Yukon River Basin

Last updated
Yukon River Basin
Yukon River Basin USGS.jpg
The location of the Basin is between Alaska and Yukon Territory
Physical characteristics
Source 
  locationAlaska and The Yukon Territory
Basin size330,000 square miles (850,000 km2)
Basin features
River system Yukon River
Population126,000 indigenous peoples

The Yukon River Basin is located between the Yukon Territory in Canada and Alaska in the United States, with a small portion in British Columbia, Canada. This basin is made up of 13 other individual basins that drain into the Yukon River and other adjoining rivers and tributaries. The Yukon River Basin is 330,000 square miles (850,000 km2) in area and 1,980 miles (3,190 km) in length. [1] Many different geological features make up the basin, including several types of terrain, shrubland, and rivers.

Contents

In the mid to late 1800s, European and American explorers discovered its natural resources and began settling in the region. [1] The Yukon River Basin remains a relatively intact ecosystem, known for its density of salmon, which are used as both food for the villagers and a growing industry for the community.

History

Some of the oldest known humans who inhabited North America are thought to have lived around the western part of the Yukon Basin. They migrated across the land bridge, Beringia, living without influence from other cultures for hundreds of years. [1]

The earliest exploration and European settlement in the Yukon River Basin was by Robert Campbell in 1840. Early explorers like Campbell came not for gold but for furs. In the 1870s, explorers like Leroy McQuesten, Arthur Harper, and Alfred Mayo discovered how plentiful the Yukon river and Yukon River basin was with minerals. Their mining ventures grew and spread until they reached the Stewart River, where they found gold, starting the Klondike Gold Rush. [1]

Geography

The Alaskan Range is part of the topography in the Yukon River Basin. The mountains range from 6,000 to 9,000 feet (1,800 to 2,700 m) in elevation. Alaskan Range.jpg
The Alaskan Range is part of the topography in the Yukon River Basin. The mountains range from 6,000 to 9,000 feet (1,800 to 2,700 m) in elevation.

The Yukon River Basin is approximately 330,000 square miles (850,000 km2) in area and 1,980 miles (3,190 km) in length. [1] This makes the Yukon River Basin the fourth largest basin in North America. It is located between the Rocky Mountains in the north and the Pacific Mountain system to the south. The Basin span across Canada in the Yukon Territory and Alaska. [2] The Yukon Flats basin is south of the Yukon River Basin and it drains deposits and reworked materials into the Flats. [3] It is within the Arctic Complex of the Arctic-Atlantic Bioregion, therefore has freshwater. [4]

The Yukon River Basin is made up of 13 other individual basins and stretches across two countries, America and Canada. While there are 13 individual basins within the Yukon Basin, there are also 5 physio-graphic regions. The topography of the Basin is very diverse with different elevations, so that is why there are regions. They include, Alaska Range (6,000–9,000 feet or 1,800–2,700 metres), Central and Eastern Brooks Range (7,000–8,000 feet or 2,100–2,400 metres), Indian River Uplands (1,500–2,000 feet or 460–610 metres), Innoko Lowlands (flat flood plains), and Kolkrine-Hodzana Highlands (2,000–4,000 feet or 610–1,220 metres). [1]

Geology

Limestone is a type of sedimentary rock found in Canada, where half the Yukon River Basin is located Stromatoporoids.jpg
Limestone is a type of sedimentary rock found in Canada, where half the Yukon River Basin is located

Half of the Yukon River Basin lies in Canada, with the other half occupying space in Alaska. The Yukon River Basin is made up of many different geological terrains, which is why there is a variety of different rocks that make up the basin itself. A few of the many types of rocks includes various types of sedimentary, igneous, and metamorphic rocks [2] There are several different land types that make up the entirety of the Yukon River Basin. These include the needleleaf forest, tall and low shrublands, broadleaf forest, lichens, barren, wet herbaceous, dwarf shrublands, dry herbaceous, ice/snow, and rivers, streams, and lakes. There are also many different types of soils that make up the Yukon River Basin. These soils include Entisols, Gelisols, Inceptisols, Inceptisols/Gelisols, Mollisols, Spodosols, and Rough Mountainous Land. [2]

Permafrost dominates the Yukon River Basin. Because of the level of permafrost in the basin, the basin itself is far more prone to flash floods. The melting of permafrost is believed to be one of the reasons that the Yukon River Basin's flow has increased over the years, causing erosion of the basin. [5]

Hydrology

The Yukon River Basin drains from east to west, with the temperature of the water increasing as the water flows down stream. [6] The water, fish, and other animals throughout the basin are used by local inhabitants for various reasons, which is why it is very important that the quality of the water be checked often and be healthy. [7] Water quality varies from site to site throughout the Yukon River Basin, for example the density throughout the eastern and southern sites of the basin is much more prominent than that of the western and northern cites. [2] Because of its northern location, the Yukon River Basin is frozen over for nearly 8 months out of the year. [2]

Climate

The climate around the Yukon River Basin varies because of factors like its topography and large size. This large area covers land from Alaska and from parts of the Yukon Territory in Canada. [7] The precipitation over the entire basin is approximately 19 inches (480 mm) per year. With the diverse topography certain places receive more rain than others. Some areas receive less than 10 inches (250 mm) of rainfall a year and others receive up to 50 inches (1,300 mm). With that being said, annual rainfall is greater on tall, rugged mountains than on flat lowland areas of the whole region. [1] The average temperature now for the Yukon River Basin is approximately 30 °C (86 °F) in the summer and −40 °C (−40 °F) in the winter. [7] However, the region has some of the most extreme temperature changes for an area that is located in a continental zone. [7] [8]

Climate change

Recent studies indicate that temperatures have been steadily rising throughout the region since the 1840s. Climate change has been a serious, on-going issue around the Yukon River Basin and other surrounding areas. With drier, hotter temperatures, there have been more forest fires and melting permafrost, which leads to changes in water flows. [2] The recent change in climate has also taken a toll on the Yukon River basin, such as flooding in 2009 due to the above average snow and ice levels, followed by and abnormal high spring temperatures. [7] Rapid melting of the ice and snow flooding, erosion, and damage from debris along the river. Not only has the climate change affected the Yukon river and the Yukon river basin but, it has also affected the watershed as a whole. [7]

Ecosystems

Aspen forest located near the Yukon River Basin, in a physiographic region called the Yukon Flats Aspen forest in Yukon Flats National Wildlife Refuge.jpg
Aspen forest located near the Yukon River Basin, in a physiographic region called the Yukon Flats

The Yukon River Basin has a relatively intact ecosystem. It is a quality habitat for birds, mammal, fish, invertebrates, and one amphibian. [9] The wood frog is the only amphibian able to survive in the ecosystem. [9] This is due to its increased level of glucose in its cells. This addition acts as an antifreeze. It allows the frogs to survive the extremely cold winters. [9] The basin consists of thousands of lakes, ponds, sloughs, wetlands, and rivers/streams to provide habitats for these animals. [9] Within the basin there are more than 150 bird species, 40 mammals, and 18 fish species. [9] There is an estimated 1.5 million ducks that breed here annually. It is also home to the longest salmon runs in history. [9] Plant life includes white spruce, paper birch, and quaking aspen forests, willow and alder thickets, grasslands, and meows. In these areas are where the animals of the ecosystem thrive. [9]

Salmon

The Yukon River Basin is home to the longest salmon runs in history. Salmon from this area are prized for their rich oily meat. This is due to the large fat reserves that they must build up in order to make the long journey up the Yukon River. [7] A few examples of these prized salmon would be of the chinook, coho and chum salmon species. [7]

Not only are the salmon prized for their meat, but also as an economic resource for villages in the area. [7] In these areas the salmon are typically dried, smoked, and frozen. [7] Without these salmon runs it is possible that the ecosystem might not thrive. Therefore, the fisheries are managed by the Alaska Department of Fish and Game along with other national and international treaties. [7]

Many studies have been done to watch the migratory patterns of the salmon. In one particular study researchers studied the migratory patterns of wild chinook salmon. [10] They did this by capturing and tagging adult chinook salmon from June to mid July in the lower Yukon river. [10] The tagged fish had radio transmitters, which were used to track the salmon and their migration patterns throughout the Yukon river. [10] This data was then used to monitor the salmon in the river system.

Table 1:
Category (year)200220032004All Years
Start of Tagging9 June3 June3 June3-9 June
End of Tagging13 July14 July19 July13-19 July
Captured1, 3102,3122,1075,729
Tagged7681,0979952,860
Moved Up River7511,0819582,790
Tracked Past Multiple Stations6831,0508932,626
Typical Pattern6661,0318632,560

This is data regarding Chinook salmon migration in the Yukon river. [10]

Demographics

The Yukon River Basin has 4 towns/cities and 43 villages, with approximately 126,000 currently inhabitants. Of those, 10 percent still rely solely on the land and 83 percent are indigenous. [9] In the towns of Dawson and Faro, there are 1,000-2,000 residents. The city Whitehorse has over 23,000 residents, while Fairbanks had around 84,000 residents. Villages around the basin hold anywhere from 30 to 800 people. [1]

Related Research Articles

<span class="mw-page-title-main">Yukon River</span> Major watercourse in northwestern North America

The Yukon River is a major watercourse of northwestern North America. From its source in British Columbia, Canada, it flows through Canada's territory of Yukon. The lower half of the river continues westward through the U.S. state of Alaska. The river is 3,190 kilometres (1,980 mi) long and empties into the Bering Sea at the Yukon–Kuskokwim Delta. The average flow is 6,400–7,000 m3/s (230,000–250,000 cu ft/s). The total drainage area is 833,000 km2 (321,500 sq mi), of which 323,800 km2 (125,000 sq mi) lies in Canada. The total area is more than 25% larger than Texas or Alberta.

<span class="mw-page-title-main">Arctic National Wildlife Refuge</span> Protected area in Alaska

The Arctic National Wildlife Refuge or Arctic Refuge is a national wildlife refuge in northeastern Alaska, United States, on traditional Gwich'in lands. The refuge is 19,286,722 acres (78,050.59 km2) of the Alaska North Slope region, with a northern coastline and vast inland forest, taiga, and tundra regions. ANWR is the largest national wildlife refuge in the country, slightly larger than the Yukon Delta National Wildlife Refuge. The refuge is administered from offices in Fairbanks. ANWR is home to a diverse range of endemic mammal species; notably, it is one of the few North American locations with all three endemic American ursids—the polar bear, grizzly bear, and American black bear, each of which resides predominantly in its own ecological niche. Besides the bears, other mammal species include the moose, caribou, wolves, red and Arctic fox, Canada lynx, wolverine, pine marten, American beaver, and North American river otter. Further inland, mountain goats may be seen near the slope. Hundreds of species of migratory birds visit the refuge yearly, and it is a vital, protected breeding location for them. Snow geese, eiders and snowy owl may be observed as well.

<span class="mw-page-title-main">Permafrost</span> Soil frozen for a duration of at least two years

Permafrost is soil or underwater sediment which continuously remains below 0 °C (32 °F) for two or more years. Land-based permafrost can include the surface layer of the soil, but if the surface is too warm, it may still occur within a few centimeters of the surface down to hundreds of meters. It usually consists of ice holding in place a combination of various types of soil, sand, and rock, though in ice-free ground, perennially frozen non-porous bedrock can serve the same role.

<span class="mw-page-title-main">Mackenzie River</span> Largest river system in Canada

The Mackenzie River is a river in the Canadian boreal forest. It forms, along with the Slave, Peace, and Finlay, the longest river system in Canada, and includes the second largest drainage basin of any North American river after the Mississippi.

<span class="mw-page-title-main">Kobuk River</span> River in Alaska, United States

The Kobuk River' is a river located in the Arctic region of northwestern Alaska in the United States. It is approximately 280 miles (451 km) long. Draining a basin with an area of 12,300 square miles (32,000 km2), the Kobuk River is among the largest rivers in northwest Alaska with widths of up to 1,500 feet and flow at a speed of 3–5 miles per hour in its lower and middle reaches. The average elevation for the Kobuk River Basin is 1,300 feet (400 m) above sea level, ranging from near sea level to 11,400 feet. Topography includes low, rolling mountains, plains and lowlands, moderately high rugged mountainous land, and some gently sloped plateaus and highlands. The river contains an exceptional population of sheefish, a large predatory whitefish within the salmon family, found throughout the Arctic that spawns in the river's upper reaches during the autumn. A portion of the vast Western Arctic Caribou Herd utilize the Kobuk river valley as winter range.

<span class="mw-page-title-main">Stikine River</span> River in British Columbia and Alaska

The Stikine River is a major river in northern British Columbia (BC), Canada and southeastern Alaska in the United States. It drains a large, remote upland area known as the Stikine Country east of the Coast Mountains. Flowing west and south for 610 kilometres (379 mi), it empties into various straits of the Inside Passage near Wrangell, Alaska. About 90 percent of the river's length and 95 percent of its drainage basin are in Canada. Considered one of the last truly wild large rivers in BC, the Stikine flows through a variety of landscapes including boreal forest, steep canyons and wide glacial valleys.

<span class="mw-page-title-main">Chum salmon</span> Species of fish

The chum salmon, also known as dog salmon or keta salmon, is a species of anadromous salmonid fish from the genus Oncorhynchus native to the coastal rivers of the North Pacific and the Beringian Arctic, and is often marketed under the trade name silverbrite salmon in North America. The English name "chum salmon" comes from the Chinook Jargon term tzum, meaning "spotted" or "marked"; while keta in the scientific name comes from Russian, which in turn comes from the Evenki language of Eastern Siberia. The term 'Dog Salmon' is most commonly used in Alaska and refers to the Salmon who's flesh Alaskans use to feed their dogs.

<span class="mw-page-title-main">Chinook salmon</span> Species of fish

The Chinook salmon is the largest and most valuable species of Pacific salmon in North America, as well as the largest in the genus Oncorhynchus. Its common name is derived from the Chinookan peoples. Other vernacular names for the species include king salmon, Quinnat salmon, Tsumen, spring salmon, chrome hog, Blackmouth, and Tyee salmon. The scientific species name is based on the Russian common name chavycha (чавыча).

<span class="mw-page-title-main">Taku River</span> River in Canada, United States

The Taku River is a river running from British Columbia, Canada, to the northwestern coast of North America, at Juneau, Alaska. The river basin spreads across 27,500 square kilometres (10,600 sq mi). The Taku is a very productive salmon river and its drainage basin is primarily wilderness.

<span class="mw-page-title-main">Geography of Yukon</span>

Yukon is in the northwestern corner of Canada and is bordered by Alaska and the Northwest Territories. The sparsely populated territory abounds with natural scenic beauty, with snowmelt lakes and perennial white-capped mountains, including many of Canada's highest mountains. The territory's climate is Arctic in territory north of Old Crow, subarctic in the region, between Whitehorse and Old Crow, and humid continental climate south of Whitehorse and in areas close to the British Columbia border. Most of the territory is boreal forest with tundra being the main vegetation zone only in the extreme north and at high elevations.

Polar ecology is the relationship between plants and animals in a polar environment. Polar environments are in the Arctic and Antarctic regions. Arctic regions are in the Northern Hemisphere, and it contains land and the islands that surrounds it. Antarctica is in the Southern Hemisphere and it also contains the land mass, surrounding islands and the ocean. Polar regions also contain the subantarctic and subarctic zone which separate the polar regions from the temperate regions. Antarctica and the Arctic lie in the polar circles. The polar circles are imaginary lines shown on maps to be the areas that receives less sunlight due to less radiation. These areas either receive sunlight or shade 24 hours a day because of the earth's tilt. Plants and animals in the polar regions are able to withstand living in harsh weather conditions but are facing environmental threats that limit their survival.

<span class="mw-page-title-main">Teshekpuk Lake</span> Lake on the coast of Alaska

Teshekpuk Lake is the largest lake in Arctic Alaska, at 22 miles (35 km) width on the Alaska North Slope within the National Petroleum Reserve-Alaska, South of Pitt Point, 12 miles (19 km) east of Harrison Bay, 80 miles (130 km) east of Point Barrow. The Teshekpuk Lake region is considered one of the most productive, diverse, and sensitive wetland ecosystems in the entire Arctic, habitat to a variety of arctic wildlife, including the resident Teshekpuk Lake caribou herd of 64,000 animals, large numbers of shorebirds and migratory waterfowl, for whom it is an essential part of the East Asian–Australasian Flyway site network.

Aufeis is a sheet-like mass of layered ice that forms from successive flows of ground or river water during freezing temperatures. This form of ice is also called overflow, icings, or the Russian term, naled. The term "Aufeis" was first used in 1859 by Alexander von Middendorff following his observations of the phenomenon in northern Siberia.

<span class="mw-page-title-main">Drunken trees</span> Stand of trees displaced from their normal vertical alignment

Drunken trees, tilted trees, or a drunken forest, is a stand of trees rotated from their normal vertical alignment.

<span class="mw-page-title-main">Arctic ecology</span> Study of the relationships between biotic and abiotic factors in the arctic

Arctic ecology is the scientific study of the relationships between biotic and abiotic factors in the arctic, the region north of the Arctic Circle. This region is characterized by stressful conditions as a result of extreme cold, low precipitation, a limited growing season and virtually no sunlight throughout the winter. The Arctic consists of taiga and tundra biomes, which also dominate very high elevations, even in the tropics. Sensitive ecosystems exist throughout the Arctic region, which are being impacted dramatically by global warming.

<span class="mw-page-title-main">Kanuti National Wildlife Refuge</span> National wildlife refuge in central Alaska, United States

Kanuti National Wildlife Refuge is a national wildlife refuge in central Alaska, United States. One of 16 refuges in Alaska, it was established in 1980 when Congress passed The Alaska National Interest Lands Conservation Act (ANILCA). At 1,640,000 acres (6,600 km2), Kanuti Refuge is about the size of the state of Delaware. Located at the Arctic Circle, the refuge is a prime example of Alaska's boreal ecosystem. It is dominated by black and white spruce, with some white birch and poplars.

<span class="mw-page-title-main">Koyukuk National Wildlife Refuge</span> Conservation area in Alaska

The Koyukuk National Wildlife Refuge is a 3,500,000-acre (14,000 km2) conservation area in Alaska. It lies within the floodplain of the Koyukuk River, in a basin that extends from the Yukon River to the Purcell Mountains and the foothills of the Brooks Range. This region of wetlands is home to fish, waterfowl, beaver and Alaskan moose, and wooded lowlands where two species of fox, bears, wolf packs, Canadian lynx and marten prowl.

<span class="mw-page-title-main">North American Arctic</span>

The North American Arctic is composed of the northern polar regions of Alaska (USA), Northern Canada and Greenland. Major bodies of water include the Arctic Ocean, Hudson Bay, the Gulf of Alaska and North Atlantic Ocean. The North American Arctic lies above the Arctic Circle. It is part of the Arctic, which is the northernmost region on Earth. The western limit is the Seward Peninsula and the Bering Strait. The southern limit is the Arctic Circle latitude of 66° 33’N, which is the approximate limit of the midnight sun and the polar night.

<span class="mw-page-title-main">Interior Alaska–Yukon lowland taiga</span> Taiga ecoregion of Canada and the United States

The interior Alaska–Yukon lowland taiga is an ecoregion in the taiga and boreal forests biome, of far northern North America.

The Northwestern Forested Mountains is a Level I ecoregion of North America designated by the Commission for Environmental Cooperation (CEC) in its North American Environmental Atlas.

References

  1. 1 2 3 4 5 6 7 8 "Environmental and Hydrologic Overview of the Yukon River Basin, Alaska and Canada" (PDF). Water Resources Investigation Report. 99–4204.
  2. 1 2 3 4 5 6 Water-supply Paper. U.S. Government Printing Office. 1915-01-01.
  3. Geological Survey Bulletin. U.S. Department of the Interior, Geological Survey; Washington, D.C. 1949-01-01.
  4. Benke, Arthur C.; Cushing, Colbert E. (2011-09-06). Rivers of North America. Academic Press. ISBN   9780080454184.
  5. Wilson, Nicole J.; Walter, M. Todd; Waterhouse, Jon (2015-02-23). "Indigenous Knowledge of Hydrologic Change in the Yukon River Basin: A Case Study of Ruby, Alaska". Arctic. 68 (1): 93–106. doi: 10.14430/arctic4459 . ISSN   1923-1245.
  6. Walvoord, Michelle A.; Striegl, Robert G. (2007). "Increased groundwater to stream discharge from permafrost thawing in the Yukon River basin: Potential impacts on lateral export of carbon and nitrogen". Geophysical Research Letters. 34 (12): L12402. Bibcode:2007GeoRL..3412402W. doi: 10.1029/2007gl030216 .
  7. 1 2 3 4 5 6 7 8 9 10 11 "Yukon River Condition Summary" (PDF). August 2012. Retrieved 15 November 2016.
  8. "USGS". USGS. March 2010.{{cite web}}: Missing or empty |url= (help)
  9. 1 2 3 4 5 6 7 8 "Yukon River Condition Summary" (PDF). August 2012. Retrieved 15 November 2016.
  10. 1 2 3 4 Eiler, J. H.; Evans, A. N.; Schreck, C. B. (2015). "Migratory Patterns of Wild Chinook Salmon Oncorhynchus tshawytscha Returning to a Large, Free-Flowing River Basin". PLOS ONE. 10 (4): 1–33. Bibcode:2015PLoSO..1023127E. doi: 10.1371/journal.pone.0123127 . PMC   4412830 . PMID   25919286.