Matanuska River

Matanuska River
Silt-laden waters of the Chickaloon River (right center) enter the Matanuska River at mile 76 (km 123) of the Glenn Highway (upper right), a major highway connecting Anchorage to the rest of the state. The valley is forested with black cottonwood, balsam poplar, white spruce and paper birch.
Country United States
State Alaska
Borough Matanuska-Susitna
Source confluence of the river's east and south forks
 - elevation 2,033 ft (620 m) [1]
 - coordinates 61°47′27″N 147°29′07″W / 61.79083°N 147.48528°W / 61.79083; -147.48528 [2]
Mouth Knik Arm, Cook Inlet
 - location 9.5 miles (15.3 km) southwest of Palmer
 - elevation 0 ft (0 m) [2]
 - coordinates 61°29′49″N 149°16′11″W / 61.49694°N 149.26972°W / 61.49694; -149.26972Coordinates: 61°29′49″N 149°16′11″W / 61.49694°N 149.26972°W / 61.49694; -149.26972 [2]
Length 75 mi (121 km) [3]
Basin 2,100 sq mi (5,439 km2) [4]
Discharge for Palmer
 - average 3,875 cu ft/s (110 m3/s) [5]
 - max 82,100 cu ft/s (2,325 m3/s)
 - min 234 cu ft/s (7 m3/s)
South-central Alaska, near Anchorage
Location of the mouth of the Matanuska River in Alaska

The Matanuska River is a 75-mile (121 km) long stream in Southcentral Alaska, United States.[3] The river drains a broad valley south of the Alaska Range eponymously known as the Matanuska Valley (Mat-Su Valley).[6]

Course

Formed by the confluence of its east and south forks, the Matanuska River flows generally southwest to the Knik Arm of Cook Inlet.[2] Downstream of its source, the river is joined by meltwater from Matanuska Glacier in the northern Chugach Mountains.[6] From there it continues through the Matanuska Valley, between the Chugach Mountains to the south and the Talkeetna Mountains to the north.[6] Population centers along its course include Chickaloon, Sutton, Palmer, and Butte.[6] It enters the Knik Arm of Cook Inlet about 9.5 miles (15.3 km) southwest of Palmer[2] and about 25 miles (40 km) northeast of Anchorage.[7]

The Glenn Highway runs roughly parallel to the river for much of its length.[6] Highway bridges over the river, listed from source to mouth, include Glacier Park Bridge, Chickaloon River Bridge, King River Bridge, Old Glenn Highway Bridge, and Glenn Highway Bridge.[7] An Alaska Railroad bridge crosses the river parallel to the Glenn Highway Bridge at Palmer Hay Flats State Game Refuge.[6] Mantanuska Glacier State Recreation Site is along the highway where Glacier Creek enters the river; King Mountain State Recreation Site is near Chickaloon, and Kepler – Bradley Lakes State Recreation Area is near Palmer.[6]

In addition to the glacier, named and unnamed streams that drain the Talkeetna and Chugach ranges feed into the river. These include Glacier, Hicks, Purinton, Caribou, and Coal creeks, and the Chickaloon and King rivers, and many others.[6] The main stem is silty with glacial run-off from spring through fall but at lower flows beneath winter ice, it runs relatively clear.[4]

The Mat-Su Valley is one of the most settled regions of Alaska and one of the few areas in the state to support agriculture. Erosion by the glacial braided river has damaged roads, farms, houses, and houses for decades.[4]

Discharge

The United States Geological Survey operates a stream gauge near Palmer.[5] Mean monthly discharge at this gauge varies from 500 cubic feet per second (14 m3/s) in March to 13,000 cubic feet per second (370 m3/s) in July. The maximum recorded flow was 82,100 cubic feet per second (2,320 m3/s) on August 10, 1971, after the break-out of a natural reservoir on Granite Creek.[8] The minimum recorded flow of 234 cubic feet per second (6.6 m3/s) occurred on April 25, 1956.[5]

Boating

The river is a popular destination for whitewater enthusiasts who float mainly in rafts or kayaks. Accessible at several bridges and other points along the Glenn Highway, the Matanuska varies from Class II (medium) to III (difficult) on the International Scale of River Difficulty. Expert paddlers sometimes run a tributary, Caribou Creek, that flows past Matanuska Glacier and is rated Class II to IV (very difficult). Hazards along the main stem include swift, cold water; big standing waves and holes along some sections; overhanging or submerged vegetation on the lower reaches, and upriver winds.[7]

Etymology

The indigenous Dena'ina Athabascan name for the river is Ch'atanhtnu, based on the root -tanh "trail extends out", meaning literally "trail comes out river".[9] The English place name Matanuska derives from a Russian term spelled in various ways, including "Matanooski" and "Mednoviska", and meaning "copper river people", perhaps referring to an implied route from Cook Inlet to the Copper River.[3]

See also

References

  1. ↑ Derived by entering source coordinates in Google Earth.
  2. 1 2 3 4 5 "Matanuska River". Geographic Names Information System. United States Geological Survey. March 31, 1981. Retrieved December 5, 2013.
  3. 1 2 3 Orth, Donald J.; United States Geological Survey (1971) [1967]. Dictionary of Alaska Place Names: Geological Survey Professional Paper 567 (PDF). University of Alaska Fairbanks. United States Government Printing Office. p. 628. Retrieved December 5, 2013.
  4. 1 2 3 Curran, J. H.; McTeague, M. L. (2011). "Geomorphology and Bank Erosion of the Matanuska River, Southcentral Alaska: Scientific Investigations Report 2011–5214" (PDF). U.S. Geological Survey. pp. 1–5. Retrieved December 5, 2013.
  5. 1 2 3 "USGS 15284000 Matanuska River at Palmer, Alaska". United States Geological Survey. Retrieved December 6, 2013.
  6. 1 2 3 4 5 6 7 8 Alaska Atlas & Gazetteer (7th ed.). Yarmouth, Maine: DeLorme. 2010. pp. 83–84. ISBN 978-0-89933-289-5.
  7. 1 2 3 Jettmar, Karen (2008) [1993]. The Alaska River Guide: Canoeing, Kayaking, and Rafting in the Last Frontier (3rd ed.). Birmingham, Alabama: Menasha Ridge Press. pp. 244–46. ISBN 978-0-89732-957-6.
  8. ↑ "Water-Data Report 2012: 15284000 Matanuska River at Palmer, AK" (PDF). United States Geological Survey. Retrieved December 7, 2013.
  9. ↑ Kari, James (2013) [2007]. Dena'ina Topical Dictionary. Fairbanks: Alaska Native Language Center. ISBN 978-1-55500-091-2.

Further reading

External links

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