Lake Champlain ( ; , ) is a large natural freshwater lake in North America. With a length of and surface area over , it lies mostly between the U.S. states of New York and Vermont, but also extends north into the Canadian province of Quebec.
Burlington, Vermont, and Plattsburgh, New York, are the largest settlements on the lake, and towards the south lies the historic Fort Ticonderoga in New York. The Quebec portion is in the regional county municipalities of Le Haut-Richelieu and Brome-Missisquoi. There are numerous islands in the lake; the largest include Grand Isle, Isle La Motte and North Hero: all part of Grand Isle County, Vermont. Because of its 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 coastline is relatively undeveloped and hosts several state parks, including North Hero and Button Bay in Vermont, and Cumberland Bay in New York. Much of New York's shoreline is located within the larger Adirondack Park. The lake is a significant part of local culture, especially Champ, a lake monster that allegedly resides there.
Hydrology
Lake Champlain covers approximately , making it the thirteenth-largest lake by area in the U.S. It lies at an elevation of , is , has a shoreline, averages in width, has an average depth of , a maximum depth of , and holds some of water.
Located in the Champlain Valley between the Green Mountains of Vermont and the Adirondack Mountains of New York, it is drained northward by the Richelieu River into the St. Lawrence River at Sorel-Tracy, Quebec. The Champlain basin covers and collects waters from the northwestern slopes of the Green Mountains and the eastern portion of the Adirondack Mountains, reaching as far south as the Lake George in New York. The lake drains nearly half of Vermont, and approximately 250,000 people get their drinking water from it.
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 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 .
Geology
The Champlain Valley is the northernmost unit of a landform system known as the Great Appalachian Valley, which stretches between Quebec to the north and Alabama to the south. The Champlain Valley is a physiographic section of the larger St. 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, the Northern United States, and the Northwest Territories.
The Chazy Reef 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.
History
The lake has long acted as a border between indigenous nations, much as it is today between 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 Waban-aki Nation, is Pitawbagok (alternative orthographies include Petonbowk and Bitawbagok), meaning "middle lake", "lake in between" or "double lake".
The Mohawk language name in modern orthography, as standardized in 1993, 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 1609. While 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.
Colonial America and the Revolutionary War
New France allocated concessions all along Lake Champlain to French settlers and built forts to defend the waterways. In colonial times, Lake Champlain was used as a water or 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 from Montreal. The southern tip at Whitehall (Skenesborough in colonial times) is north of Glens Falls on the Hudson River and north of Albany, New York.
Beginning of the Revolutionary War At the start of the Revolutionary War, British forces occupied the Champlain Valley. However, it did not take long for American 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.Countryman (2003), p. 103 The British forts Ticonderoga and Crown Point were known to have ample supplies of artillery and were weakly manned by 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 placed Lake Champlain as a strategic arena during the Revolutionary War.
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 the fight in Boston. Benedict Arnold shared the command with Allen, and they captured Fort Ticonderoga, Crown Point and the southern Loyalist settlement of Skenesborough. By taking control of these forts, Americans gained heavy artillery as well as control of a vast water highway: Lake Champlain provided 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.
Siege of Quebec: 1775–1776 Immediately after taking Forts Ticonderoga and Crown Point, the Americans began planning an attack on British Canada. The siege of Quebec was a two-pronged assault and occurred throughout the winter of 1775–76. Brigadier General Richard Montgomery led the first assault up the Champlain Valley into Canada, while Arnold led a second army to Quebec via the Maine wilderness. Despite the strategic advantage of controlling a direct route to Quebec by way of the Champlain Valley, the siege 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 Continental Army struggled to take Quebec with diminishing supplies, support, and harsh northern winter weather.
The Continental Army 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 they were too late and too few to influence 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.
Both British and American forces spent the summer of 1776 building their naval fleets, at opposite ends of Lake Champlain. By 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. 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 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.
Battle of Valcour Island On October 11, 1776, the British and American naval fleets met on the western side of Valcour Island. Arnold established the location, as it provided the Continental fleet with a natural defensive position. The British and American vessels engaged in combat for much of the day, only stopping at 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 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 the Lake Champlain waterway.
The approaching winter of 1776–77 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.
General Burgoyne's campaign
In early 1777, British General John Burgoyne led 8,000 troops from Canada, down Lake Champlain and into 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 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 Battle of Bemis Heights. Burgoyne's army suffered its final defeat and ended its invasion south into the colonies. On October 17 Burgoyne surrendered his army at Saratoga. This defeat 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 Americans.
Aftermath of 1777