Английская Википедия:Gasconade River

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Шаблон:Short description

Файл:Gasconaderivermap.png

The Gasconade River is about Шаблон:Convert long[1] and is located in central and south-central Missouri.[2][3]

The Gasconade River begins in the Ozarks southwest of Hartville in Wright County and flows generally north-northeastwardly through Wright, Laclede, Pulaski, Phelps, Maries, Osage and Gasconade counties, through portions of the Mark Twain National Forest. It flows into the Missouri River near the town of Gasconade in Gasconade County.[4][3][5] At Rich Fountain, the river has a mean annual discharge of 3,097 cubic feet per second.[6]

Name

The name Gasconade is derived from "Gascon", an inhabitant of the French region of Gascony.[7] The people of that province were noted for their boastfulness. It was applied by the early French to the Indians living on its banks who bragged about their exploits. The name means to boast or brag, and thus the river received its name. The waters of the river are boisterous and boastful and the name is also descriptive.[8]

River course

The headwaters of the Gasconade are in the southeastern corner of Webster County northeast of Seymour, Missouri where it drains the eastern margin of the Springfield Plateau at approximately Шаблон:Coord.[9] The river joins the Missouri River at the city of Gasconade at Шаблон:Coord.[10] The river follows a meandering course through the Ordovician age dolomite and sandstone bedrock of the Ozark Salem Plateau creating spectacular bluffs and incised meanders along the way.[11] Numerous springs and caves occur within the drainage area and along the river course. Significant tributaries include the Osage Fork of Webster and Laclede counties and Roubidoux Creek and Big Piney River of Texas and Pulaski counties. The Roubidoux and Big Piney flow respectively along the west and east boundaries of Fort Leonard Wood which lies a short distance south and east of the Gasconade.

The plateau surface near the midpoint is Шаблон:Convert above the river bottom near the river midpoint northeast of Waynesville creating scenic river bluffs.[12] At the junction with the Missouri the river bottom is about Шаблон:Convert lower in elevation than the old plateau surface above the river.[10] The elevation of the plateau rim at the headwaters is at or above Шаблон:Convert with local hilltops at over Шаблон:Convert (second highest elevation in Missouri near Cedar Gap). The elevation at the confluence with the Missouri is Шаблон:Convert giving an overall drainage basin relief of Шаблон:Convert.

The Gasconade River is the longest river completely within the boundary of Missouri. It has been called one of the world's crookedest rivers.[13]

Recreational use

It is ranked with a difficulty of I and II (seldom) by those who canoe, kayak and float.[14] It is considered a good float stream because there's typically not a heavy congestion of boats. It is common to go for many miles without seeing another boat.[15]

There are caves and an abundance of wildlife along the river and is considered a popular place by anglers for its largemouth bass and smallmouth bass.[15]

See also

Notes

Шаблон:Reflist

Sources

Шаблон:Authority control

  1. U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map Шаблон:Webarchive, accessed May 31, 2011
  2. Шаблон:Cite web
  3. 3,0 3,1 Шаблон:Cite web
  4. Шаблон:Cite GNIS
  5. Шаблон:Cite web
  6. Шаблон:Cite web
  7. Шаблон:Cite web
  8. Шаблон:Cite book
  9. USGS Mansfield NW 7.5 min. Quadrangle Topoquest
  10. 10,0 10,1 USGS Gasconade 7.5 min. Quad
  11. A. G. Unklesbay, Jerry D. Vineyard. Missouri Geology — Three Billion Years of Volcanoes, Seas, Sediments, and Erosion, University of Missouri Press, 1992. Шаблон:ISBN
  12. USGS Dixon 7.5 min. Quad
  13. Шаблон:Cite web
  14. Шаблон:Cite web
  15. 15,0 15,1 Шаблон:Cite web