Misplaced Pages

#597402

84-642: The path follows both shores of the Charles River from Boston, Massachusetts to Norumbega Park in Newton , passing through Watertown and Waltham . The path consists of several segments in the Charles River Reservation separated by road and bridge crossings and forms part of the planned East Coast Greenway , the 3,000-mile trail system connecting cities from Maine to Florida. The Paul Dudley White Bicycle Path runs on both sides of

168-424: A lake , bay or ocean but joins another river (a parent river). Sometimes also called a branch or fork. A distributary , or a distributary channel , is a stream that branches off and flows away from a main stream channel, and the phenomenon is known as river bifurcation . Distributaries are common features of river deltas , and are often found where a valleyed stream enters wide flatlands or approaches

252-403: A bed armor layer, and other depositional features, plus well defined banks due to bank erosion, are good identifiers when assessing for perennial streams. Particle size will help identify a perennial stream. Perennial streams cut through the soil profile, which removes fine and small particles. By assessing areas for relatively coarse material left behind in the stream bed and finer sediments along

336-401: A continuous body of surface water flowing within the bed and banks of a channel . Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long, large streams are usually called rivers , while smaller, less voluminous and more intermittent streams are known as streamlets , brooks or creeks . The flow of a stream

420-658: A continuous aquatic habitat until they reach maturity. Crayfish and other crustaceans , snails , bivalves (clams), and aquatic worms also indicate the stream is perennial. These require a persistent aquatic environment for survival. Fish and amphibians are secondary indicators in assessment of a perennial stream because some fish and amphibians can inhabit areas without persistent water regime. When assessing for fish, all available habitat should be assessed: pools, riffles, root clumps and other obstructions. Fish will seek cover if alerted to human presence, but should be easily observed in perennial streams. Amphibians also indicate

504-470: A continuous or intermittent stream. The same non-perennial channel might change characteristics from intermittent to ephemeral over its course. Washes can fill up quickly during rains, and there may be a sudden torrent of water after a thunderstorm begins upstream, such as during monsoonal conditions. In the United States, an intermittent or seasonal stream is one that only flows for part of

588-422: A drainage network. Although each tributary has its own source, international practice is to take the source farthest from the river mouth as the source of the entire river system, from which the most extended length of the river measured as the starting point is taken as the length of the whole river system, and that furthest starting point is conventionally taken as the source of the whole river system. For example,

672-404: A path into mines or other underground chambers. According to official U.S. definitions, the channels of intermittent streams are well-defined, as opposed to ephemeral streams, which may or may not have a defined channel, and rely mainly on storm runoff, as their aquatic bed is above the water table . An ephemeral stream does not have the biological, hydrological, and physical characteristics of

756-412: A perennial stream and include tadpoles , frogs , salamanders , and newts . These amphibians can be found in stream channels, along stream banks, and even under rocks. Frogs and tadpoles usually inhabit shallow and slow moving waters near the sides of stream banks. Frogs will typically jump into water when alerted to human presence. Well defined river beds composed of riffles, pools, runs, gravel bars,

840-483: A perennial stream, fine sediment may cling to riparian plant stems and tree trunks. Organic debris drift lines or piles may be found within the active overbank area after recent high flow. Streams, headwaters, and streams flowing only part of the year provide many benefits upstream and downstream. They defend against floods, remove contaminants, recycle nutrients that are potentially dangerous as well as provide food and habitat for many forms of fish. Such streams also play

924-713: A rowing and sculling locale, with many boathouses and the three-mile Head of the Charles Regatta , the world's largest long-distance rowing regatta. The major boathouses, starting up stream near Watertown, are Community Rowing, Inc. , housing competitive, recreational, and learning programs along with the Boston College Crew; Northeastern University's Henderson; Cambridge Boat Club; Newell , home of Harvard Men's Rowing; Weld , home of Harvard Women's Rowing; Riverside Boat Club; Boston University's DeWolfe; Massachusetts Institute of Technology's Pierce; and, in

SECTION 10

#1732787831598

1008-406: A slow-moving wetted channel or stagnant area. This is evidence that iron-oxidizing bacteria are present, indicating persistent expression of oxygen-depleted ground water. In a forested area, leaf and needle litter in the stream channel is an additional indicator. Accumulation of leaf litter does not occur in perennial streams since such material is continuously flushed. In the adjacent overbank of

1092-486: A stream as intermittent, "showing interruptions in time or space". Generally, streams that flow only during and immediately after precipitation are termed ephemeral . There is no clear demarcation between surface runoff and an ephemeral stream, and some ephemeral streams can be classed as intermittent—flow all but disappearing in the normal course of seasons but ample flow (backups) restoring stream presence — such circumstances are documented when stream beds have opened up

1176-424: A stream is a critical factor in determining its character and is entirely determined by its base level of erosion. The base level of erosion is the point at which the stream either enters the ocean, a lake or pond, or enters a stretch in which it has a much lower gradient, and may be specifically applied to any particular stretch of a stream. In geological terms, the stream will erode down through its bed to achieve

1260-524: A thin layer called sheet wash, combined with a network of tiny rills, which together form the sheet runoff; when this water is focused in a channel, a stream is born. Some rivers and streams may begin from lakes or ponds. Freshwater's primary sources are precipitation and mountain snowmelt. However, rivers typically originate in the highlands, and are slowly created by the erosion of mountain snowmelt into lakes or rivers. Rivers usually flow from their source topographically, and erode as they pass until they reach

1344-627: A vital role in preserving our drinking water quality and supply, ensuring a steady flow of water to surface waters and helping to restore deep aquifers. The extent of land basin drained by a stream is termed its drainage basin (also known in North America as the watershed and, in British English, as a catchment). A basin may also be composed of smaller basins. For instance, the Continental Divide in North America divides

1428-555: A way to use the Charles to power mills. In 1639, the town dug a canal from the Charles to a nearby brook that drained to the Neponset River . By this action, a portion of the Charles's flow was diverted, providing enough current for several mills. The new canal and the brook together are now called Mother Brook . The canal is regarded as the first industrial canal in North America. It remains in use for flood control . Waltham

1512-414: Is a large natural stream that is much wider and deeper than a creek and not easily fordable, and may be a navigable waterway . The linear channel between the parallel ridges or bars on a shoreline beach or river floodplain, or between a bar and the shore. Also called a swale . A tributary is a contributory stream to a larger stream, or a stream which does not reach a static body of water such as

1596-560: Is common along the Charles. With catches from the Charles from Natick to Boston the public is advised not to eat carp , and for non-pregnant, non-nursing adults, to limit large mouth bass consumption to no more than twice a month. Children and pregnant or nursing women should eat nothing from the Charles River. Both cautions are due to PCB and pesticide contamination. Up river from Natick, similar advisories are in effect for all fish on account of mercury , chlordane , and DDT in

1680-565: Is controlled by three inputs – surface runoff (from precipitation or meltwater ), daylighted subterranean water , and surfaced groundwater ( spring water ). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in

1764-586: Is home to a wide range of freshwater fish species and some diadromous species. There are over 25 species able to be found in the Charles and some of the most common freshwater fish include the Redfin Pickerel, Largemouth Bass, Golden Shiner, Yellow Perch, a variety of sunfish (such as Bluegills, Redbreast Sunfish, and Pumpkinseeds), and some species of catfish (Yellow Bullhead, Brown Bullhead, White Bullhead). The diadromous fish (fish that spend parts of their lives in fresh and salt water) that can be found in

SECTION 20

#1732787831598

1848-441: Is known as surface hydrology and is a core element of environmental geography . A brook is a stream smaller than a creek, especially one that is fed by a spring or seep . It is usually small and easily forded . A brook is characterised by its shallowness. A creek ( / k r iː k / ) or crick ( / k r ɪ k / ): In hydrography, gut is a small creek; this is seen in proper names in eastern North America from

1932-506: Is popular with runners and bikers. Many runners gauge their distance and speed by keeping track of the mileage between the bridges along the route. After two decades of water quality improvement efforts spearheaded by the Environmental Protection Agency, on July 13, 2013, swimming for the general public was officially permitted for the first time in more than 50 years. Fishing from the banks or small craft

2016-425: Is sometimes termed a "young" or "immature" stream, and the later state a "mature" or "old" stream. Meanders are looping changes of direction of a stream caused by the erosion and deposition of bank materials. These are typically serpentine in form. Typically, over time the meanders gradually migrate downstream. If some resistant material slows or stops the downstream movement of a meander, a stream may erode through

2100-456: Is usually called a creek and marked on topographic maps with a solid blue line. There are five generic classifications: "Macroinvertebrate" refers to easily seen invertebrates , larger than 0.5 mm, found in stream and river bottoms. Macroinvertebrates are larval stages of most aquatic insects and their presence is a good indicator that the stream is perennial. Larvae of caddisflies , mayflies , stoneflies , and damselflies require

2184-626: The 9 + 1 ⁄ 2 -mile (15 km) tidal estuary from Watertown Dam to Boston Harbor. From 1816 to 1968, the U.S. Army operated a gun and ammunition storage and later production facility known as the Watertown Arsenal . While it was key to many of the nation's war efforts over its several decades in operation, not the least of which being the American Civil War and World War I , its location in Watertown so near

2268-737: The Atlantic Ocean . The indigenous Massachusett named it Quinobequin , meaning "meandering" or "meandering still water". The Charles River is fed by approximately 80 streams and several major aquifers as it flows 80 miles (129 km), starting at Teresa Road just north of Echo Lake ( 42°12′54″N 71°30′52″W  /  42.215°N 71.514444°W  / 42.215; -71.514444 ) in Hopkinton, passing through 23 cities and towns in eastern Massachusetts before emptying into Boston Harbor . Thirty-three lakes and ponds and 35 municipalities are entirely or partially part of

2352-698: The Charles River Museum of Industry and Waltham Common . The route extends upstream with a combination of paths and streets, to Auburndale , the Newton neighborhood where Norumbega Park is located. There are plans to extend the path upstream along the curving river to Needham, Dedham, and the West Roxbury neighborhood of Boston. Bike recreation opportunities continue to the east with North Point Park in Cambridge, and Nashua Street Park on

2436-756: The Charles River Speedway operated along part of the river. Today's Charles River basin between Boston and Cambridge is almost entirely a work of human design. Owen A. Galvin was appointed head of the Charles River Improvement Commission by Governor William E. Russell in 1891. Their work led to the design initiatives of noted landscape architects Charles Eliot and Arthur Shurcliff , both of whom had apprenticed with Frederick Law Olmsted and Guy Lowell . This designed landscape includes over 20 parks and natural areas along 19 miles (31 km) of shoreline, from

2520-725: The Environmental Protection Agency graded the river's 2017 bacterial water quality "A−". A study published in the Journal of the American Water Resources Association in April 2008 and completed by researchers at Northeastern University, found high concentrations of E. coli bacteria in the Charles River after a long period of no rain. Using a mathematical model , the researchers then determined that two major tributaries,

2604-785: The Fresh Pond Bikeway, and the Alewife Brook Parkway Path, also connects to the network of mixed-use trails to the northwest. Charles River The Charles River ( Massachusett : Quinobequin ), sometimes called the River Charles or simply the Charles , is an 80-mile-long (129 km) river in eastern Massachusetts . It flows northeast from Hopkinton to Boston along a highly meandering route, that doubles back on itself several times and travels through 23 cities and towns before reaching

Charles River Bike Path - Misplaced Pages Continue

2688-677: The Massachusetts Institute of Technology are located along the Charles River. Near its mouth, it forms the border between downtown Boston and Cambridge and Charlestown . The river opens into a broad basin and is lined by the parks of the Charles River Reservation . On the Charles River Esplanade stands the Hatch Shell , where concerts are given in summer evenings. The basin is especially known for its Independence Day celebration. The middle section of

2772-545: The Stony Brook and Muddy River , are the predominant sources of E. coli in the lower Charles River. Starting in 2007, the Charles River Swimming Club has organized an annual race for its members, but obtains a special permit and must monitor water quality and rainfall in the days leading up to the race. The "first public swim" in the Charles since the 1950s was conducted on July 13, 2013, by

2856-691: The Tombigbee River basin. Continuing in this vein, a component of the Mississippi River basin is the Ohio River basin, which in turn includes the Kentucky River basin, and so forth. Stream crossings are where streams are crossed by roads , pipelines , railways , or any other thing which might restrict the flow of the stream in ordinary or flood conditions. Any structure over or in a stream which results in limitations on

2940-713: The coastal plains around a lake or an ocean . They can also occur inland, on alluvial fans , or where a tributary stream bifurcates as it nears its confluence with a larger stream. Common terms for individual river distributaries in English-speaking countries are arm and channel . There are a number of regional names for a stream. A stream's source depends on the surrounding landscape and its function within larger river networks. While perennial and intermittent streams are typically supplied by smaller upstream waters and groundwater, headwater and ephemeral streams often derive most of their water from precipitation in

3024-480: The velocity of the stream. A perennial stream is one which flows continuously all year. Some perennial streams may only have continuous flow in segments of its stream bed year round during years of normal rainfall. Blue-line streams are perennial streams and are marked on topographic maps with a solid blue line. The word "perennial" from the 1640s, meaning "evergreen," is established in Latin perennis, keeping

3108-416: The water cycle , instruments in groundwater recharge , and corridors for fish and wildlife migration. The biological habitat in the immediate vicinity of a stream is called a riparian zone . Given the status of the ongoing Holocene extinction , streams play an important corridor role in connecting fragmented habitats and thus in conserving biodiversity . The study of streams and waterways in general

3192-602: The "barbarous names" for "English" ones. The Prince made many such changes, but only four survive today, one of which is the Charles River which Charles named for himself. The native name for the Charles River was Quinobequin , possibly meaning "meandering" in Massachusett from quinnuppe or "it turns." Other sources state this name was transferred from the Kennebec River in Maine to Cambridge by Prince Charles at

3276-599: The 1620s, Captain John Smith of Jamestown explored and mapped the coast of New England, originally naming the Charles River the Massachusetts River, which he derived from the Massachusett people living in the region, not from their actual name for the river, Quinobequin . When Smith presented his map to Prince Charles, future King Charles I , he suggested that the Prince should feel free to change any of

3360-712: The 1960s, and the program to clean up the Charles for good took shape in 1965 with the creation of the Charles River Watershed Association. In 1978, a new Charles River Dam was constructed downstream from the Science Museum site to keep salt water out of the basin. In 1995, the United States Environmental Protection Agency declared a goal of making the river swimmable by 2005. In 1996, Governor William Weld plunged, fully clothed, into

3444-839: The Boston side. There are discontinuities near North Station and the Zakim Bridge before the Boston Harborwalk continues on both sides of the harbor. The Somerville Community Path extension connects the Boston end of the Charles River Path to the network of mixed-use trails to the northwest. Sequential connections heading north starting at the Watertown Branch Rail Trail , the Watertown-Cambridge Greenway ,

Charles River Bike Path - Misplaced Pages Continue

3528-572: The Charles River drainage basin . Despite the river's length and relatively large drainage area (308 square miles; 798 km ), its source is only 26 miles (42 km) from its mouth, and the river drops only 350 feet (107 m) from source to sea. The Charles River watershed contains more than 8,000 acres (32 km ) of protected wetlands, referred to as Natural Valley Storage. These areas are important in preventing downstream flooding and providing natural habitats to native species. Harvard University , Brandeis University , Boston University , and

3612-659: The Charles River Basin. In the 1950s a highway, Storrow Drive , was built along the edge of the Esplanade to connect Charles Circle with Soldiers Field Road, and the Esplanade was enlarged on the water side of the new highway. The Inner Belt highway was proposed to cross the Charles River at the Boston University Bridge , but its construction was canceled in the 1970s. As sewage , industrial wastewater and urban runoff flowed freely into

3696-543: The Charles River Conservancy, Charles River Watershed Association (CRWA), Esplanade Association, and DCR. Both the annual race and the Conservancy event have been held in deep water with swimmers jumping in off a dock, to avoid the toxic sediments on the bottom of the river that still make beach swimming dangerous. Swimming without a permit is punishable by a fine up to $ 250. The Charles River

3780-474: The Charles River is often at its worst after a large rainfall because of pollutants carried by runoff, and sewage overflows. For 2011, the EPA reported that the Charles met state bacterial standards for boating and swimming 96% and 89% of the time on dry days, and 74% and 35% of the time on wet days, respectively. Overall boatability and swimability of 82% and 54% in 2011 compared with 39% and 19% in 1995. In June 2018,

3864-578: The Charles are mostly anadromous species (fish that migrate from sea to freshwater to spawn). These include the Alewife Herring, American Shad, White Perch, and Striped Bass. The only catadromous species (fish that migrate from freshwater to sea to spawn) in the Charles is the American Eel. With the many initiatives to improve the health of the river in the years since the formation of the CRWA,

3948-401: The Charles did great environmental harm. The arsenal was declared a Super Fund site, and after its closure by the government it had to be cleaned at significant expense before it could be safely used again for other purposes. Likewise, the many factories and mills along the banks of the Charles supported a buoyant economy in their time but left a legacy of massive pollution. For several years,

4032-741: The Charles near the Museum of Science and river tour boat excursions depart from a lagoon near the museum. In early June, the Hong Kong Boston Dragon Boat Festival is held in Cambridge , near the Weeks Footbridge . The Charles River Bike Path runs 23 miles (37 km) along the banks of the Charles, starting at the Museum of Science and passing the campuses of MIT, Harvard and Boston University. The path

4116-848: The Lower Basin, Union Boat Club. The Lower Basin between the Longfellow and Harvard (Massachusetts Avenue) bridges has the sailing docks of Community Boating , the Harvard University Sailing Center, and the MIT Sailing Pavilion. Sailboat, kayak, and paddleboard rentals are available at the Boston University Sailing Pavilion. Charles River Canoe and Kayak has four locations along the Charles, renting kayaks, canoes, and paddleboards. Duck Boats regularly enter

4200-566: The MIT Sea Grant College Program and the Charles River Alliance of Boaters (CRAB). Online and hardcopy charts are available as a public service. The river is busy, apart from the winter months, with rowing , sculling , canoeing , kayaking , paddleboarding , dragonboating , and sailing , both recreational and competitive. Most of the watercraft activity occurs from the Museum of Science to

4284-476: The Massachusetts Division of Marine Fisheries and the U.S. Fish and Wildlife Service , targeted American Shad as a species to revive in the river's ecosystem. In the years from 2006 to 2011, the river was stocked with millions of shad fry. Research showed that these shad were in fact returning to the river to spawn, a testament to the improved health of the river. Stream A stream is

SECTION 50

#1732787831598

4368-840: The Mid-Atlantic states (for instance, The Gut in Pennsylvania, Ash Gut in Delaware, and other streams) down into the Caribbean (for instance, Guinea Gut , Fish Bay Gut , Cob Gut , Battery Gut and other rivers and streams in the United States Virgin Islands , in Jamaica (Sandy Gut, Bens Gut River, White Gut River), and in many streams and creeks of the Dutch Caribbean ). A river

4452-650: The New Dam at the Charlestown Bridge to the dam near Watertown Square. Eliot first envisioned today's river design in the 1890s, an important model being the layout of the Alster basin in Hamburg , but major construction began only after Eliot's death with the damming of the river's mouth at today's Boston Museum of Science , an effort led by James Jackson Storrow . The new dam, completed in 1910, stabilized

4536-533: The atmosphere either by evaporation from soil and water bodies, or by plant evapotranspiration. By infiltration some of the water sinks into the earth and becomes groundwater, much of which eventually enters streams. Most precipitated water is partially bottled up by evaporation or freezing in snow fields and glaciers. The majority of the water flows as a runoff from the ground; the proportion of this varies depending on several factors, such as climate, temperature, vegetation, types of rock, and relief. This runoff begins as

4620-525: The base level of erosion throughout its course. If this base level is low, then the stream will rapidly cut through underlying strata and have a steep gradient, and if the base level is relatively high, then the stream will form a flood plain and meander. Typically, streams are said to have a particular elevation profile , beginning with steep gradients, no flood plain, and little shifting of channels, eventually evolving into streams with low gradients, wide flood plains, and extensive meanders. The initial stage

4704-597: The base stage of erosion. The scientists have offered a way based on data to define the origin of the lake. A classified sample was the one measured by the Chinese researchers from the University of Chinese Academy of Sciences. As an essential symbol of the river formation environment, the river source needs an objective and straightforward and effective method of judging . A calculation model of river source catchment area based on critical support flow (CSD) proposed, and

4788-401: The center of Watertown , above which is a dam. These 17 miles (27 km) see motorboat traffic from two marinas and a boat ramp near Watertown, as well as two marinas downstream and boats entering from Boston Harbor through an old lock next to the Museum of Science. A canoe and kayak ADA-accessible launch at Magazine Beach in Cambridge opened 23 September 2019. The Charles is renowned as

4872-474: The fish. Long before European settlers named and shaped the Charles, Native Americans living in New England made the river a central part of their lives. At the time of European colonization in the early 1600s, settlements of Massachusett people were present along the river at Nonantum in current-day Newton and Pigsgusset in current-day Watertown . Prior to the arrival of Puritan colonists in

4956-707: The flow is reduced to a trickle or less. Typically torrents have Apennine rather than Alpine sources, and in the summer they are fed by little precipitation and no melting snow. In this case the maximum discharge will be during the spring and autumn. An intermittent stream can also be called a winterbourne in Britain, a wadi in the Arabic -speaking world or torrente or rambla (this last one from arabic origin) in Spain and Latin America. In Australia, an intermittent stream

5040-447: The form of rain and snow. Most of this precipitated water re-enters the atmosphere by evaporation from soil and water bodies, or by the evapotranspiration of plants. Some of the water proceeds to sink into the earth by infiltration and becomes groundwater, much of which eventually enters streams. Some precipitated water is temporarily locked up in snow fields and glaciers , to be released later by evaporation or melting. The rest of

5124-407: The health and variety of fish in the river have greatly improved. One example of this is the reintroduction of American Shad into the Charles. American Shad used to be one of the most common species in the river until the 1800s when population numbers decreased because of new dams and poor water quality. With improved water quality and partial dam breaches created in modern times, the CRWA, along with

SECTION 60

#1732787831598

5208-532: The lake has significant feeder rivers. The Kagera River, which flows into Lake Victoria near Bukoba's Tanzanian town , is the longest feeder, though sources do not agree on which is the Kagera's longest tributary and therefore the Nile's most remote source itself. To qualify as a stream, a body of water must be either recurring or perennial. Recurring (intermittent) streams have water in the channel for at least part of

5292-443: The little long pond"), and Quinnipiac River ("long pond") in present-day Massachusetts , Connecticut , and New Hampshire . As native populations were driven out by European settlers, the Charles River became an early center for hydropower and manufacturing in North America. Although in portions of its length, the Charles drops slowly in elevation and has relatively little current, early settlers in Dedham, Massachusetts , found

5376-422: The mainly easterly-draining Atlantic Ocean and Arctic Ocean basins from the largely westerly-flowing Pacific Ocean basin. The Atlantic Ocean basin, however, may be further subdivided into the Atlantic Ocean and Gulf of Mexico drainages. (This delineation is termed the Eastern Continental Divide .) Similarly, the Gulf of Mexico basin may be divided into the Mississippi River basin and several smaller basins, such as

5460-412: The meaning as "everlasting all year round," per "over" plus annus "year." This has been proved since the 1670s by the "living years" in the sense of botany. The metaphorical sense of "enduring, eternal" originates from 1750. They are related to "perennial." See biennial for shifts in vowels. Perennial streams have one or more of these characteristics: Absence of such characteristics supports classifying

5544-453: The neck between two legs of a meander to become temporarily straighter, leaving behind an arc-shaped body of water termed an oxbow lake or bayou . A flood may also cause a meander to be cut through in this way. The stream load is defined as the solid matter carried by a stream. Streams can carry sediment, or alluvium. The amount of load it can carry (capacity) as well as the largest object it can carry (competence) are both dependent on

5628-421: The origin of the Nile River is the confluence of the White Nile and the Blue Nile, but the source of the whole river system is in its upper reaches. If there is no specific designation, "length of the Nile" refers to the "river length of the Nile system", rather than to the length of the Nile river from the point where it is formed by a confluence of tributaries. The Nile's source is often cited as Lake Victoria, but

5712-453: The path westward from Watertown Square to Norumbega Park in Newton was completed. The path continues along the north side of the river from Watertown Square to Bridge Street, there crossing back from Watertown to Newton. This segment was completed in 1997. The riverwalk then continues along the south bank, crossing back to the north bank at the Blue Heron Bridge, built 2004 just for the path, and continuing to Moody Street in Waltham, near

5796-422: The path will be turned into a river boardwalk as part of the straightening of the Massachusetts Turnpike . The portion between the Longfellow Bridge and Boston University Boathouse on the Cambridge side was rebuilt in 2015-16. In 2019, DCR started soliciting public comments for a planned rebuild on the Cambridge side from the Boston University Bridge to the Eliot Bridge . In 2004, a $ 9M master plan to extend

5880-417: The relationship between CSA and CSD with a minimum catchment area established. Using the model for comparison in two basins in Tibet (Helongqu and Niyang River White Water), the results show that the critical support flow (Qc) of the housing dragon song is 0.0028 m /s. At the same time, the white water curvature is 0.0085 m /s. Besides, the critical support flow can vary with hydrologic climate conditions, and

5964-416: The river between the Watertown Dam and Wellesley is partially protected by the properties of the Upper Charles River Reservation and other state parks, including the Hemlock Gorge Reservation , Cutler Park , and the Elm Bank Reservation . A detailed depth chart of the lower basin of the Charles River, from near the Watertown Dam to the New Charles River Dam , has been created by a partnership between

6048-494: The river from the surrounding city, the Charles River became well known for its high level of pollutants , gaining such notoriety that by 1955, Bernard DeVoto wrote in Harper's Magazine that the Charles was "foul and noisome, polluted by offal and industrious wastes, scummy with oil, unlikely to be mistaken for water." Fish kills and submerged vehicles were a common sight, along with toxic chemical plumes that colored parts of

6132-456: The river pink and orange. The Standells sang about the sorry state of the Charles in their 1965 song " Dirty Water ". Once popular with swimmers, awareness of the river's high pollution levels forced the state to shut down several popular swimming areas, including Cambridge's Magazine Beach and Gerry Landing public beaches. Efforts to clean up the river and restore it to a state where swimming and fishing would be acceptable began as early as

6216-660: The river to prove his commitment to cleaning up the river. On November 12, 2004, Christopher Swain became the first person to swim the Charles River's entire length, in an effort to raise public awareness of the river's environmental health. In July 2007, the river hosted the Charles River Masters Swim Race, the first sanctioned race in the Charles in over five decades. A combination of public and private initiatives helped drastically lower levels of pollutants by focusing on eliminating combined sewer overflows and stormwater runoff . Since Weld's stunt,

6300-556: The river within the Charles River Reservation . From the Museum of Science on the Charles River Dam Bridge , they run on sidewalk or striped asphalt path to Watertown Square (Galen Street/ Route 16 bridge), a loop of 17.1 miles (27.5 km). The paths run along the edge of Cambridge and Watertown on the north; and the West End, Back Bay, and Allston-Brighton neighborhoods of Boston on the south side. Part of

6384-546: The river's condition has improved dramatically, although it was not deemed entirely swimmable by 2005. The Conservation Law Foundation opposes the permit given to Mirant for the Veolia Energy North America Kendall Cogeneration Station , an electricity plant near Kendall Square , charging that the water it releases causes blooms of hazardous microorganisms because of its warm temperature. The water quality of

6468-425: The side of the stream or within the floodplain will be a good indicator of persistent water regime. A perennial stream can be identified 48 hours after a storm. Direct storm runoff usually has ceased at this point. If a stream is still flowing and contributing inflow is not observed above the channel, the observed water is likely baseflow. Another perennial stream indication is an abundance of red rust material in

6552-579: The time he renamed this river in his name. Still another explanation is that Quinobequin was a descriptive term for any long body of water for Eastern Algonquin peoples, which European explorers and settlers interpreted as a local proper name. Examples include the Kennebec River ("long water place") and Kennebunk in Maine , the Quinebaug River ("long pond"), Quinapoxet River ("at

6636-655: The vital support flow Qc in wet areas (white water) is larger than in semi-arid regions (heap slot). The proposed critical support flow (CSD) concept and model method can be used to determine the hydrographic indicators of river sources in complex geographical areas, and it can also reflect the impact of hydrologic climate change on river recharge in different regions. The source of a river or stream (its point of origin) can consist of lakes, swamps, springs, or glaciers. A typical river has several tributaries; each of these may be made up of several other smaller tributaries, so that together this stream and all its tributaries are called

6720-512: The water flows off the land as runoff, the proportion of which varies according to many factors, such as wind, humidity, vegetation, rock types, and relief. This runoff starts as a thin film called sheet wash, combined with a network of tiny rills, together constituting sheet runoff; when this water is concentrated in a channel, a stream has its birth. Some creeks may start from ponds or lakes. The streams typically derive most of their water from rain and snow precipitation. Most of this water re-enters

6804-515: The water level from Boston to Watertown, eliminating the existing mud flats, and a narrow embankment was built between Leverett Circle and Charlesgate. After Storrow's death, his widow Mrs. James Jackson Storrow donated $ 1 million toward the creation of a more generously landscaped park along the Esplanade; it was dedicated in 1936 as the Storrow Memorial Embankment. This also enabled the construction of many public docks in

6888-521: The year and is marked on topographic maps with a line of blue dashes and dots. A wash , desert wash, or arroyo is normally a dry streambed in the deserts of the American Southwest , which flows after sufficient rainfall. In Italy, an intermittent stream is termed a torrent ( Italian : torrente ). In full flood the stream may or may not be "torrential" in the dramatic sense of the word, but there will be one or more seasons in which

6972-402: The year. A stream of the first order is a stream which does not have any other recurring or perennial stream feeding into it. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream. Streams of lower order joining a higher order stream do not change the order of the higher stream. The gradient of

7056-422: Was the site of the first fully integrated textile factory in America, built by Francis Cabot Lowell in 1814, and by the 19th century the Charles River was one of the most industrialized areas in the United States. Its hydropower soon fueled many mills and factories. By the century's end, 20 dams had been built across the river, mostly to generate power for industry. An 1875 government report listed 43 mills along

#597402