoned. Locals scavenged materials used in the abandoned fort for use in their homes and public buildings. By

3780-508: The old concrete bridge destroyed by the November 1927 flood. In 2016, about 60% of male smallmouth bass bore eggs ( androgyny ). Pollution from farmland runoff, containing the weedkiller atrazine is a possible suspect. Download coordinates as: Green Mountains The Green Mountains are a mountain range in the U.S. state of Vermont and are a subrange of the Appalachian Mountains . The range runs primarily south to north and extends approximately 250 miles (400 km) from

3850-414: The ports of Burlington, Vermont , Port Henry, New York , and Plattsburgh, New York , today are primarily used by small craft, ferries and lake cruise ships, they were of substantial commercial and military importance in the 18th and 19th centuries. New France allocated concessions all along Lake Champlain to French settlers and built forts to defend the waterways. In colonial times, Lake Champlain

3920-407: The relatively undeveloped coastline of the lake. The cities of Plattsburgh, New York , and Burlington, Vermont , are on the lake's western and eastern shores, respectively, and the town of Ticonderoga, New York , is in the southern part of the region. The Quebec portion is in the regional county municipalities of Le Haut-Richelieu and Brome-Missisquoi . There are a number of islands in the lake;

3990-448: The risks to humans from water-related health hazards and control the introduction, spread, and impact of non-native nuisance species to preserve the integrity of the Lake Champlain ecosystem. Senior staff who helped organize the Environmental Protection Agency in 1970 recall that International Paper was one of the first companies to call upon the brand-new agency, because it was being pressured by both New York and Vermont with regard to

4060-462: The river as a canoe route between the Lake Champlain drainage and the Saint-François River drainage. The river supports canoe traffic from Lake Champlain to Mansonville, Quebec , where there is a falls. From there, an ancient portage (carrying place) runs 6 miles (9.7 km) to Perkins Landing on Lake Memphremagog . Abenaki groups met seasonally on the bluffs at Eagle Point in Newport, Vermont , to catch and dry whitefish . The Missisquoi Valley

4130-479: The rivers flow - Berkshire, Town of Enosburgh, Village of Enosburg Falls, Jay, Lowell, Montgomery, Village of North Troy, Richford, Westfield, and the Town of Troy, and evaluate the potential benefits of the Wild & Scenic designation. At the end of the study in 2012, the committee is scheduled to provide an assessment as to whether the rivers fit designation criteria and whether designation is supported, and make recommendations of voluntary strategies for protection of

4200-444: The rivers' resources. As a result of the National Park Service and Study Committee recommendation, 46.1 miles (74.2 km) of the Missisquoi River and Trout River were added to the National Wild and Scenic River System on December 19, 2014. The Valley Bridge spans the Missisquoi River on a north-west/south-east axis. This bridge is located on the Canada-US border, between the two customs posts. The northwest part of this bridge

4270-415: The significance of Lake Champlain during the post-Revolutionary War period. During the War of 1812 , British and American forces faced each other in the Battle of Lake Champlain, also known as the Battle of Plattsburgh , fought on September 11, 1814. This ended the final British invasion of the northern states during the War of 1812. It was fought just prior to the signing of the Treaty of Ghent , and

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4340-421: The spring and summer of 1776, at opposite ends of the lake, and fought a significant naval engagement on October 11 at the Battle of Valcour Island . While it was a tactical defeat for the Americans, and the small fleet led by Benedict Arnold was almost destroyed, the Americans gained a strategic victory; the British invasion was delayed long enough so the approach of winter prevented the fall of these forts until

4410-481: The states of New York and Vermont . The lake is located at the frontier between Abenaki and Mohawk ( Iroquois Confederacy ) traditional territories. The official toponym for the lake, according to the orthography established by the Grand Council of Wanab-aki Nation, is Pitawbagok (alternative orthographies include Petonbowk and Bitawbagok), meaning "middle lake", "lake in between" or "double lake". The Mohawk name in modern orthography, as standardized in 1993,

4480-447: The strategic advantage of controlling a direct route to Quebec by way of the Champlain Valley, the American siege of British Canada during the winter of 1775 failed. The Continental Army mistakenly assumed that it would receive support from the Canadians upon their arrival at Quebec. This was not the case, and the rebel army struggled to take Quebec with diminishing supplies, support, and harsh northern winter weather. The Continental Army

4550-478: The village of Lowell . Intermediate course (in Quebec) (segment of 24.1 kilometres (15.0 mi), with a drop of 10 metres (33 ft)) Lower course (in Vermont) (segment of 58.5 kilometres (36.4 mi), with a drop of 122 metres (400 ft)) It flows west through northern Franklin County approximately 10 miles (16 km) south of the Canada–US border, past the small communities of Richford , East Berkshire , Enosburg Falls , and Sheldon Springs . On

4620-411: The west side of Interstate 89 in northwestern Franklin County, it turns to the north, passing through Missisquoi National Wildlife Refuge in its lower 5 miles (8.0 km) before entering the south end of Missisquoi Bay, an arm of Lake Champlain that straddles the Canada-Vermont border. In the last segment of 5.6 kilometres (3.5 mi) (i.e. from Dead Creek) in Swanton , the Missisquoi River crosses

4690-428: Was among the first areas of Southern Quebec's Eastern Townships to be settled by Loyalist refugees, who came upriver from camps on Missisquoi Bay. In September 2008 the government of the United States approved a bill to study the Missisquoi and Trout rivers for potential designation as Wild and Scenic Rivers. It passed the House with bi-partisan support, and the rivers could potentially receive permanent protection in

4760-473: Was forced to camp outside Quebec's walls for the winter, with reinforcements from New York, Pennsylvania , Massachusetts , New Hampshire and Connecticut allowing the soldiers to maintain their siege of the city. However, smallpox descended on both the sieging forces and their reinforcements and savaged the American force. The reinforcements traveled hundreds of miles up the frozen Lake Champlain and St. Lawrence River, but were too late and too few to influence

4830-417: Was instrumental to the momentum of the Revolutionary War, as the defeat of the British army along the Champlain-Hudson waterway convinced France to ally with the American army. Following the failed British campaign led by General Burgoyne, the British still maintained control over the Champlain waterway for the duration of the Revolutionary War. The British used the Champlain waterway to supply raids across

4900-481: Was used as a water (or, in winter, ice) passage between the Saint Lawrence and Hudson valleys. Travelers found it easier to journey by boats and sledges on the lake rather than go overland on unpaved and frequently mud-bound roads. The lake's northern tip at Saint-Jean-sur-Richelieu , Quebec (known as St. John in colonial times under British rule) is just 25 miles (40 km) from Montreal , Quebec. The southern tip at Whitehall (Skenesborough in revolutionary times)

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