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Richelieu River

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111-674: The Richelieu River ( French: [ʁiʃ(ə)ljø] ) is a river of Quebec , Canada , and a major right-bank tributary of the St. Lawrence River . It rises at Lake Champlain , from which it flows northward through Quebec and empties into the St. Lawrence. It was formerly known by the French as the Iroquois River and the Chambly River , and was named for Cardinal Richelieu ,

222-582: A lake , an ocean , or another river. A stream refers to water that flows in a natural channel , a geographic feature that can contain flowing water. A stream may also be referred to as a watercourse. The study of the movement of water as it occurs on Earth is called hydrology , and their effect on the landscape is covered by geomorphology . Rivers are part of the water cycle , the continuous processes by which water moves about Earth. This means that all water that flows in rivers must ultimately come from precipitation . The sides of rivers have land that

333-547: A trip hammer , and grind grains with a millstone . In the Middle Ages , water mills began to automate many aspects of manual labor , and spread rapidly. By 1300, there were at least 10,000 mills in England alone. A medieval watermill could do the work of 30–60 human workers. Water mills were often used in conjunction with dams to focus and increase the speed of the water. Water wheels continued to be used up to and through

444-740: A boat along certain stretches. In these religions, such as that of the Altai in Russia , the river is considered a living being that must be afforded respect. Rivers are some of the most sacred places in Hinduism. There is archeological evidence that mass ritual bathing in rivers at least 5,000 years ago in the Indus river valley . While most rivers in India are revered, the Ganges is most sacred. The river has

555-483: A breakout campaign began in 2001. Partners, such as CIME Haut-Richelieu has controlled the invasion of this plant in the harvesting. River A river is a natural freshwater stream that flows on land or inside caves towards another body of water at a lower elevation , such as an ocean , lake , or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by

666-515: A central role in various Hindu myths, and its water is said to have properties of healing as well as absolution from sins. Hindus believe that when the cremated remains of a person is released into the Ganges, their soul is released from the mortal world. Freshwater fish make up 40% of the world's fish species, but 20% of these species are known to have gone extinct in recent years. Human uses of rivers make these species especially vulnerable. Dams and other engineered changes to rivers can block

777-413: A common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape around it, forming deltas and islands where the flow slows down. Rivers rarely run in a straight line, instead, they bend or meander ; the locations of

888-408: A continuous flow of water throughout the year. This may be because an arid climate is too dry depending on the season to support a stream, or because a river is seasonally frozen in the winter (such as in an area with substantial permafrost ), or in the headwaters of rivers in mountains, where snowmelt is required to fuel the river. These rivers can appear in a variety of climates, and still provide

999-564: A habitat for aquatic life and perform other ecological functions. Subterranean rivers may flow underground through flooded caves. This can happen in karst systems, where rock dissolves to form caves. These rivers provide a habitat for diverse microorganisms and have become an important target of study by microbiologists . Other rivers and streams have been covered over or converted to run in tunnels due to human development. These rivers do not typically host any life, and are often used only for stormwater or flood control. One such example

1110-495: A large scale. This has been attributed to unusually large floods destroying infrastructure; however, there is evidence that permanent changes to climate causing higher aridity and lower river flow may have been the determining factor in what river civilizations succeeded or dissolved. Water wheels began to be used at least 2,000 years ago to harness the energy of rivers. Water wheels turn an axle that can supply rotational energy to move water into aqueducts , work metal using

1221-580: A long erosion since the end of the Ordovician to the late Tertiary. Subsequently, after being covered with a thick layer of ice during the Quaternary, the lowlands of the St. Lawrence was overwhelmed by the Champlain Sea in the wake of the collapse of the foundation underlying, therefore, the weight of glaciers. After dropping clays and sands, the sea had to decline, following the recovery of

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1332-556: A peak in the 1970s, when between two or three dams were completed every day, and has since begun to decline. New dam projects are primarily focused in China , India , and other areas in Asia . The first civilizations of Earth were born on floodplains between 5,500 and 3,500 years ago. The freshwater, fertile soil, and transportation provided by rivers helped create the conditions for complex societies to emerge. Three such civilizations were

1443-891: A ritualistic sense has been compared to the Christian ritual of baptism , famously the Baptism of Jesus in the Jordan River . Floods also appear in Norse mythology , where the world is said to emerge from a void that eleven rivers flowed into. Aboriginal Australian religion and Mesoamerican mythology also have stories of floods, some of which contain no survivors, unlike the Abrahamic flood. Along with mythological rivers, religions have also cared for specific rivers as sacred rivers. The Ancient Celtic religion saw rivers as goddesses. The Nile had many gods attached to it. The tears of

1554-425: A river can take several forms. Tidal rivers (often part of an estuary ) have their levels rise and fall with the tide . Since the levels of these rivers are often already at or near sea level, the flow of alluvium and the brackish water that flows in these rivers may be either upriver or downriver depending on the time of day. Rivers that are not tidal may form deltas that continuously deposit alluvium into

1665-1026: A river's banks can change frequently. Rivers get their alluvium from erosion , which carves rock into canyons and valleys . Rivers have sustained human and animal life for millennia, including the first human civilizations . The organisms that live around or in a river such as fish , aquatic plants , and insects have different roles, including processing organic matter and predation . Rivers have produced abundant resources for humans, including food , transportation , drinking water , and recreation. Humans have engineered rivers to prevent flooding, irrigate crops, perform work with water wheels , and produce hydroelectricity from dams. People associate rivers with life and fertility and have strong religious, political, social, and mythological attachments to them. Rivers and river ecosystems are threatened by water pollution , climate change , and human activity. The construction of dams, canals , levees , and other engineered structures has eliminated habitats, has caused

1776-460: A section of the river behind them into a lake or reservoir. This can provide nearby cities with a predictable supply of drinking water. Hydroelectricity is desirable as a form of renewable energy that does not require any inputs beyond the river itself. Dams are very common worldwide, with at least 75,000 higher than 6 feet (1.8 m) in the U.S. Globally, reservoirs created by dams cover 193,500 square miles (501,000 km ). Dam-building reached

1887-438: A water body is that body's riparian zone . Plants in the riparian zone of a river help stabilize its banks to prevent erosion and filter alluvium deposited by the river on the shore, including processing the nitrogen and other nutrients it contains. Forests in a riparian zone also provide important animal habitats . River ecosystems have also been categorized based on the variety of aquatic life they can sustain, also known as

1998-502: A water cycle that involved precipitation. The term flumen , in planetary geology , refers to channels on Saturn 's moon Titan that may carry liquid. Titan's rivers flow with liquid methane and ethane . There are river valleys that exhibit wave erosion , seas, and oceans. Scientists hope to study these systems to see how coasts erode without the influence of human activity, something that isn't possible when studying terrestrial rivers. Chambly Canal The Chambly Canal

2109-627: Is a National Historic Site of Canada in the Province of Quebec , running along the Richelieu River past Saint-Jean-sur-Richelieu , Carignan , and Chambly . Building commenced in 1831 and the canal opened in 1843. It served as a major commercial route during a time of heightened trade between the United States and Canada. Trade dwindled after World War I, and as of the 1970s, traffic has been replaced by recreational vessels. It

2220-467: Is a national historic site operated by Parks Canada . The agency also manages other national historic sites along the river: Fort Chambly, Fort Ste. Thérèse, and St. Ours Canal. Given the rich historical past of the region, the Richelieu River brings in its banks and its islands several sites, some of which are owned by Parks Canada National Historic Site Canal Chambly National Historic Site

2331-445: Is a tributary , and the place they meet is a confluence . Rivers must flow to lower altitudes due to gravity . The bed of a river is typically within a river valley between hills or mountains . Rivers flowing through an impermeable section of land such as rocks will erode the slopes on the sides of the river. When a river carves a plateau or a similar high-elevation area, a canyon can form, with cliffs on either side of

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2442-493: Is about 4 km (2.5 mi) and a maximum width of 1 km (0.62 mi)). Formerly agricultural, it is now largely residential. It previously was the site of Fort Sainte Thérèse , built in 1665, but this was abandoned at the end of the 18th century and has now disappeared. The Richelieu is one of three rivers flowing from Quebec south to north, the other two being the Châteauguay and Chaudière . Ice jams can form in

2553-504: Is also important for the lumber industry , as logs can be shipped via river. Countries with dense forests and networks of rivers like Sweden have historically benefited the most from this method of trade. The rise of highways and the automobile has made this practice less common. One of the first large canals was the Canal du Midi , connecting rivers within France to create a path from

2664-841: Is also the namesake of Fort Richelieu . Cardinal Richelieu's tenure as chief minister coincided with much of the early period of the permanent French settlement of the Quebec region of New France in the first half of the 17th century. Five forts Already an important pathway for the Iroquois, particularly the easternmost nation of the Mohawk , the Richelieu River soon became one for French traders as well. The French regime built five forts along its length: Fort Richelieu at its mouth, Fort St. Louis (or Fort Chambly ) in Chambly, Fort Sainte Thérèse and Fort Saint-Jean upriver, and Fort Ste. Anne on

2775-564: Is an ancient dam built on the Nile 4,500 years ago. The Ancient Roman civilization used aqueducts to transport water to urban areas . Spanish Muslims used mills and water wheels beginning in the seventh century. Between 130 and 1492, larger dams were built in Japan, Afghanistan, and India, including 20 dams higher than 15 metres (49 ft). Canals began to be cut in Egypt as early as 3000 BC, and

2886-448: Is at a higher elevation than the river itself, and in these areas, water flows downhill into the river. The headwaters of a river are the smaller streams that feed a river, and make up the river's source. These streams may be small and flow rapidly down the sides of mountains . All of the land uphill of a river that feeds it with water in this way is in that river's drainage basin or watershed. A ridge of higher elevation land

2997-405: Is because any natural impediment to the flow of the river may cause the current to deflect in a different direction. When this happens, the alluvium carried by the river can build up against this impediment, redirecting the course of the river. The flow is then directed against the opposite bank of the river, which will erode into a more concave shape to accommodate the flow. The bank will still block

3108-453: Is correlated with and thus can be used to predict certain data points related to rivers, such as the size of the drainage basin (drainage area), and the length of the channel. The ecosystem of a river includes the life that lives in its water, on its banks, and in the surrounding land. The width of the channel of a river, its velocity, and how shaded it is by nearby trees. Creatures in a river ecosystem may be divided into many roles based on

3219-552: Is crucial and, in the middle of the century, Saint-Jean became the most important inner harbour of Quebec and Canada. The resort has largely replaced the business generated by the Richelieu which is considered a "heritage corridor". The river, which crosses densely populated areas as well as several agricultural areas is ecologically challenged, especially in the Chambly Basin. Measures concerning wastewater treatment reduced

3330-530: Is home to more than 50 species of fish, offers excellent sport fishing opportunities. Important sport species include northern pike , longnose gar , bowfin , smallmouth bass , largemouth bass , carp , and black crappie . But the Richelieu also hosts several threatened or endangered species, such as the copper redhorse , river redhorse , and lake sturgeon , so fishing seasons and capture limits are regulated. Since agricultural products Montérégie enjoy an enviable reputation, many restaurateurs settle near

3441-497: Is in part because of a projected loss of snowpack in mountains, meaning that melting snow can't replenish rivers during warm summer months, leading to lower water levels. Lower-level rivers also have warmer temperatures, threatening species like salmon that prefer colder upstream temperatures. Attempts have been made to regulate the exploitation of rivers to preserve their ecological functions. Many wetland areas have become protected from development. Water restrictions can prevent

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3552-402: Is part of permafrost ice caps, or trace amounts of water vapor in the atmosphere. However, there is evidence that rivers flowed on Mars for at least 100,000 years. The Hellas Planitia is a crater left behind by an impact from an asteroid. It has sedimentary rock that was formed 3.7 billion years ago, and lava fields that are 3.3 billion years old. High resolution images of the surface of

3663-570: Is rarely static, the exact location of a river border may be called into question by countries. The Rio Grande between the United States and Mexico is regulated by the International Boundary and Water Commission to manage the right to fresh water from the river, as well as mark the exact location of the border. Up to 60% of fresh water used by countries comes from rivers that cross international borders. This can cause disputes between countries that live upstream and downstream of

3774-701: Is that of the Mississippi River , whose drainage basin covers 40% of the contiguous United States . The river was then used for shipping crops from the American Midwest and cotton from the American South to other states as well as the Atlantic Ocean. The role of urban rivers has evolved from when they were a center of trade, food, and transportation to modern times when these uses are less necessary. Rivers remain central to

3885-553: Is the Sunswick Creek in New York City, which was covered in the 1800s and now exists only as a sewer-like pipe. While rivers may flow into lakes or man-made features such as reservoirs , the water they contain will always tend to flow down toward the ocean . However, if human activity siphons too much water away from a river for other uses, the riverbed may run dry before reaching the sea. The outlets mouth of

3996-422: Is the case of the aplectrelle winter (Aplectrum hyemale), the leek (Allium tricoccum) and Canada lily (Lilium canadense). In the late 1990s, there was the presence of water chestnut at the mouth of the river. This invasive species threaten to stifle the fauna and flora, as it multiplies at lightning speed. The Ministry of Sustainable Development, Environment and Parks of Quebec struggle to get rid of, and indeed

4107-609: Is very high compared to that of most other regions of the province of Quebec. Just over 70% of this area is used for agricultural purposes. With the opening of the Chambly Canal in 1843, navigation became possible on the Richelieu between the Saint Lawrence River and Lake Champlain. At the southern end of the lake, New York had built the Champlain Canal (opened in 1823), which allows for navigation to

4218-842: Is what typically separates drainage basins; water on one side of a ridge will flow into one set of rivers, and water on the other side will flow into another. One example of this is the Continental Divide of the Americas in the Rocky Mountains . Water on the western side of the divide flows into the Pacific Ocean , whereas water on the other side flows into the Atlantic Ocean . Not all precipitation flows directly into rivers; some water seeps into underground aquifers . These, in turn, can still feed rivers via

4329-599: The 2024 Summer Olympics . Another example is the restoration of the Isar in Munich from being a fully canalized channel with hard embankments to being wider with naturally sloped banks and vegetation. This has improved wildlife habitat in the Isar, and provided more opportunities for recreation in the river. As a natural barrier , rivers are often used as a border between countries , cities, and other territories . For example,

4440-487: The Atlantic Ocean to the Mediterranean Sea . The nineteenth century saw canal-building become more common, with the U.S. building 4,400 miles (7,100 km) of canals by 1830. Rivers began to be used by cargo ships at a larger scale, and these canals were used in conjunction with river engineering projects like dredging and straightening to ensure the efficient flow of goods. One of the largest such projects

4551-603: The Fort Lennox , the Fort Saint-Jean . As for the national historic site of Fort Chambly , it receives every year thousands of visitors during the 20Bière% 20and% 20Saveurs http://www.bieresetsaveurs.com/ celebrated the first days of September. In addition, the curious visitor to learn more about the history of the region could go to 20of% 20Top-Richelieu http://www.museeduhaut-richelieu.com/accueilmhr.html , Saint-Jean-sur-Richelieu. Fishing The Richelieu, which

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4662-684: The Hudson River and, downstream, the city of New York , a major market and port. There the Hudson flows into the Atlantic Ocean . It is a major international trading port. Saint-Jean-sur-Richelieu, Chambly, Beloeil, Mont-Saint-Hilaire , and Sorel-Tracy are important communities on its route. The average slope of the Richelieu River is 0.19 metres per kilometre (1.0 ft/mi), but 24 metres (79 ft) in elevation between Saint-Jean-sur-Richelieu and Chambly for an average flow of 330 cubic metres per second (12,000 cu ft/s). By convention,

4773-501: The Industrial Revolution as a source of power for textile mills and other factories, but were eventually supplanted by steam power . Rivers became more industrialized with the growth of technology and the human population . As fish and water could be brought from elsewhere, and goods and people could be transported via railways , pre-industrial river uses diminished in favor of more complex uses. This meant that

4884-584: The Isle La Motte, Vermont , in Lake Champlain near its source. In the 17th century, the repeated attacks by the Iroquois endangered the existence of New France. The colonists built their first military posts: Fort Richelieu in Sorel and Fort Saint-Jean. The latter, built in 1666, became the developing center of the city of Saint-Jean, today Saint-Jean-sur-Richelieu. In the 18th century, the region

4995-791: The Lamari River in New Guinea separates the Angu and the Fore people in New Guinea. The two cultures speak different languages and rarely mix. 23% of international borders are large rivers (defined as those over 30 meters wide). The traditional northern border of the Roman Empire was the Danube , a river that today forms the border of Hungary and Slovakia . Since the flow of a river

5106-525: The Nile and the Ganges . The Quran describes these four rivers as flowing with water, milk, wine, and honey, respectively. The book of Genesis also contains a story of a great flood . Similar myths are present in the Epic of Gilgamesh , Sumerian mythology, and in other cultures. In Genesis, the flood's role was to cleanse Earth of the wrongdoing of humanity. The act of water working to cleanse humans in

5217-568: The River Continuum Concept . "Shredders" are organisms that consume this organic material. The role of a "grazer" or "scraper" organism is to feed on the algae that collects on rocks and plants. "Collectors" consume the detritus of dead organisms. Lastly, predators feed on living things to survive. The river can then be modeled by the availability of resources for each creature's role. A shady area with deciduous trees might experience frequent deposits of organic matter in

5328-627: The River Lethe to forget their previous life. Rivers also appear in descriptions of paradise in Abrahamic religions , beginning with the story of Genesis . A river beginning in the Garden of Eden waters the garden and then splits into four rivers that flow to provide water to the world. These rivers include the Tigris and Euphrates , and two rivers that are possibly apocryphal but may refer to

5439-787: The Sumerians in the Tigris–Euphrates river system , the Ancient Egyptian civilization in the Nile, and the Indus Valley Civilization on the Indus River . The desert climates of the surrounding areas made these societies especially reliant on rivers for survival, leading to people clustering in these areas to form the first cities . It is also thought that these civilizations were the first to organize

5550-485: The climate . The alluvium carried by rivers, laden with minerals, is deposited into the floodplain when the banks spill over, providing new nutrients to the soil, allowing them to support human activity like farming as well as a host of plant and animal life. Deposited sediment from rivers can form temporary or long-lasting fluvial islands . These islands exist in almost every river. About half of all waterways on Earth are intermittent rivers , which do not always have

5661-625: The cultural identity of cities and nations. Famous examples include the River Thames 's relationship to London , the Seine to Paris , and the Hudson River to New York City . The restoration of water quality and recreation to urban rivers has been a goal of modern administrations. For example, swimming was banned in the Seine for over 100 years due to concerns about pollution and the spread of E. coli , until cleanup efforts to allow its use in

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5772-484: The discharge of a river, the amount of water passing through it at a particular time. The flow of a river can act as a means of transportation for plant and animal species, as well as a barrier. For example, the Amazon River is so wide in parts that the variety of species on either side of its basin are distinct. Some fish may swim upstream to spawn as part of a seasonal migration . Species that travel from

5883-465: The extinction of some species, and lowered the amount of alluvium flowing through rivers. Decreased snowfall from climate change has resulted in less water available for rivers during the summer. Regulation of pollution, dam removal , and sewage treatment have helped to improve water quality and restore river habitats. A river is a natural flow of freshwater that flows on or through land towards another body of water downhill. This flow can be into

5994-436: The sea . The sediment yield of a river is the quantity of sand per unit area within a watershed that is removed over a period of time. The monitoring of the sediment yield of a river is important for ecologists to understand the health of its ecosystems, the rate of erosion of the river's environment, and the effects of human activity. Rivers rarely run in a straight direction, instead preferring to bend or meander . This

6105-425: The softshell turtle , which is an endangered species. But the wildlife species most frequently sighted are birds . Because the river flows in a north-south axis, it is a migration corridor and one can observe several migrating birds . A staging area is located near Saint-Jean-sur-Richelieu , and depending on the time of year, birdswatchers can see various species of birds. For example, in the fall, visitors can see

6216-475: The water cycle , the processes by which water moves around the Earth. Water first enters rivers through precipitation , whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow , or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins , areas where surface water eventually flows to

6327-521: The water table , the groundwater beneath the surface of the land stored in the soil . Water flows into rivers in places where the river's elevation is lower than that of the water table. This phenomenon is why rivers can still flow even during times of drought . Rivers are also fed by the melting of snow glaciers present in higher elevation regions. In summer months, higher temperatures melt snow and ice, causing additional water to flow into rivers. Glacier melt can supplement snow melt in times like

6438-568: The British built Fort Lennox on an island of the Richelieu River, near the Canada-U.S. border, to prevent against possible attacks from Americans, whom they had fought during the War of 1812 . The British and French built large fortified posts, as shown by Fort Lennox at Île aux Noix, Fort Sainte Thérèse, and Fort St. Louis (or Fort Chambly). The security offered by the forts and the fertile lands of

6549-466: The Richelieu River to combine fine dining and picturesque landscape. True country of maple and apple cider and sugar shacks abound in the area. In urban and agricultural areas, there are mainly small mammals such as skunks , raccoon , squirrel and marmots . Forest areas, which represent 16% of the land in the watershed, host a variety of wildlife: there are among others American mink , deer , beaver , frogs and several species of turtles including

6660-604: The Richelieu is generally divided into three main sections: Several river islands are along the route of the Richelieu River. Arguably the most famous, Île aux Noix is in the Haut-Richelieu and houses Fort Lennox , considered a national historic site of Canada. Downstream, the Sainte-Thérèse Island near Saint-Jean-sur-Richelieu (in Saint-Luc's sector), is the largest island on the Richelieu (its length

6771-442: The Richelieu. Railroad development However, by the end of the 19th century railroads had largely replaced the river as commercial arteries. A tragic intersection of the two modes of transport occurred in 1864 when a train plunged off a swing bridge into the river after missing a red signal , killing 99 people. Tourist industry Tourists visit New York and Montreal through the river. Its contribution to regional prosperity

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6882-521: The Richelieu. The main Richelieu tributaries are rivers: Acadia , South Huron and Lacolle . The river's mean discharge is 330 cubic metres per second (12,000 cu ft/s). Nearly 340,000 people across eight Regional county municipalities (RCM in English or MRC in French) and 65 municipalities, live in the Quebec portion of the watershed of the river. The population density (140 inhabitants per km)

6993-516: The U.S. portion of the Lakes to Locks Passage , linking with the Hudson River and allowing navigation using the Richelieu between the St. Lawrence River and New York City and the Erie Canal . The Piste cyclable du Canal-de-Chambly is a 20 km (12 mi) bicycle path that follows the towpath along the canal. The bike path is part of Quebec's Route Verte bicycle path network. The canal

7104-648: The United States, originating in the western slopes of the Green Mountains and the eastern slopes of the Adirondack Mountains of New York State . The Champlain Valley makes up most of the drainage basin. With a length of 124 km (77 mi), the Richelieu River takes its source at the north end of Lake Champlain, now on the border between Canada ( Quebec ) and the United States ( Vermont and New York state). The river flows through many towns in Quebec: Lacolle , Île aux Noix , Saint-Jean-sur-Richelieu , Chambly , Beloeil , Saint-Charles-sur-Richelieu , Saint-Denis-sur-Richelieu , Saint-Ours and Sorel-Tracy , where

7215-422: The area. This group (sub-formation Chambly) contains the younger sedimentary rocks of the region: a series of shales and "calcaireuses" that turn red in the upper parts. Historically, the formation of rocks in the region is due to its immersion, towards the end of the Ordovician geological era, which led to the establishment of marine sediments. Then raised by tectonic forces, the entire region has been subjected to

7326-596: The arrival of thousands of geese and ducks . One can also see the loggerhead shrike (an endangered species), as well as the peregrine and golden eagle (classified as a vulnerable species), and cerulean warblers , to name but a few. Regarding the flora, the catchment of the River belongs to the bioclimatic domain maple-hickory hickory. It includes among others sugar maple and silver maple of hickory hickory of bur oak and oak bicolor of American elms and black ash, and several bushes and herbaceous . Of these, several are considered vulnerable or endangered. This

7437-406: The base, and left the area in its current state. The valley has a few pronounced relief that is covered with a large clay deposit of up to 50 metres (160 ft) thick. The lowlands were once part of plain of alluviums of St. Lawrence valley, greater than it is today. In a relatively recent geological time, glaciation changed the relief which subsequently was reduced by sediment deposits dating from

7548-695: The bodies of humans and animals worldwide, as well as in the soil, with potentially negative health effects. Research into how to remove it from the environment, and how harmful exposure is, is ongoing. Fertilizer from farms can lead to a proliferation of algae on the surface of rivers and oceans, which prevents oxygen and light from dissolving into water, making it impossible for underwater life to survive in these so-called dead zones . Urban rivers are typically surrounded by impermeable surfaces like stone, asphalt , and concrete. Cities often have storm drains that direct this water to rivers. This can cause flooding risk as large amounts of water are directed into

7659-422: The canals, and the Hudson River . The construction of rail transport in the mid-19th century competed with such river/canal routes and ultimately succeeded them, because of faster service with greater freight capacity. Because of the river's strategic position between New France and New England , several military fortifications were erected on its course. It served as a key pathway for several military tours and

7770-405: The complete draining of rivers. Limits on the construction of dams, as well as dam removal , can restore the natural habitats of river species. Regulators can also ensure regular releases of water from dams to keep animal habitats supplied with water. Limits on pollutants like pesticides can help improve water quality. Today, the surface of Mars does not have liquid water. All water on Mars

7881-436: The effect of normalizing the effects of rivers; the greatest floods are smaller and more predictable, and larger sections are open for navigation by boats and other watercraft. A major effect of river engineering has been a reduced sediment output of large rivers. For example, the Mississippi River produced 400 million tons of sediment per year. Due to the construction of reservoirs , sediment buildup in man-made levees , and

7992-565: The entire region. The little furniture or not permeable deposits consist of unconsolidated sediments which occupy 62 percent of the area. It includes the compact clay or silty matrix till, glaciolacustrine sediments for the Champlain Sea clay, fine current and organic sediment floodplain sediments. Indigenous occupation The Richelieu River was territory of the Iroquois and Abenaki , confederacies whose peoples were primarily based to

8103-423: The establishment of wells that can theoretically power a community network or industry. In the second case, there are formation that permit at most the implementation of individual wells. A third category has emerged, that of permeable surficial buried underlying impermeable horizon, which are often highly productive aquifers. Permeable surficial sand and gravel together from various sources and represent 18 percent of

8214-451: The fish zonation concept. Smaller rivers can only sustain smaller fish that can comfortably fit in its waters, whereas larger rivers can contain both small fish and large fish. This means that larger rivers can host a larger variety of species. This is analogous to the species-area relationship , the concept of larger habitats being host to more species. In this case, it is known as the species-discharge relationship, referring specifically to

8325-673: The floating of wood on rivers to transport it, was especially important. Rivers also were an important source of drinking water . For civilizations built around rivers, fish were an important part of the diet of humans. Some rivers supported fishing activities, but were ill-suited to farming, such as those in the Pacific Northwest . Other animals that live in or near rivers like frogs , mussels , and beavers could provide food and valuable goods such as fur . Humans have been building infrastructure to use rivers for thousands of years. The Sadd el-Kafara dam near Cairo , Egypt,

8436-412: The flow of the river beneath its surface. These help rivers flow straighter by increasing the speed of the water at the middle of the channel, helping to control floods. Levees are also used for this purpose. They can be thought of as dams constructed on the sides of rivers, meant to hold back water from flooding the surrounding area during periods of high rainfall. They are often constructed by building up

8547-399: The flow, causing it to reflect in the other direction. Thus, a bend in the river is created. Rivers may run through low, flat regions on their way to the sea. These places may have floodplains that are periodically flooded when there is a high level of water running through the river. These events may be referred to as "wet seasons' and "dry seasons" when the flooding is predictable due to

8658-650: The form of leaves. In this type of ecosystem, collectors and shredders will be most active. As the river becomes deeper and wider, it may move slower and receive more sunlight . This supports invertebrates and a variety of fish , as well as scrapers feeding on algae. Further downstream, the river may get most of its energy from organic matter that was already processed upstream by collectors and shredders. Predators may be more active here, including fish that feed on plants, plankton , and other fish. The flood pulse concept focuses on habitats that flood seasonally, including lakes and marshes . The land that interfaces with

8769-508: The goddess Isis were said to be the cause of the river's yearly flooding, itself personified by the goddess Hapi . Many African religions regard certain rivers as the originator of life. In Yoruba religion , Yemọja rules over the Ogun River in modern-day Nigeria and is responsible for creating all children and fish. Some sacred rivers have religious prohibitions attached to them, such as not being allowed to drink from them or ride in

8880-428: The irrigation of desert environments for growing food. Growing food at scale allowed people to specialize in other roles, form hierarchies, and organize themselves in new ways, leading to the birth of civilization. In pre-industrial society , rivers were a source of transportation and abundant resources. Many civilizations depended on what resources were local to them to survive. Shipping of commodities, especially

8991-434: The late summer, when there may be less snow left to melt, helping to ensure that the rivers downstream of the glaciers have a continuous supply of water. Rivers flow downhill, with their direction determined by gravity . A common misconception holds that all or most rivers flow from North to South, but this is not true. As rivers flow downstream, they eventually merge to form larger rivers. A river that feeds into another

9102-474: The level of river branching in a drainage basin. Several systems of stream order exist, one of which is the Strahler number . In this system, the first tributaries of a river are 1st order rivers. When two 1st order rivers merge, the resulting river is 2nd order. If a river of a higher order and a lower order merge, the order is incremented from whichever of the previous rivers had the higher order. Stream order

9213-561: The local ecosystems of rivers needed less protection as humans became less reliant on them for their continued flourishing. River engineering began to develop projects that enabled industrial hydropower , canals for the more efficient movement of goods, as well as projects for flood prevention . River transportation has historically been significantly cheaper and faster than transportation by land. Rivers helped fuel urbanization as goods such as grain and fuel could be floated downriver to supply cities with resources. River transportation

9324-407: The mechanical shadoof began to be used to raise the elevation of water. Drought years harmed crop yields, and leaders of society were incentivized to ensure regular water and food availability to remain in power. Engineering projects like the shadoof and canals could help prevent these crises. Despite this, there is evidence that floodplain-based civilizations may have been abandoned occasionally at

9435-400: The migration routes of fish and destroy habitats. Rivers that flow freely from headwaters to the sea have better water quality, and also retain their ability to transport nutrient-rich alluvium and other organic material downstream, keeping the ecosystem healthy. The creation of a lake changes the habitat of that portion of water, and blocks the transportation of sediment, as well as preventing

9546-399: The natural meandering of the river. Dams block the migration of fish such as salmon for which fish ladder and other bypass systems have been attempted, but these are not always effective. Pollution from factories and urban areas can also damage water quality. " Per- and polyfluoroalkyl substances (PFAS) is a widely used chemical that breaks down at a slow rate. It has been found in

9657-429: The natural terrain with soil or clay. Some levees are supplemented with floodways, channels used to redirect floodwater away from farms and populated areas. Dams restrict the flow of water through a river. They can be built for navigational purposes, providing a higher level of water upstream for boats to travel in. They may also be used for hydroelectricity , or power generation from rivers. Dams typically transform

9768-425: The plain show evidence of a river network, and even river deltas. These images reveal channels formed in the rock, recognized by geologists who study rivers on Earth as being formed by rivers, as well as "bench and slope" landforms, outcroppings of rock that show evidence of river erosion. Not only do these formations suggest that rivers once existed, but that they flowed for extensive time periods, and were part of

9879-534: The post-glacial of Champlain Sea. The most prominent of the watershed of the river geological formation is also formed by the Monteregian Hills . In addition, nearly half of the banks of the Richelieu River are kept in natural state. Regarding the hydrogeology of the area, there are two major classes of surficial: permeable and little or no permeability. In the first case, we find sand and gravel formations for

9990-515: The powerful minister under Louis XIII . This river was a long a key route of water transport for trading, first by indigenous peoples, and then for cross-border trade between Canada and the United States. With 19th-century construction of the Champlain Canal (1823) south of Lake Champlain and the Chambly Canal (1843) to the north, the Richelieu provided a direct route from the Saint Lawrence River to New York via Lake Champlain ,

10101-591: The presence of certain pollutants in recent years. The Richelieu River caused extensive flooding during the spring of 2011, damaging or destroying more than 3,000 homes in Quebec and at least 750 in Vermont. Although its commercial significance has waned, the Richelieu has remained an important recreational waterway. The Chambly Canal (9 locks) permits pleasure boats to bypass the rapids at Saint-Jean-sur-Richelieu and Chambly. The Champlain Canal and Lake Champlain form

10212-482: The rapids and allowing easier transportation of export products such as sawlogs, pulp, hay, and coal from Canada to the United States. Following the first channel, a network of channels was formed. These allowed those traversing the Richelieu to access the Hudson River and then New York. Sorel and Saint-Jean-sur-Richelieu, which were both incorporated in the 1850s, arose as a direct result of the increased traffic on

10323-448: The removal of natural banks replaced with revetments , this sediment output has been reduced by 60%. The most basic river projects involve the clearing of obstructions like fallen trees. This can scale up to dredging , the excavation of sediment buildup in a channel, to provide a deeper area for navigation. These activities require regular maintenance as the location of the river banks changes over time, floods bring foreign objects into

10434-471: The result of deposition of shoreline. The Utica shale usually contain an abundance of mica flakes and important content of quartz . The Utica shale is especially conducive to shale gas exploitation. Those of Lorraine group are dark gray color, and contain also sandstone lenses up to 5 cm (2.0 in) thick. These are the rocks of the Lorraine Group (sub-formation Breault) that cover most of

10545-536: The reverse, death and destruction, especially through floods . This power has caused rivers to have a central role in religion , ritual , and mythology . In Greek mythology , the underworld is bordered by several rivers. Ancient Greeks believed that the souls of those who perished had to be borne across the River Styx on a boat by Charon in exchange for money. Souls that were judged to be good were admitted to Elysium and permitted to drink water from

10656-607: The river attracted farmers. In the early nineteenth century the region of Haut-Richelieu got its nickname, the "Valley of the strongholds" ( Vallée des forts ). After the period of the British conquest of New France in 1759–1760, and after the American War of Independence by the Thirteen Colonies (1776–1783), the Crown offered British military and Loyalists land for their service and in compensation for losses in what

10767-428: The river empties into the Saint Lawrence River , around 40 km (25 mi) northeast of Montreal and southwest of Quebec City . The Richelieu River is the largest tributary of the south or right shore of the Saint Lawrence River and drains a large area of southern Quebec. The Quebec portion of the watershed (about 15% of its total area) includes 18 lakes and ponds, as well as forty rivers and tributary streams of

10878-468: The river, and natural sediment buildup continues. Artificial channels are often constructed to "cut off" winding sections of a river with a shorter path, or to direct the flow of a river in a straighter direction. This effect, known as channelization, has made the distance required to traverse the Missouri River in 116 kilometres (72 mi) shorter. Dikes are channels built perpendicular to

10989-552: The river. Areas of a river with softer rock weather faster than areas with harder rock, causing a difference in elevation between two points of a river. This can cause the formation of a waterfall as the river's flow falls down a vertical drop. A river in a permeable area does not exhibit this behavior and may even have raised banks due to sediment. Rivers also change their landscape through their transportation of sediment , often known as alluvium when applied specifically to rivers. This debris comes from erosion performed by

11100-625: The river. A country that is downstream of another may object to the upstream country diverting too much water for agricultural uses, pollution, as well as the creation of dams that change the river's flow characteristics. For example, Egypt has an agreement with Sudan requiring a specific minimum volume of water to pass into the Nile yearly over the Aswan Dam , to maintain both countries access to water. The importance of rivers throughout human history has given them an association with life and fertility . They have also become associated with

11211-457: The rivers themselves, debris swept into rivers by rainfall, as well as erosion caused by the slow movement of glaciers. The sand in deserts and the sediment that forms bar islands is from rivers. The particle size of the debris is gradually sorted by the river, with heavier particles like rocks sinking to the bottom, and finer particles like sand or silt carried further downriver . This sediment may be deposited in river valleys or carried to

11322-412: The rivers. Due to these impermeable surfaces, these rivers often have very little alluvium carried in them, causing more erosion once the river exits the impermeable area. It has historically been common for sewage to be directed directly to rivers via sewer systems without being treated, along with pollution from industry. This has resulted in a loss of animal and plant life in urban rivers, as well as

11433-409: The sea from their mouths. Depending on the activity of waves, the strength of the river, and the strength of the tidal current, the sediment can accumulate to form new land. When viewed from above, a delta can appear to take the form of several triangular shapes as the river mouth appears to fan out from the original coastline . In hydrology , a stream order is a positive integer used to describe

11544-414: The sea to breed in freshwater rivers are anadromous. Salmon are an anadromous fish that may die in the river after spawning, contributing nutrients back to the river ecosystem. Modern river engineering involves a large-scale collection of independent river engineering structures that have the goal of flood control , improved navigation, recreation, and ecosystem management. Many of these projects have

11655-519: The spread of waterborne diseases such as cholera . In modern times, sewage treatment and controls on pollution from factories have improved the water quality of urban rivers. Climate change can change the flooding cycles and water supply available to rivers. Floods can be larger and more destructive than expected, causing damage to the surrounding areas. Floods can also wash unhealthy chemicals and sediment into rivers. Droughts can be deeper and longer, causing rivers to run dangerously low. This

11766-572: The spring with the melting of ice in the south while the north is still frozen, causing floods. The valley of the Richelieu river is based on sedimentary rocks formed during the Cambrian of the Paleozoic era around 450 million years ago. The bedrock consists of shale clay and sandstone. The shales are sedimentary rocks from the mechanical disintegration of preexisting rocks. The sandstones are composed of quartz grains joined together and are always

11877-563: The west and south, and the east and north, respectively. French explorers In 1535, the French explorer Jacques Cartier discovered the mouth of Richelieu River, during his second voyage in New France (Canada). Samuel de Champlain and his team reached the mouth of the river in 1603. Champlain returned to the river in 1608 and in 1609, exploring upriver and through Lake Champlain to modern-day Albany, New York . Toponymy The river

11988-589: Was a strategic location increasingly coveted by both the French and British colonial empires. The two powers wanted to expand their territory and control the lucrative fur trade. After defeating France in the Seven Years' War (known as the French and Indian War in North America), Great Britain took over its territory of New France east of the Mississippi River in 1763. Between 1819 and 1829,

12099-597: Was formerly known as "Masoliantekw" , which means "water where there is plenty of food" in Abenaki . Because of their encounters with the Iroquois nations along this way, the French called it the Riviere Iroquois at the beginning of the colony. Some early journals and maps refer to the lower river as the Sorel River. It was named for the powerful Cardinal Richelieu (1585–1642), Minister of Louis XIII , who

12210-476: Was now the United States. Numerous new settlers chose the banks of the Richelieu. During the Lower Canada Rebellion of 1837, the battles of Saint-Denis and Saint-Charles occurred along the Richelieu. Economy During the 19th century, the Richelieu became an important economic thoroughfare instead of a path for war. In 1843, the construction of the Chambly Canal was completed, bypassing

12321-558: Was the scene of several battles between the end of the 17th and early 19th centuries, first between the French and the Iroquois; then between the French and the English, during the regime of New France; and finally between the British and the rebel Americans after 1760. The Richelieu River has a drainage basin of 23,720 square kilometres (9,160 sq mi) – including those of Lake Champlain 19,925 km (7,693 sq mi) and Missisquoi Bay (1,289 km (498 sq mi)). Of this, 19,600 km (7,600 sq mi) are in

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