The Gasconade River begins in the Ozarks southeast 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.
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 . The river joins the Missouri River at the city of Gasconade at . The river follows a meandering course through the Ordovician age dolostone and sandstone bedrock of the Ozark Salem Plateau creating spectacular bluffs and incised meanders along the way. 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 300 feet (91 m) above the river bottom near the river midpoint northeast of Waynesville creating scenic river bluffs. At the junction with the Missouri the river bottom is about 400 feet (120 m) lower in elevation than the old plateau surface above the river. The elevation of the plateau rim at the headwaters is at or above 1,600 feet (490 m) with local hilltops at over 1,700 feet (520 m) (second highest elevation in Missouri near Cedar Gap). The elevation at the confluence with the Missouri is 500 feet (150 m) giving an overall drainage basin relief of 1,200 feet (370 m).
The Gasconade River is the longest river completely within the boundary of Missouri. It has been called one of the world's crookedest rivers.
It is ranked with a difficulty of I and II (seldom) by those who canoe, kayak and float. 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.
- U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map, accessed May 31, 2011
- http://reference.allrefer.com/gazetteer/G/G00936-gasconade-river.html, http://southwestpaddler.com/docs/missouri6b.html
- http://geonames.usgs.gov/pls/gnispublic/f?p=gnispq:3:1414915318411313::NO::P3_FID:750029, http://southwestpaddler.com/docs/missouri6b.html, http://www.missouricanoe.org/river-maps/gasconade.html
- USGS Mansfield NW 7.5 min. Quadrangle Topoquest
- USGS Gasconade 7.5 min. Quad
- A. G. Unklesbay, Jerry D. Vineyard. Missouri Geology — Three Billion Years of Volcanoes, Seas, Sediments, and Erosion, University of Missouri Press, 1992. ISBN 0-8262-0836-3
- USGS Dixon 7.5 min. Quad
- "Gasconade River, Missouri". Southwestpaddler.com. Retrieved 2012-08-17.
- "Missouri's Gasconade River". Missouricanoe.org. Retrieved 2012-08-17.
- [dead link]
- Columbia Gazetteer of North America entry
- DeLorme (2002). Missouri Atlas & Gazetteer. Yarmouth, Maine: DeLorme. ISBN 0-89933-353-2.
- U.S. Geological Survey Geographic Names Information System: Gasconade River
- Missouri Canoe - an electronic reprint of a Missouri Department of Conservation document
- Southwest Paddler
- Canoe Missouri