- North American Beaver
Castor canadensis Conservation status Scientific classification Kingdom: Animalia Phylum: Chordata Class: Mammalia Order: Rodentia Family: Castoridae Genus: Castor Species: C. canadensis Binomial name Castor canadensis
- C. c. acadicus Bailey
- C. c. baileyi Nelson
- C. c. belugae Taylor
Cook Inlet beaver
- C. c. caecator Bangs
- C. c. canadensis Kuhl
- C. c. concisor
- C. c. carolinensis Rhoads
- C. c. duchesnei
- C. c. frondator Mearns
- C. c. idoneus
- C. c. labradorensis
- C. c. leucodonta Gray
- C. c. mexicanus Bailey
Rio Grande beaver
- C. c. michiganensis Bailey
- C. c. missouriensis Bailey
Missouri River beaver
- C. c. pacificus Rhoads
- C. c. pallidus
- C. c. phaeus Heller
- C. c. rostralis
- C. c. repentinus Goldman
- C. c. sagittatus
- C. c. shastensis Taylor
- C. c. subauratus
California Golden beaver
- C. c. taylori Davis
- C. c. texensis Bailey
The North American Beaver (Castor canadensis) is the only species of beaver in the Americas, native to North America and introduced to South America. In the United States and Canada, where no other species of beaver occurs, it is usually simply referred to as "beaver". Its other vernacular names, including American beaver and Canadian beaver, distinguish this species from the one other extant beaver, Castor fiber, native to Eurasia. ("Canadian beaver" also refers to the subspecies Castor canadensis canadensis.)
- 1 Description
- 2 Behaviour
- 3 Reproduction
- 4 Subspecies
- 5 Differences from European beaver
- 6 Ecology
- 7 Urban beavers
- 8 As introduced non-native species
- 9 As food
- 10 Symbolism
- 11 References
- 12 Further reading
- 13 External links
This beaver is the largest rodent in North America and the third largest rodent in the world, after the South American capybara and the Eurasian beaver. Adults usually weigh 15 to 35 kg (33 to 77 lb), with 20 kg (44 lb) a typical mass, and measure around 1 m (3.3 ft) in total body length. Very old individuals can weigh as much as 45 kg (99 lb).
Like the capybara, the beaver is semi-aquatic. The beaver has many traits suited to this lifestyle. It has a large flat paddle-shaped tail and large, webbed hind feet reminiscent of a human diver's swimfins. The unwebbed front paws are smaller, with claws. The eyes are covered by a nictitating membrane which allows the beaver to see underwater. The nostrils and ears are sealed while submerged. A thick layer of fat under its skin insulates the beaver from its cold water environment.
The beaver's fur consists of long, coarse outer hairs and short, fine inner hairs (see Double coat). The fur has a range of colours but usually is dark brown. Scent glands near the genitals secrete an oily substance known as castoreum, which the beaver uses to waterproof its fur.
Before their near extirpation by trapping in North America, beaver were practically ubiquitous and lived from the arctic tundra to the deserts of northern Mexico, and from the Atlantic to the Pacific Oceans. Explorer David Thompson, after crossing much of North America in 1784, stated that "this Continent...from the Atlantic to the Pacific Ocean, may be said to have been in the possession of two distinct races of Beings, Man and the Beaver."
Beavers are mainly active at night. They are excellent swimmers but are more vulnerable on land and tend to remain in the water as much as possible. They are able to remain submerged for up to 15 minutes. They use their flat, scaly tail both to signal danger by slapping the surface of the water and as a location for fat storage.
They construct their homes, or "lodges," out of sticks, twigs, and mud in lakes, streams, and tidal river deltas. These lodges may be surrounded by water, or touching land, including burrows dug into river banks. They are well known for building dams across streams and constructing their lodge in the artificial pond which forms. When building in a pond, the beavers first make a pile of sticks and then eat out one or more underwater entrances and two platforms above the water surface inside the pile. The first is used for drying off. Towards winter, the lodge is often plastered with mud which when it freezes has the consistency of concrete. A small air hole is left in the top of the lodge.
The dam is constructed using logs from trees the beavers cut down, as well as rocks, grass and mud. The inner bark, twigs, shoots and leaves of such trees are also an important part of the beaver's diet. The trees are cut down using their strong incisor teeth. Their front paws are used for digging and carrying and placing materials. Some researchers have shown that the sound of running water dictates when and where a beaver builds its dam. Besides providing a safe home for the beaver, beaver ponds also provide habitat for waterfowl, fish, and other aquatic animals. Their dams help reduce soil erosion and can help reduce flooding. However, beaver dams are not permanent and depend on the beavers' continued presence for their maintenance. Beavers generally concentrate on building and repairing dams in the fall in preparation for the coming winter. In northern areas they often don't repair breaches in the dam made by otters, and sometimes breach the dam themselves and lower the water level in the pond in order to create more breathing space under the ice or get easier access to trees below the dam. In a 1988 study in Alberta, Canada, no beavers repaired "sites of water loss" during the winter. Of 178 sites of water loss, beavers repaired 78 when water was opened, and did not repair 68. The rest were partially repaired. .
Beavers are most famous, and infamous, for their dam-building. They maintain their pond-habitat by reacting quickly to the sound of running water, and damming it up with tree branches and mud. Early ecologists believed that this dam-building was an amazing feat of architectural planning, indicative of the beaver's high intellect. This theory was questioned when a recording of running water was played in a field near a beaver pond. Despite the fact that it was on dry land, the beaver covered the tape player with branches and mud. The largest beaver dam is 2,790 ft (850 m) in length—more than half a mile long—and was discovered via satellite imagery in 2007. It is located on the southern edge of Wood Buffalo National Park in northern Alberta and is twice the width of the Hoover Dam which spans 1,244 ft (379 m).
Normally, the purpose of the dam is to provide water around their lodges that is deep enough that it does not freeze solid in winter. The dams also flood areas of surrounding forest, giving the beaver safe access to an important food supply, which is the leaves, buds, and inner bark of growing trees. They prefer aspen and poplar, but will also take birch, maple, willow, alder, black cherry, red oak, beech, ash, hornbeam and occasionally pine and spruce. They will also eat cattails, water lilies and other aquatic vegetation, especially in the early spring (and contrary to widespread belief, they do not eat fish). In areas where their pond freezes over, beavers collect food in late fall in the form of tree branches, storing them underwater (usually by sticking the sharp chewed base of the branches into the mud on the pond bottom), where they can be accessed through the winter. Often the pile of food branches projects above the pond and collects snow. This insulates the water below it and keeps the pond open at that location.
Beavers usually mate for life. The young beaver "kits" typically remain with their parents for up to two years.
Common natural predators include gray wolves, coyotes, and mountain lions. Less significant predators include bears, which can dig into a lodge, wolverines, fox, Canadian lynx, bobcats, and alligators. Despite repeated claims there is no evidence that river otters are predators of beavers.
North American beaver have one litter per year, coming into estrus for only 12 to 24 hours, between late December and May but peaking in January. Unlike most other rodents, beaver pairs are monogamous, staying together for multiple breeding seasons. Gestation averages 128 days and they average three kits per litter with a range of two to six kits. Most beaver do not reproduce until they are three years of age, but about 20% of two year old females reproduce.
The first fossil records of beaver are 10 to 12 million years old in Germany, and they are thought to have migrated to North America across the Bering Strait. The oldest fossil record of beaver in North America are of two beaver teeth in Dayville, Oregon and are 7 million years old.
There are 25 subspecies of beaver in North America, but different subspecies have been reintroduced to areas with previously geographically isolated subspecies, following population decline or extirpation of the indigenous subspecies. This has led to very substantial mixing of the subspecies gene pools, and some subspecies may have disappeared entirely.
The most widespread subspecies are C. c. acadicus (New England beaver), C. c. canadensis (Canadian beaver), C. c. carolinensis (Carolina beaver), and C. c. missouriensis (Missouri River beaver). The Canadian beaver originally inhabited almost all of the forested area of Canada, and because of its more valued fur, was often selected for reintroductions elsewhere. The Carolina beaver is found in the southeastern United States, the Missouri River beaver, as its name suggests, is found in the Missouri River and its tributaries, and C. c. acadicus is found throughout the New England area in the northeastern United States.
Differences from European beaver
Although superficially similar to the European beaver (Castor fiber), there are several important differences between the two species. North American beavers tend to be smaller, with smaller, more rounded heads, shorter, wider muzzles, thicker, longer and darker underfur, wider, more oval-shaped tails and have longer shin bones, allowing them a greater range of bipedal locomotion than the European species. North American beavers have shorter nasal bones than their European cousins, with the widest point being at the middle of the snout for the former, and in the tip for the latter. The nasal opening for the North American species is square, unlike that of the European race which is triangular. The foramen magnum is triangular in the North American beaver, and rounded in the European. The anal glands of the North American beaver are smaller and thick-walled with a small internal volume compared to that of the European species. Finally, the guard hairs of the North American beaver have a shorter hollow medulla at their tips. Fur colour is also different. Overall, 50% of North American beavers have pale brown fur, 25% are reddish brown, one fifth are brown and 6% are blackish, while in European beavers 66% have pale brown or beige fur, 20% have reddish brown, nearly 8% are brown and only 4% have blackish coats.
The two species are not genetically compatible. North American beavers have 40 chromosomes, while European beavers have 48. Also, more than 27 attempts were made in Russia to hybridize the two species, with one breeding between a male North American beaver and a female European resulting in one stillborn kit. These factors make interspecific breeding unlikely in areas where the two species' ranges overlap.
The beaver was trapped out and almost extirpated in North America as its fur and castoreum were highly sought after. The beaver furs were used to make clothing and beaver hats. In the United States extensive trapping began in the early 17th century with more than 10,000 beaver per year taken for the fur trade in Connecticut and Massachusetts between 1620 and 1630. From 1630 to 1640, approximately 80,000 beaver were taken annually from the Hudson River and western New York. As eastern beaver populations were depleted, French and American trappers pushed west. In fact, much of the westward expansion and exploration of North America was driven by the quest for this animal's fur. Before the 1849 California Gold Rush, there was an earlier 19th century California Fur Rush which drove the earliest American settlement in that State. During the approximately 30 years (1806–1838) of the era of the Mountain Man, the West from Missouri to California and from Canada to Mexico was thoroughly explored and the beaver was brought to the brink of extinction.
With protection in the late 19th and early 20th centuries the current beaver population has rebounded to an estimated 10 to 15 million; however this is still a fraction of the originally estimated 100 to 200 million North American beaver before the days of the fur trade.
These animals are considered pests in some parts of their range because their dams can cause flooding in nearby areas. Because they are persistent in repairing any damage to the dam, they were historically relocated or exterminated. However, non-lethal methods of containing beaver-related flooding have been developed. One such flow device has been utilized by both the Canadian and U.S. governments, called "Beaver Deceivers," or levelers, invented and pioneered by wildlife biologist, Skip Lisle.
The beaver is a keystone species, increasing biodiversity in its territory through creation of beaver ponds and wetlands. As wetlands are formed and riparian habitats enlarged, aquatic plants colonize newly available watery habitat. Insect, invertebrate, fish, mammal, and bird diversity are also expanded.
Effects on stream flows and water quality
Beaver ponds increase stream flows in seasonally dry streams by storing run-off in the rainy season, which raises groundwater tables via percolation from beaver ponds. In a recent study using 12 serial aerial photo mosaics from 1948 to 2002, the impact of the return of beaver on open water area in east-central Alberta, Canada found that the mammals were associated with a 9-fold increase in open water area. Beaver returned to the area in 1954 after a long absence since their extirpation by the fur trade in the nineteenth century. Even during drought years, where beaver were present, there was 60 per cent more open water than those same areas during previous drought periods when beaver were absent. The authors concluded that beaver have a dramatic influence on the creation and maintenance of wetlands even during extreme drought.
From streams from the Maryland coastal plain in the east to Lake Tahoe in the west, beaver ponds have been shown to remove sediment and pollutants including total suspended solids, total nitrogen, phosphates, carbon and silicates, improving stream water quality. In addition, fecal coliform and streptococci bacteria excreted into streams by grazing cattle are reduced by beaver ponds, where slowing currents lead to settling of the bacteria in bottom sediments.
The term "beaver fever" is a misnomer coined by the American press in the 1970s, following findings that the parasite Giardia lamblia, which causes Giardiasis, is carried by beavers. However, further research has shown that the many animals and birds carry this parasite, and the major source of water contamination is by other humans. Recent concerns point to domestic animals as a significant vector of giardia with young calves in dairy herds testing as high as 100% positive for giardia. In addition, fecal coliform and streptococci bacteria excreted into streams by grazing cattle have been shown to be reduced by beaver ponds, where the bacteria are trapped in bottom sediments. In fact, New Zealand has giardia outbreaks but no beaver, whereas Norway has plenty of beaver but had no giardia outbreaks until recently (in the most populous (by humans) south of the country.
Effects on bird diversity
Trumpeter swans (Cygnus buccinator) and Canada geese (Branta canadensis) often depend on beaver lodges as nesting sites. Canada's small trumpeter swan population was observed not to nest on large lakes, preferring instead to nest on the smaller lakes and ponds associated with beaver activity.
Beaver may benefit the birds frequenting their ponds in several additional ways. Removal of some pondside trees by beavers would increase the density and height of the grass–forb–shrub layer, which enhances waterfowl nesting cover adjacent to ponds. Both forest gaps where trees had been felled by beaver and a "gradual edge" described as a complex transition from pond to forest with intermixed grasses, forbs, saplings, and shrubs are strongly associated with greater migratory bird species richness and abundance. Coppicing of waterside willows and cottonwoods by beavers leads to dense shoot production which provides important cover for birds and the insects they feed on.
As trees are drowned by rising beaver impoundments they become ideal nesting sites for woodpeckers, who carve cavities that attract many other bird species including flycatchers (Empidonax spp.), tree swallows (Tachycineta bicolor), tits (Paridae spp.), wood ducks (Aix sponsa), goldeneyes (Bucephala spp.), mergansers (Mergus spp.), owls (Titonidae, Strigidae) and American kestrels (Falco sparverius). Piscivores, including herons (Ardea spp.), grebes (Podicipedidae), cormorants (Phalacrocorax ssp.), American bitterns (Botaurus lentiginosa), great egret (Ardea alba), snowy egret (Egretta thula), mergansers and belted kingfishers (Megaceryle alcyon), utilize beaver ponds for fishing. Hooded mergansers (Lophodytes cucullatus), green heron (Butorides virescens), great blue heron (Ardea herodias) and belted kingfisher occurred more frequently in New York wetlands where beaver were active than at sites with no beaver activity.
Effects on trout and salmon
Beaver ponds have been shown to have a beneficial effect on trout and salmon populations, in fact many authors believe that the decline of salmonid fishes is related to the decline in beaver populations. Research in the Stillaguamish River basin in Washington state, found that extensive loss of beaver ponds resulted in an 89% reduction in coho salmon (Oncorhynchus kisutch) smolt summer production and an almost equally detrimental 86% reduction in critical winter habitat carrying capacity. Swales and Leving had previously shown on the Coldwater River in British Columbia that off-channel beaver ponds were preferentially populated by coho salmon over other salmonids and provided overwintering protection, protection from high summer snowmelt flows and summer coho rearing habitat. The presence of beaver dams has also been shown to either increase the number of fish, their size, or both, in a study of brook trout (Salvelinus fontinalis), rainbow trout (Oncorhynchus mykiss) and brown trout (Salmo trutta) in Sagehen Creek, which flows into the Little Truckee River at an altitude of 5,800 feet in the northern Sierra Nevada. These findings are consistent with a study of small streams in Sweden, that found that brown trout were larger in beaver ponds compared with those in riffle sections, and that beaver ponds provide habitat for larger trout in small streams during periods of drought. Similarly, brook trout, coho salmon and sockeye salmon (Oncorhynchus nerka) were significantly larger in beaver ponds than those in un-impounded stream sections in Colorado and Alaska. Contrary to popular myth, most beaver dams do not pose barriers to trout and salmon migration, although they may be restricted seasonally during periods of low stream flows. Rainbow, brown and brook trout have been shown to cross as many as 14 consecutive beaver dams. Both adults and juveniles of coho salmon, steelhead trout, sea run cutthroat (Oncorhyncus clarki clarki), Dolly Varden trout (Salvelinus malma malma), and sockeye salmon are able to cross beaver dams. In southeast Alaska, coho jumped dams as high as 2 meters, were found above all beaver dams and had their highest densities in streams with beaver. In Oregon coastal streams, beaver dams are ephemeral and almost all wash out in high winter flows only to be re-built every summer. Migration of adult Atlantic salmon (Salmo salar) may be limited by beaver dams but the presence of juveniles upstream from the dams suggests that the dams are penetrated by parr. Downstream migration of Atlantic salmon smolts was similarly unaffected by beaver dams, even in periods of low flows. Two year old Atlantic salmon parr in beaver ponds in eastern Canada showed faster summer growth in length and mass and were in better condition than parr upstream or downstream from the pond. The importance of winter habitat to salmonids afforded by beaver ponds may be especially important (and underappreciated) in streams without deep pools or where ice cover makes contact with the bottom of shallow streams. Enos Mills wrote in 1913, "One dry winter the stream...ran low and froze to the bottom, and the only trout in it that survived were those in the deep holes of beaver ponds." Cutthroat trout (Oncorhynchus clarki) and bull trout (Salvelinus confluentus) were noted to overwinter in Montana beaver ponds, brook trout congregated in winter in New Brunswick and Wyoming beaver ponds, and coho salmon in Oregon beaver ponds. In 2011 a meta-analysis of studies of beaver impacts on salmonids found that beaver were a net benefit to salmon and trout populations primarily by improving habitat (building ponds) both for rearing and overwintering and that this conclusion was based over half the time on scientific data. In contrast, the most often cited negative impact of beavers on fishes were barriers to migration although that conclusion was based on scientific data only 29% of the time. They also found that when beaver dams do present barriers that these are generally short-lived, as the dams are overtopped or blown out by storm surges.
Efforts to restore salmonid habitat in the western United States have focused primarily on establishing large woody debris in streams to slow flows and create pools for young salmonids. However research in Washington state found that the average summer smolt production per beaver dam ranges from 527 to 1,174 fish, whereas the summer smolt production from a pool formed by instream large woody debris is about 6–15 individuals, suggesting that re-establishment of beaver populations would be 80 times more effective.
Recently, beaver have been discovered living in brackish water in estuarine tidal marshes, where Chinook salmon (Oncorhynchus tshawytscha) densities were five times higher in beaver ponds than in neighboring areas.
Effects on riparian trees and vegetation
Conventional wisdom has held that beaver girdle and fell trees and that they diminish riparian trees and vegetation, but the opposite appears to be true when studies are conducted longer-term. In 1987, Beier reported that beaver had caused local extinction of Quaking aspen (Populus tremuloides) and Black cottonwood (Populus trichocarpa) on 4-5% of stream reaches on the lower Truckee River in the Sierra Nevada mountains, however Willow (Salix spp.) responded by re-growing vigorously in most reaches. He further speculated that without control of beaver populations that aspen and cottonwood could go extinct on the Truckee River. However, not only have aspen and cottonwood survived ongoing beaver colonization but a recent study of ten Sierra Nevada streams in the Lake Tahoe basin utilizing aerial multispectral videography has shown that deciduous, thick herbaceous, and thin herbaceous vegetation are more highly concentrated near beaver dams, whereas coniferous trees are decreased. These findings are consistent with those of Pollock, who reported that in Bridge Creek, a stream in semi-arid eastern Oregon, the width of riparian vegetation on stream banks was increased several-fold as beaver dams watered previously dry terraces adjacent to the stream. In a second study of riparian vegetation based on observations of Bridge Creek over a 17 year time period, although portions of the study reach were periodically abandoned by beaver following heavy utilization of streamside vegetation, within a few years dense stands of woody plants of greater diversity occupied a larger portion of the floodplain. Although black cottonwood and thinleaf alder did not generally re-sprout after beaver cutting, they frequently grew from seeds landing on freshly exposed alluvial deposits secondary to beaver activity. Therefore, beaver appear to increase riparian vegetation given enough years to aggrade sediments and pond heights sufficiently to create widened, well-watered riparian zones, especially in areas of low summer rainfall.
The surface of beaver ponds are typically at or near bank-full, so even small increases in stream flows cause the pond to overflow its banks. Thus, high stream flows spread water and nutrients to beyond the stream banks to wide riparian zones when beaver dams are present.
Beavers and stream restoration
In the 1930s, the U.S. Government put 600 beaver to work alongside the Civilian Conservation Corps in projects to stop soil erosion by streams in Oregon, Washington, Wyoming, and Utah. At the time it was estimated that each beaver, whose initial cost was about $5, completed work worth $300.
In a pilot study in Washington state, the Lands Council is reintroducing beavers to evaluate their projections that if 10,000 miles of suitable habitat were repopulated then 650 trillion gallons of spring runoff would be held back for release in the arid fall season. This project was developed in response to a 2003 Washington Department of Ecology proposal to spend as much as ten billion dollars on construction of several dams on Columbia River tributaries to retain storm season runoff. The State of Utah published a Beaver Management Plan which includes re-establishing beavers in ten streams per year for the purpose of watershed restoration each year from 2010 through 2020.
After 200 years, a beaver returned to New York City in 2007, making its home along the Bronx River, having spent time living at the Bronx Zoo as well as the Botanical Gardens. Beavers have not lived in New York City since the early 19th century when trappers extirpated them completely from the state. The return of "Jose", named after Representative Jose Serrano from the Bronx, has been seen as evidence that efforts to restore the river have been successful. In the summer of 2010 a second beaver joined Jose, doubling the beaver population in New York City. Beaver were once important to the city's economy and a pair of beavers appears on the city's official seal and flag.
In Chicago, several beavers have returned and made a home near the Lincoln Park's North Pond. The "Lincoln Park Beaver" has not been as well received by the Chicago Park District and the Lincoln Park Conservancy, which was concerned over damage to trees in the area. In March 2009, they hired an exterminator to remove a beaver family using live traps, and accidentally killed the mother when she got caught in a snare and drowned. Relocation costs $4,000-$4,500 per animal. Scott Garrow, District Wildlife Biologist with the Illinois Department of Natural Resources, opined that relocating the beavers may be "a waste of time", as there are records of beaver recolonizing North Pond in Lincoln Park in 1994, 2003, 2004, 2008 and 2009. As of fall 2009 a new beaver lodge has appeared on North Pond's northwest bank.
Outside San Francisco, in downtown Martinez, California, a male and female beaver arrived in Alhambra Creek in 2006. The Martinez beavers built a dam 30 feet wide and at one time 6 feet high, and chewed through half the willows and other creekside landscaping the city planted as part of its $9.7 million 1999 flood-improvement project. When the City Council wanted to remove the beavers because of fears of flooding, local residents organized to protect them, forming an organization called "Worth a Dam". Resolution included installation of a flow device through the beaver dam so that the pond's water level could not become excessive. Now protected, the beaver have transformed Alhambra Creek from a trickle into multiple dams and beaver ponds, which in turn, lead to the return of steelhead trout and river otter in 2008, and mink in 2009. The Martinez beavers probably originated from the Sacramento-San Joaquin River Delta which once held the largest concentration of beaver in North America.
In 1999, Washington, D.C.'s annual Cherry Blossom Festival was plagued by a family of beavers who lived in the Tidal Basin. The offenders were caught and removed, but not before damaging 14 cherry trees, including some of the largest and oldest trees.
As introduced non-native species
In the 1940s, beavers were brought to the island of Tierra Del Fuego in southern Chile and Argentina, for commercial fur production. However, the project failed and the beavers, a few pairs, were released into the wild. Having no natural predators in their new environment, they quickly spread throughout the island, and to other islands in the region, reaching a number of 100,000 individuals within just 50 years. They are now considered a serious invasive species in the region, due to their massive destruction of forest trees, and efforts are being made for their eradication. The drastically different ecosystem has led to substantial environmental damage, as the ponds created by the beavers have no ecological purpose (wetlands do not form there as they do in the beavers' native territory) and there are no native, large predators. They have also been found to cross saltwater to islands northward; a possible encroachment on the mainland has naturalists highly concerned.
In contrast, areas with introduced beaver were associated with increased populations of native puye fish (Galaxias maculatus), whereas the exotic brook trout (Salvelinus fontinalis) and rainbow trout (Oncorhynchus mykiss) had negative impacts on native stream fishes in the Cape Horn Biosphere Reserve, Chile.
Beaver meat is similar tasting to lean beef, but care must be taken to prevent contamination from the animal's strong castor (musk) gland. It is usually slow-cooked in a broth, and was a valuable food source to Native Americans. Early French Canadian Catholics considered beaver to be "four-legged fish" that could be eaten at Lent.
Despite their name, the fried pastries found in parts of Canada called beaver tails contain no beaver.
As the national animal and one of the national symbols of Canada, the beaver is depicted on the Canadian five-cent piece and was on the first Canadian postage stamp, the Three Penny Beaver. It is also the state animal of Oregon and New York, and a common school emblem for engineering schools, including the California Institute of Technology, the Massachusetts Institute of Technology, and the University of Alberta as well as the mascot for Oregon State University, Babson College, and the City College of New York. The beaver also appears in the coats of arms of the Hudson's Bay Company, University of Toronto, Wilfrid Laurier University, and the London School of Economics.
Much of the early economy of New Netherland was based on the beaver fur trade. As such, the seal of New Netherland featured the beaver; likewise, the coats of arms of Albany, New York and New York City included the beaver.
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- ^ Rudolf Ruedemann, W. J. Schoonmaker (1938-12-02). "Beaver-Dams as Geologic Agents". Science: 523–525. Bibcode 1938Sci....88..523R. doi:10.1126/science.88.2292.523.
- ^ Isabelle Groc (April,2010). "Beavers Sign up to Fight Effects of Climate Change". Discover. http://discovermagazine.com/2010/apr/19-beavers-sign-up-fight-effects-climate-change. Retrieved 2010-07-27.
- ^ "The Beaver Solution: Solving our Water Storage Dilemma in Eastern Washington". The Lands Council. March, 2010. http://www.landscouncil.org/beaversolution/what_can_beavers_do.asp. Retrieved 2010-07-27.
- ^ Utah Beaver Management Plan (Report). Utah Division of Wildlife Resources. 2010-01-06. pp. 25. http://wildlife.utah.gov/furbearer/pdf/beaver_plan_2010-2020.pdf. Retrieved 2010-08-29.
- ^ "New York City Beaver Returns". Science Daily. Dec. 20, 2008. http://www.sciencedaily.com/releases/2008/12/081218080817.htm.
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- ^ Design Trust for Public Space (June 17, 2009). "Bronx River Crossing". http://designtrust.blogspot.com/2009/06/bronx-river-crossing.html. Retrieved Dec. 4, 2009.
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- ^ Carolyn Jones (April 16, 2008). "Moment of truth for Martinez beavers". San Francisco Chronicle.
- ^ "Worth a Dam website". http://www.martinezbeavers.org.
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- ^ Thomas Jefferson Farnham (1857). Life, adventures, and travels in California. Blakeman & Co.. p. 383. http://books.google.com/?id=cwMNAAAAIAAJ&dq=travels+in+california+farnham&printsec=frontcover#v=onepage&q=beaver&f=false.
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- ^ Nelson Poirier (2010-11-27). "Our symbolic beaver overcomes challenges of past". Moncton, New Brunswick: Times & Transcript. http://timestranscript.canadaeast.com/travelleisure/article/1324978. Retrieved 2010-11-18.
- ^ a b The Beaver Heritage Canada
- ^ The HBC Coat of Arms, Hbc Heritage
- "Castor canadensis". Integrated Taxonomic Information System. http://www.itis.gov/servlet/SingleRpt/SingleRpt?search_topic=TSN&search_value=180212. Retrieved 18 March 2006.
- Dietland Müller-Schwarze, Lixing Sun (2003). The beaver: natural history of a wetlands engineer. Cornell University Press. pp. 190. ISBN 9780801440984.
- Mills, Enos (1913). In Beaver World. Kessinger Publishing. pp. 255. ISBN 9780766193871.
- Collier, Eric (2007). Three Against the Wilderness. Touchwood Editions. pp. 288. ISBN 9781894898546.
- Long, Kim (2000). Beavers: A Wildlife Handbook. Boulder: Johnson Books. p. 37. ISBN 1-55566-251-X.
- Ecology of the Beaver
- The romance of the beaver; being the history of the beaver in the western hemisphere, by A. Radclyffe Dugmore. Illustrated with photographs from life and drawings by the author. Publisher: Philadelphia, J.B. Lippincott company; London, W. Heinemann 1914 (a searchable facsimile at the University of Georgia Libraries)
- "Worth a Dam" (beaver information and educational site)
- The Beaver A Keystone Species, a short video by Mike Foster
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