Canadian River: Difference between revisions
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==Passage== |
==Passage== |
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The river rises on the east side of the [[Sangre de Cristo Mountains]], at approximately {{convert|9600|ft|m|abbr=on}},<ref>{{GNIS|1101881|Canadian River}}</ref> in remote southwestern [[Las Animas County, Colorado]], approximately 1.5 mi (2.5 km) north of the [[New Mexico]] border. It flows ESE across the border, then south, passing west of [[Raton, New Mexico]]. It forms a deep canyon south of [[Springer, New Mexico]]. At its first [[dam]] at [[Conchas Lake]], the river turns eastward. It is also dammed at [[Logan, New Mexico]], where it forms [[Ute Lake]]. From there it crosses the [[Texas Panhandle]], dammed at [[Sanford, Texas]], where it forms [[Lake Meredith]]. The canyon the river carves through eastern New Mexico and the Texas Panhandle is the northern border of the [[Llano Estacado]], separating it from the rest of the [[Great Plains]]. From Texas the Canadian continues eastward into Oklahoma, passing just south of [[Oklahoma City, Oklahoma|Oklahoma City]]. At [[Eufaula, Oklahoma]], it is dammed once again, forming [[ |
The river rises on the east side of the [[Sangre de Cristo Mountains]], at approximately {{convert|9600|ft|m|abbr=on}},<ref>{{GNIS|1101881|Canadian River}}</ref> in remote southwestern [[Las Animas County, Colorado]], approximately 1.5 mi (2.5 km) north of the [[New Mexico]] border. It flows ESE across the border, then south, passing west of [[Raton, New Mexico]]. It forms a deep canyon south of [[Springer, New Mexico]]. At its first [[dam]] at [[Conchas Lake]], the river turns eastward. It is also dammed at [[Logan, New Mexico]], where it forms [[Ute Lake]]. From there it crosses the [[Texas Panhandle]], dammed at [[Sanford, Texas]], where it forms [[Lake Meredith]]. The canyon the river carves through eastern New Mexico and the Texas Panhandle is the northern border of the [[Llano Estacado]], separating it from the rest of the [[Great Plains]]. From Texas the Canadian continues eastward into Oklahoma, passing just south of [[Oklahoma City, Oklahoma|Oklahoma City]]. At [[Eufaula, Oklahoma]], it is dammed once again, forming [[Lake]], its largest. About {{convert|20|mi|km}} downstream it joins the Arkansas River, about {{convert|40|mi|km}} west of the [[Arkansas]] border. |
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Much of the time the Canadian is just a slow trickle bounded by red mud flats and [[quicksand]]. When sufficient [[rain]] has fallen, the river can carry substantial amounts of water. |
Much of the time the Canadian is just a slow trickle bounded by red mud flats and [[quicksand]]. When sufficient [[rain]] has fallen, the river can carry substantial amounts of water. |
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Revision as of 04:17, 5 August 2009
The Canadian River is the largest tributary of the Arkansas River. It is about 906 miles (1,458 km) long, starting in Colorado and traveling through New Mexico, the Texas Panhandle, and most of Oklahoma.
The Canadian is sometimes referred to as the South Canadian River to differentiate it from the North Canadian River that flows into it.
Passage
The river rises on the east side of the Sangre de Cristo Mountains, at approximately 9,600 ft (2,900 m),[1] in remote southwestern Las Animas County, Colorado, approximately 1.5 mi (2.5 km) north of the New Mexico border. It flows ESE across the border, then south, passing west of Raton, New Mexico. It forms a deep canyon south of Springer, New Mexico. At its first dam at Conchas Lake, the river turns eastward. It is also dammed at Logan, New Mexico, where it forms Ute Lake. From there it crosses the Texas Panhandle, dammed at Sanford, Texas, where it forms Lake Meredith. The canyon the river carves through eastern New Mexico and the Texas Panhandle is the northern border of the Llano Estacado, separating it from the rest of the Great Plains. From Texas the Canadian continues eastward into Oklahoma, passing just south of Oklahoma City. At Eufaula, Oklahoma, it is dammed once again, forming Lake Eufaula, its largest. About 20 miles (32 km) downstream it joins the Arkansas River, about 40 miles (64 km) west of the Arkansas border.
Much of the time the Canadian is just a slow trickle bounded by red mud flats and quicksand. When sufficient rain has fallen, the river can carry substantial amounts of water.
Name origin
It is unclear why the river is called the Canadian. The name may have been given to the river by early French hunters and traders who came from Canada. The upper part was called Rio Colorado by the Spanish. Some researchers think early explorers believed the river flowed into Canada. It does flow northeast through part of the Texas Panhandle. In 1929 Muriel H. Wright wrote that the Canadian River was named about 1820 by French traders who noted another group of traders from Canada had camped on the river near its confluence with the Arkansas River.[2]
The name could be of Spanish origin from the word cañada (meaning canyon), as the Canadian River formed a steep canyon in northern New Mexico and a somewhat broad canyon in Texas. A few historical records document this explanation. Generally, the French origin of the name is considered more probable.[3]
By the Treaty of Doak's Stand in 1820, the Canadian River was made the northern boundary of the Choctaw Nation. Early emigrants to California followed the south bank of the Canadian to Santa Fe. In 1845 the river was explored by Lieutenants James William Abert and William G. Peck of the U.S. Army Corps of Topographical Engineers. Their journey was chronicled in the Journal of Lieutenant J.W. Abert from Bent’s Fort to St. Louis, first published in 1846. The Texas Ranger Division also was active in the area.
See also
References
- ^ U.S. Geological Survey Geographic Names Information System: Canadian River
- ^ Wright, Muriel H. "Some Geographic Names of French Origin in Oklahoma", Chronicles of Oklahoma, 7(2):188-193, June 1929.
- ^ Hale, Edward E. "French Place-Names in New Mexico", French Review, 3(2):110-112, November 1929.
External links
- "Canadian River", Handbook of Texas Online
- Sketch of the Canadian River from A pictorial history of Texas, from the earliest visits of European adventurers, to A.D. 1879, Portal to Texas History, University of Texas.