Vancouver Lake | |
---|---|
Location | Clark County, Washington |
Coordinates | 45°40′40″N122°43′16″W / 45.6779°N 122.721°W |
Primary inflows | Columbia River (intermittent) and Burnt Bridge Creek (continuous) |
Primary outflows | Lake River (intermittent) |
Catchment area | Vancouver Lake/Lake River, Lakeshore, Burnt Bridge Creek, Salmon Creek, Whipple Creek, Flume Creek |
Basin countries | United States |
Max. width | > 2 mi (3.2 km) |
Surface area | approx. 2,400 acres (9.7 km2) |
Average depth | < 3 ft (0.9 m) |
Max. depth | 12 to 15 feet (3.7 to 4.6 m) |
Shore length1 | > 7 mi (11 km) |
Islands | 1 |
1 Shore length is not a well-defined measure. |
Vancouver Lake is located just west of Vancouver, Washington, United States, north of the Columbia River and Portland, Oregon, south of Ridgefield, Washington, and the Ridgefield National Wildlife Refuge.
The lake is shallow, with a maximum depth of 12 to 15 feet (3.7 to 4.6 m) and a mean depth of less than 3 feet (0.9 m). [1] [2] There is an island in the northern half of the lake named Turtle Island. [3] The island was formed from the tailings of an Army Corps of Engineers dredging project, which dredged around the perimeter of the lake in the early 1980s. Lake River flows from the north shore to the Columbia River near Ridgefield. Due to seasonal variation in relative river and lake levels, Lake River experiences intermittent flow reversal and flows into Vancouver Lake for considerable periods of time.
The sources for Vancouver Lake's water include a flushing channel (equipped with tidal gates to control flows) from the Columbia River near the southwest shoreline and Burnt Bridge Creek on the eastern shoreline, which winds about ten miles (sixteen kilometres) through many of the city's residential areas. Until the 1980s, this creek was neglected and a major source of pollution for the lake.
Lower River Road leads west out of Vancouver to a park on the shore of Vancouver Lake which includes a large swimming area. [4] A trail leads to Frenchman's Bar Park on the nearby Columbia River.
A study published in 2014 by Curt D.Peterson, et al, PSU Dept of Geology, includes results from multiple core samples which demonstrate there's been a lake in this location continuously going back at least 4000 years.
Vancouver Lake is home to a variety of wildlife species, many of which it shares with the nearby Ridgefield National Wildlife Refuge. Descriptions from the late 19th century describe Vancouver Lake as clear, up to 20 ft (6.1 m) deep and containing sturgeon. Current turbidity, more shallow depths and a lack of aquatic plant structures have diminished the variety of species and more recent surveys showed the most abundant fish by mass were brown bullhead, white crappie, black crappie, and common carp, with a few juvenile salmonids and a population of channel catfish, largemouth bass, bluegill, pumpkinseed, yellow perch, naturalized goldfish, northern pikeminnow, American shad, mosquito fish, largescale sucker, and freshwater sculpin. [5] [6] Rich fringe environments provide habitat for amphibians such as tree frogs, reptiles such as garter snakes and a wide variety of birds, including large species such as great blue herons, osprey and bald eagles. It is within the Pacific Flyway. Large mammals on its banks include raccoons, a few black-tailed deer and an occasional coyote.
Vancouver Lake was referenced in Lewis and Clark's journal entries from November 4, 1805 (v. 6, 17).
Shortly after the lake was deeded to the Port of Vancouver, Washington, in 1919, agricultural interests proposed draining it, (A smaller lake to the north, Shillapoo Lake, was drained and used for agriculture) but by the end of the 1920s, recreational uses were also considered. Because of cold weather, the lake was frozen solid to "several inches" in depth on February 10, 1929, and was home to 500 ice skaters one weekend. [7] The lake was briefly considered as a decommissioning harbor in 1945, but after the Memorial Day flood of 1948 was also seen as a possible resource in flood control. [8]
Suburbanization of its watershed area led to an increase in water pollution. Surface runoff brought increased sediment while residential drain fields and increased use of fertilizers rich in nitrogen and phosphorus contributed to eutrophication. DDT was also used for mosquito control until its effects on fish and birds became apparent, and the county discontinued it. A 2005 report showed higher than normal levels of various contaminants in the lake's fish. [9]
Since then, there have been various interests in the area as it relates to habitat preservation, recreation and industry, culminating in the "Habitek" plan of the mid-1980s and the multi-agency Burnt Bridge Creek Watershed Plan of 1995. Algal bloom has been an intermittent problem for recreational use of the lake (officially recognized by the county in 2003) since cyanobacteria such as Anabaena , Microcystis aeruginosa and Cylindrospermopsin raciborskii may produce neurotoxins such as cylindrospermopsin. [10] [11]
The Vancouver Lake Watershed Partnership was formed in October 2004, bringing various public agencies with interest and jurisdiction together. [12]
Vancouver Lake plays host to two water sport oriented recreation clubs. Vancouver Lake Crew is a high school and master aged rowing club that uses the lake as its primary practice facility. Along with rowing, kayaking, canoeing, and dragon boating are also popular activities hosted by Vancouver Lake Crew. On the opposite East shore sits the Vancouver Lake Sailing Club where sailboats can be launched, with opportunities for sailing education and racing.
In 2017, lake users noticed an increasing level of Eurasian Water Milfoil (EWM) in the lake. In late 2018, concerned citizens joined forces with local and state agencies to assess the EWM infestation. In early 2019, local volunteers formed a 501c(3) non-profit, Friends of Vancouver Lake. Working with the Vancouver Lake Crew, Vancouver Lake Sailing Club, and hundreds of concerned community members, they secured a Washington State permit to treat the lake with a newly-approved herbicide, ProcellaCOR. This fast-acting herbicide is targeted to EWM, but non-toxic to humans, fish, and wildlife. While environmental conditions prevented a treatment in 2019, Vancouver Lake and its flushing channel were treated with ProcellaCOR July 7, 2020. Post-treatment surveys several weeks later showed no trace of EWM in the lake or flushing channel.
The Columbia River is the largest river in the Pacific Northwest region of North America. The river forms in the Rocky Mountains of British Columbia, Canada. It flows northwest and then south into the U.S. state of Washington, then turns west to form most of the border between Washington and the state of Oregon before emptying into the Pacific Ocean. The river is 1,243 miles long, and its largest tributary is the Snake River. Its drainage basin is roughly the size of France and extends into seven states of the United States and one Canadian province. The fourth-largest river in the United States by volume, the Columbia has the greatest flow of any river entering the Pacific outside of Asia, and the 36th greatest discharge of any river in the world.
Clark County is the southernmost county in the U.S. state of Washington. As of the 2020 census, the population was 503,311, making it Washington's fifth-most populous county. Its county seat and largest city is Vancouver. It was the first county in Washington, first named Vancouver County in 1845 before being renamed for William Clark of the Lewis and Clark Expedition in 1849. It was created by the Provisional Government of Oregon in Oregon Country on August 20, 1845, and at that time covered the entire present-day state. Clark County is the third-most-populous county in the Portland-Vancouver-Hillsboro Metropolitan Statistical Area, and is across the Columbia River from Portland, Oregon.
Lake Washington is a large freshwater lake adjacent to the city of Seattle, Washington, United States. It is the largest lake in King County and the second largest natural lake in the state of Washington, after Lake Chelan. It borders the cities of Seattle on the west, Bellevue and Kirkland on the east, Renton on the south, and Kenmore on the north, and encloses Mercer Island. The lake is fed by the Sammamish River at its north end and the Cedar River at its south.
The Cedar River is a river in the U.S. state of Washington. About 45 miles (72 km) long, it originates in the Cascade Range and flows generally west and northwest, emptying into the southern end of Lake Washington. Its upper watershed is a protected area called the Cedar River Watershed, which provides drinking water for the greater Seattle area.
The Pend Oreille River is a tributary of the Columbia River, approximately 130 miles (209 km) long, in northern Idaho and northeastern Washington in the United States, as well as southeastern British Columbia in Canada. In its passage through British Columbia its name is spelled Pend-d'Oreille River. It drains a scenic area of the Rocky Mountains along the U.S.-Canada border on the east side of the Columbia. The river is sometimes defined as the lower part of the Clark Fork, which rises in western Montana. The river drains an area of 66,800 square kilometres (25,792 sq mi), mostly through the Clark Fork and its tributaries in western Montana and including a portion of the Flathead River in southeastern British Columbia. The full drainage basin of the river and its tributaries accounts for 43% of the entire Columbia River Basin above the confluence with the Columbia. The total area of the Pend Oreille basin is just under 10% of the entire 258,000-square-mile (670,000 km2) Columbia Basin. Box Canyon Dam is currently underway on a multimillion-dollar project for a fish ladder.
Lake Apopka is the fourth largest lake in the U.S. state of Florida. It is located 15 miles (24 km) northwest of Orlando, mostly within the bounds of Orange County, although the western part is in Lake County. Fed by a natural spring, rainfall and stormwater runoff, water from Lake Apopka flows through the Apopka-Beauclair Canal and into Lakes Beauclair and Dora. From Lake Dora, water flows into Lake Eustis, then into Lake Griffin and then northward into the Ocklawaha River, which flows into the St. Johns River. Multiple parks or nature trails are present around the lake including Magnolia Park, Lake Apopka Wildlife Drive, Ferndale Preserve, Oakland Nature Preserve, Dr. Bradford Memorial Park, and Newton Park, named for A. B. Newton.
The North Shore Channel is a drainage canal built between 1907 and 1910 to flush the sewage-filled North Branch of the Chicago River down the Chicago Sanitary and Ship Canal. The sewage carrying duty has been largely taken over by the Chicago Deep Tunnel, but there are still occasional discharges due to heavy rains.
Nicola Lake is a glacially formed narrow, deep lake located in the South-Central Interior of British Columbia, Canada approximately thirty kilometres northeast of the city of Merritt. It was a centrepoint of the first settlements in the grasslands lying south of Kamloops, and today is used for recreation and as a water storage site to provide irrigation and water flows to fisheries downstream in the Nicola River. The lake is important in the history of the local Nicola people as the location of one of their major communities, Nicola Lake Indian Reserve No. 1, which lies on its eastern shore and is the home of the Upper Nicola Indian Band. Many of the band work for the Douglas Lake Cattle Company, aka the Douglas Lake Ranch, whose headquarters are also adjacent to the lake.
Lake River is a tributary, about 11 miles (18 km) long, of the Columbia River in the U.S. state of Washington. It flows north from Vancouver Lake in Vancouver to meet the larger river near Ridgefield and the northern tip of Bachelor Island. The Wilkes Expedition of 1841 referred to Lake River as Calipaya Inlet.
Still Creek is a long stream flowing across Central Burnaby, British Columbia and into Burnaby Lake. Still Creek's path lies mainly through the industrial area which contributes to its high level of pollution, although through dedicated work of local volunteers the creek is slowly recovering.
Crab Creek is a stream in the U.S. state of Washington. Named for the presence of crayfish, it is one of the few perennial streams in the Columbia Basin of central Washington, flowing from the northeastern Columbia River Plateau, roughly 5 km (3.1 mi) east of Reardan, west-southwest to empty into the Columbia River near the small town of Beverly. Its course exhibits many examples of the erosive powers of extremely large glacial Missoula Floods of the late Pleistocene, which scoured the region. In addition, Crab Creek and its region have been transformed by the large-scale irrigation of the Bureau of Reclamation's Columbia Basin Project (CBP), which has raised water table levels, significantly extending the length of Crab Creek and created new lakes and streams.
State Route 501 is a 13.97-mile-long (22.48 km) state highway in the southern part of the U.S. state of Washington. It is split into two sections in Clark County, a north–south alignment connecting Interstate 5 (I-5) in Vancouver to the Port of Vancouver and the Ridgefield National Wildlife Refuge, and a west–east alignment connecting Ridgefield to I-5. Prior to the 1964 highway renumbering, SR 501 was designated as Secondary State Highway 1T (SSH 1T), established in 1937 and re-aligned to serve the Port of Vancouver in 1963.
Lacamas Creek is in Clark County, Washington, United States, and flows about 12.5 miles (20.1 km) from headwaters near Camp Bonneville to Lacamas Lake and Round Lake in Camas, and eventually into the Washougal River. Its name is derived from that of the native camas plant. Lacamas Creek is fed by numerous streams, but the five largest tributaries are Matney Creek, Shanghai Creek, Fifth Plain Creek, China Ditch, and Dwyer Creek.
The Watuppa Ponds are two large, naturally occurring, spring-fed, glacially formed ponds located in Fall River and Westport, Massachusetts. Watuppa is a native word meaning "place of boats". The two ponds were originally one body of water, connected by a narrow rocky straight called "The Narrows" located on a thin strip of land between the two ponds which forms part boundary of between Fall River and Westport. The border between Fall River and Westport is also divided between the two ponds. Together, the ponds have an overall north–south length of about 7.5 miles, and have an average east–west width of about a mile. The ponds are drained by the Quequechan River, and flows in a westerly direction through the center of Fall River from South Watuppa Pond to Mount Hope Bay.
Lake Phalen is an urban lake located in Saint Paul, Minnesota and in its suburb of Maplewood. It is one of the largest lakes in Saint Paul and is the centerpiece of the Phalen Regional Park System. The lake drains into the Mississippi River after traveling through Phalen Creek. The lake and surrounding 494-acre (2.00 km2) park receive around 500,000 visitors each year.
The Columbia Slough is a narrow waterway, about 19 miles (31 km) long, in the floodplain of the Columbia River in the U.S. state of Oregon. From its source in the Portland suburb of Fairview, the Columbia Slough meanders west through Gresham and Portland to the Willamette River, about 1 mile (1.6 km) from the Willamette's confluence with the Columbia. It is a remnant of the historic wetlands between the mouths of the Sandy River to the east and the Willamette River to the west. Levees surround much of the main slough as well as many side sloughs, detached sloughs, and nearby lakes. Drainage district employees control water flows with pumps and floodgates. Tidal fluctuations cause reverse flow on the lower slough.
Gee Creek is a 4th order tributary to the Columbia River, a.k.a. small creek, within Clark County, Washington named for William Gee, an early pioneer upon whose land the stream arose from. The Upper Gee Creek watershed, with an 8.7-square-mile (23 km2) drainage basin, is completely located within the Ridgefield quadrangle. The mainstem extends approximately 11.5 miles (18.5 km), of which 4.9 miles (7.9 km) are located within the Upper Gee Creek basin. Originating in the hills along Interstate 5, through Ridgefield, Washington and empties into a series of lakes on the Columbia River Floodplain. Abrams Park in Ridgefield is a local access point for Gee Creek and since 2003, has had a stream flow gauge installed to collect hydrological data. The lowest segment of Gee Creek meanders for 3 miles (4.8 km) through the Ridgefield National Wildlife Refuge.
Burnt Bridge Creek is a 13-mile (21 km) stream flowing for most of its length within the city of Vancouver in the U.S. state of Washington. It begins as drainage from field ditches near the unincorporated community of Orchards, east of the city. The creek flows generally west to Vancouver Lake. The lake drains to Lake River, which empties into the Columbia River about 11 miles (18 km) downstream of the city.
The Belgrade Lakes are a chain of lakes around Belgrade, Maine. The flow sequence is from East Pond to North Pond to Great Pond to Long Pond to Messalonskee Lake and thence via Messalonskee Stream to the Kennebec River at Waterville. The lakes have long been an important resort area for fishing, boating, and swimming; and shoreline development includes residences for individuals employed in the cities of Waterville and Augusta.
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: CS1 maint: multiple names: authors list (link)Feb 9. ... Vancouver lake is frozen from shore to shore and about 500 persons were skating there last night. The ice is several inches thick and perfectly safe.