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Cimarron Range

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The Sangre de Cristo Mountains ( Spanish for " Blood of Christ ") are the southernmost subrange of the Rocky Mountains . They are located in southern Colorado and northern New Mexico in the United States . The mountains run from Poncha Pass in South-Central Colorado , trending southeast and south, ending at Glorieta Pass , southeast of Santa Fe, New Mexico . The mountains contain a number of fourteen thousand foot peaks in the Colorado portion, as well as several peaks in New Mexico which are over thirteen thousand feet.

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48-604: Cimarron Range may refer to: Cimarron Range in the Sangre de Cristo Mountains in New Mexico Cimarron Ridge in the San Juan Mountains [REDACTED] Topics referred to by the same term This disambiguation page lists articles about distinct geographical locations with the same name. If an internal link led you here, you may wish to change

96-666: A National Natural Landmark in 1976 as one of the best known examples of igneous dikes . The mountains can be seen from as far as 133 mi (214 km) to the north from Colorado Springs , 65 mi (105 km) to the south from Raton, New Mexico , and 85 mi (137 km) to the east from La Junta, Colorado . The Culebra Range runs almost due north and south, with its northern limit at La Veta Pass in Colorado, and its southern limit at Costilla Creek , just south of Big Costilla Peak in New Mexico. Its highest point

144-645: A palaeochannel next to Nolan, a site in the Tensas Basin , show that part of the river's meander belt flowed through up to 3200 BCE. While it was previously thought that this relict channel was active at the same time as another relict of the Mississippi River 's meander belt, it has been shown that this channel of the Arkansas was inactive approximately 400 years before the Mississippi channel

192-631: A high ridge separating the San Luis Valley on the west from the watershed of the Arkansas River on the east. The Crestones are a group of four 14,000 feet (4,000 m)+ peaks ( fourteeners ) in the Sangre de Cristo Range above Crestone, Colorado . The Spanish Peaks are a pair of mountains, West Spanish Peak , 13,626 ft (4,153 m), and East Spanish Peak , 12,860 ft (3,920 m), located in southwestern Huerfano County , Colorado . The Spanish Peaks were designated

240-674: A rich agricultural history and has been the scene of land disputes between the descendants of Hispanic settlers and Anglo ranchers since the 1860s. The Taos Mountains span the western lobe of the range from Costilla Creek in the north, to Tres Ritos in the south. They include the highest point in New Mexico, Wheeler Peak , at 13,161 feet (4,011 m), which is part of the Wheeler Peak Wilderness . Other notable peaks include Pueblo Peak, which at 12,305 feet (3,751 m) rises dramatically above Taos Pueblo , and Latir Peak , at 12,708 feet (3,873 m). Williams Lake

288-563: Is Culebra Peak at 14,047 ft (4,282 m), which is notable for being the only fourteener in Colorado on private land with an access fee. Climbers wishing to ascend Culebra must pay a fee (currently US$ 150 per person), and the number of climbers per year is limited. It is also the most southerly fourteener in the U.S. Rockies. Standing to the east of the main crest are the two prominent Spanish Peaks (West: 13,626 ft (4,153 m), East: 12,860 ft (3,920 m)). These peaks were important landmarks for 19th century travelers on

336-558: Is located below Wheeler Peak in the Wheeler Peak Wilderness. Taos Ski Valley lies just to the west of Wheeler Peak. Much of the central portion of the Taos Mountains is on Taos Pueblo land. As viewed from Taos , they are locally called "Taos Mountain." The southern portion of the Taos Mountains, between Palo Flechado Pass and Tres Ritos ( U.S. Route 64 and NM Route 518), is lower and less dramatic than

384-601: The 100th meridian west formed part of the U.S.–Mexico border from the Adams–Onís Treaty (in force 1821) until the Texas Annexation or Treaty of Guadalupe Hidalgo . The river is alternatively pronounced / ɑːr ˈ k æ n z ə s / ar- KAN -zəs or / ˈ ɑːr k ən s ɔː / AR -kən-saw . The path of the Arkansas River has changed over time. Sediments from the river found in

432-539: The Cenozoic Laramide orogeny . They are bounded on the west by the Rio Grande rift and on the east by a series of reverse and thrust faults . Vertical displacement along the faults is at least 4,200 metres (13,800 ft), and gravity measurements suggest the uplift has been thrust eastward great distances. This faulting places Precambrian basement rock in contact with sedimentary strata along

480-663: The McClellan-Kerr Arkansas River Navigation System joins the Verdigris River. Into western Arkansas , the river path works between the encroaching Boston and Ouachita mountains, including many isolated, flat-topped mesas, buttes, or monadnocks such as Mount Nebo , Petit Jean Mountain , and Mount Magazine , the highest point in the state. The river valley expands as it encounters much flatter land beginning just west of Little Rock, Arkansas . It continues eastward across

528-481: The Mississippi River from Prairie du Chien, Wisconsin toward the Gulf of Mexico, but turned back at the mouth of the Arkansas River. By that time, they had encountered Native Americans carrying European trinkets and feared confrontation with Spanish conquistadors. Jean-Baptiste Bénard de la Harpe , a French trader, explorer, and nobleman had led an expedition into what is now Oklahoma in 1718–19. His original objective

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576-466: The Pecos River . The peaks include Truchas Peak , 13,102 ft (3,993 m), as their highest point. Other notable peaks are Santa Fe Baldy (12,622 ft (3,847 m)) and Jicarita Peak (12,835 ft (3,912 m)). The Pecos Wilderness is crossed by many trails and is popular for backpacking and for fishing in its high alpine lakes. The Sangre de Cristo Mountains were uplifted during

624-576: The Royal Gorge . At Cañon City, Colorado , the Arkansas River valley widens and flattens markedly. Just west of Pueblo, Colorado , the river enters the Great Plains . Through the rest of Colorado , Kansas , and much of Oklahoma , it is a typical Great Plains riverway, with wide, shallow banks subject to seasonal flooding and periods of dwindling flow. Tributaries include the Cimarron and

672-619: The Salt Fork Arkansas rivers. In eastern Oklahoma, the river begins to widen further into a more contained consistent channel. To maintain more reliable flow rates, a series of dams and large reservoir lakes have been built on the Arkansas and its intersecting tributaries, including the Canadian , Verdigris , Neosho (Grand) , Illinois , and Poteau rivers. These locks and dams enable the river to be navigable by barges and large river craft downriver of Muskogee, Oklahoma , where

720-566: The Sangre de Cristo Wilderness in Colorado and the Pecos Wilderness in New Mexico, as well as some smaller wilderness areas, such as Latir Peak Wilderness . The Great Sand Dunes National Park and Preserve lies on the southwest side of the mountains in Colorado and are managed by the National Park Service. The Sangre de Cristo Mountains are divided into various subranges, described here from north to south. Use of

768-541: The Santa Fe Trail followed the Arkansas through much of Kansas, picking it up near Great Bend and continuing through to La Junta, Colorado . Some users elected to take the challenging Cimarron Cutoff starting at Cimarron, Kansas . During the American Civil War, each side tried to prevent the other from using the Arkansas River and its tributaries as a route for moving reinforcements. Initially,

816-620: The Tulsa Port of Catoosa on the Verdigris River , enters the Arkansas River near Muskogee, and runs via an extensive lock and dam system to the Mississippi River. Through Oklahoma and Arkansas, dams which artificially deepen and widen the river to sustain commercial barge traffic and recreational use give the river the appearance of a series of reservoirs. The McClellan–Kerr Arkansas River Navigation System diverts from

864-794: The snowpack in the Sawatch and Mosquito mountain ranges. It flows east into Kansas and finally through Oklahoma and Arkansas, where it meets the Mississippi River. At 1,469 miles (2,364 km), it is the sixth-longest river in the United States , the second-longest tributary in the Mississippi– Missouri system, and the 47th longest river in the world . Its origin is in the Rocky Mountains in Lake County, Colorado , near Leadville . In 1859, placer gold discovered in

912-601: The Arkansas River 2.5 mi (4.0 km) upstream of the Wilbur D. Mills Dam to avoid the long winding route which the lower Arkansas River follows. This circuitous portion of the Arkansas River between the Wilbur D. Mills Dam and the Mississippi River was historically bypassed by river vessels. Early steamboats instead followed a network of rivers—known as the Arkansas Post Canal—;which flowed north of

960-572: The Arkansas River as a supply route. In September 1864, a body of Confederate irregulars led by General Stand Watie (Cherokee) successfully ambushed a Union supply ship bound for Fort Gibson. The vessel was destroyed, and a part of its cargo was looted by the Confederates. By 1890, water from the Arkansas River was being used to irrigate more than 20,000 acres (8,100 ha) of farmland in Kansas. By 1910, irrigation projects in Colorado had caused

1008-540: The Arkansas River for thousands of years. The first Europeans to see the river were members of the Spanish Coronado expedition on June 29, 1541. Also in the 1540s, Hernando de Soto discovered the junction of the Arkansas with the Mississippi. The Spanish originally called the river Napeste . "The name "Arkansas" was first applied by French Father Jacques Marquette , who called the river Akansa in his journal of 1673. The Joliet-Marquette expedition travelled

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1056-491: The Arkansas River in central Colorado have been known for exceptional trout fishing, particularly fly fishing , since the 19th century, when greenback cutthroat trout dominated the river. Today, brown trout dominate the river, which also contains rainbow trout . Trout Unlimited considers the Arkansas one of the top 100 trout streams in America, a reputation the river has had since the 1950s. From Leadville to Pueblo,

1104-425: The Arkansas River include Canon City , Pueblo , La Junta , and Lamar, Colorado ; Garden City , Dodge City , Hutchinson , and Wichita, Kansas ; Tulsa, Oklahoma ; and Fort Smith and Little Rock, Arkansas . The May 2002 I-40 bridge disaster took place on I-40 's crossing of Kerr Reservoir on the Arkansas River near Webbers Falls, Oklahoma . Since 1902, Kansas has claimed that Colorado takes too much of

1152-537: The Arkansas River is serviced by numerous fly shops and guides operating in Buena Vista, Salida, Cañon City, and Pueblo. Colorado Parks and Wildlife provides regular online fishing reports for the river. A fish kill occurred on December 29, 2010, in which an estimated 100,000 freshwater drum lined the Arkansas River bank . An investigation, conducted by the Arkansas Game and Fish Commission, found

1200-661: The Arkansas River, reaching a place called Arkansas Post , about 60 miles (97 km) above the confluence of the Arkansas and the Mississippi rivers. In mid-April 1822, the Robert Thompson , towing a keelboat, was the first steamboat to navigate the Arkansas as far as Fort Smith. For five years, Fort Smith was known as the head of navigation for steamboats on the river. It lost the title to Fort Gibson in April 1832, when three steamboats, Velocipede , Scioto, and Catawba , all arrived at Fort Gibson later that month. Later,

1248-475: The Arkansas. These included flatboats ( bateaus ) and keelboats . Along with the pirogues, they transported piles of deer, bear, otter, beaver, and buffalo skins up and down the river. Agricultural products such as corn, rice, dried peaches, beans, peanuts, snakeroot, sarsaparilla, and ginseng had grown in economic importance. On March 31, 1820, the Comet became the first steamboat to successfully navigate part of

1296-552: The Leadville area brought thousands seeking to strike it rich, but the easily recovered placer gold was quickly exhausted. The Arkansas River's mouth is at Napoleon, Arkansas , and its drainage basin covers nearly 170,000 square miles (440,000 km ). Its volume is much smaller than the Missouri and Ohio rivers, with a mean discharge of about 40,000 cubic feet per second (1,100 m /s). The Arkansas from its headwaters to

1344-656: The Union Army abandoned its forts in the Indian Territory, including Fort Gibson and Fort Smith, to maximize its strength for campaigns elsewhere. The Confederate Army sent troops from Texas to support its Native American allies. Union troops returned to the area later in the war, after defeating the Confederates at the Battle of Pea Ridge and the Battle of Fort Smith . They began recovering the position it had previously abandoned, most notably Fort Gibson and reopened

1392-692: The United States annexed Texas after the Mexican–American War , in 1846. The treaty was made shortly after the "Old Settler" Cherokee were pushed out of Texas and moved near what became known as Webbers Falls on the Arkansas River. They planned to reunite with the Cherokee who had moved there on the Trail of Tears in 1839. That area, then part of Arkansas Territory , would become Indian Territory and later Oklahoma . This area had long been

1440-494: The areas around the Great Lakes began exploring the Mississippi and some of its northern tributaries. They soon learned that the birchbark canoes, which had served them so well on the northern waterways, were too light for use on southern rivers such as the Arkansas. They turned to making and using dugout canoes, which they called pirogues , made by hollowing out the trunks of cottonwood trees. Cottonwoods are plentiful along

1488-603: The compact did not stop further disputes by the two states over water rights to the river. The Kansas–Oklahoma Arkansas River Basin Compact was created in 1965 to promote mutual consideration and equity over water use in the basin shared by those states. The Kansas–Oklahoma Arkansas River Commission was established, charged with administering the compact and reducing pollution. The compact was approved and implemented by both states in 1970 and has been in force since then. The McClellan–Kerr Arkansas River Navigation System begins at

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1536-607: The east side of the Cimarron Range. This is a minor subrange, significantly lower than the rest of the Sangre de Cristos; it lies east of the southernmost portion of the Taos Mountains. Rounding out the Sangre de Cristo Mountains are the Santa Fe Mountains, which include all peaks south of NM Route 518. This group lies near Santa Fe and surrounds the Pecos Wilderness , which protects the source watershed of

1584-514: The eastern margin of the uplift except where igneous rocks have been intruded along the fault. Arkansas River The Arkansas River is a major tributary of the Mississippi River . It generally flows to the east and southeast as it traverses the U.S. states of Colorado , Kansas , Oklahoma , and Arkansas . The river's source basin lies in Colorado, specifically the Arkansas River Valley. The headwaters derive from

1632-628: The last words of a priest who was killed by Native Americans. Much of the mountains are within various National Forests: the Rio Grande and San Isabel in Colorado, and the Carson and Santa Fe in New Mexico. These publicly accessible areas are managed by the United States Forest Service and are popular for hunting , camping , hiking , mountain biking , backpacking , climbing , and cross-country and downhill skiing . The mountains include two large wilderness areas ,

1680-419: The link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Cimarron_Range&oldid=952342460 " Category : Place name disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages Sangre de Cristo Mountains#Cimarron Range The name of

1728-580: The lower Arkansas River and followed a shorter and more direct route to the Mississippi River. When the McClellan–Kerr Arkansas River Navigation System was constructed between 1963 and 1970, the Arkansas Post Canal was significantly improved, while the lower Arkansas River continued to be bypassed by commercial vessels. Many nations of Native Americans lived near, or along, the 1,450-mile (2,334-km) stretch of

1776-491: The mountain branch of the Santa Fe Trail . The western slope of the Culebras and the San Luis Valley are located within the Sangre de Cristo Land Grant , dating back to the 1840s but still a factor in the pattern of land ownership within the grant. The San Luis Valley is arid. The town of San Luis, Colorado has an annual precipitation of only 9.6 inches (240 mm).The surrounding area, traversed by Culebra Creek , has

1824-457: The mountains may refer to the occasional reddish hues observed during sunrise and sunset, and when alpenglow occurs, especially when the mountains are covered with snow. Although the particular origin of the name is unclear, it has been in use since the early 19th century. Before that time the terms "La Sierra Nevada", "La Sierra Madre", "La Sierra", and "The Snowies" (used by English speakers) were used. According to legend, "sangre de Cristo" were

1872-470: The northern section, with its high point being Cerro Vista, 11,939 ft (3,639 m). The Fernando Mountains are a small subrange lying in this section, just south of US Route 64. The Cimarron Range lies across the Moreno Valley to the east of the Taos Mountains. It is a lower range, with its highest point being Baldy Mountain at 12,441 ft (3,792 m). The Philmont Scout Ranch lies on

1920-480: The plains and forests of eastern Arkansas until it flows into the Mississippi River near Napoleon, Arkansas . Water flow in the Arkansas River (as measured in central Kansas ) has dropped from approximately 248 cubic feet per second (7.0 m /s) average from 1944–1963 to 53 cubic feet per second (1.5 m /s) average from 1984–2003, largely because of the pumping of groundwater for irrigation in eastern Colorado and western Kansas . Important cities along

1968-613: The river to stop flowing in July and August. Flooding in 1927 severely damaged or destroyed nearly every levee downstream of Fort Smith, and led to the development of the Arkansas River Flood Control Association. It also resulted in the Federal government assigning responsibility for flood control and navigation on the Arkansas River to the U.S. Army Corps of Engineers (USACOE). The headwaters of

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2016-481: The river's water; it has filed numerous lawsuits over this issue in the U.S. Supreme Court that continue to this day, generally under the name of Kansas v. Colorado . The problems over the possession and use of Arkansas River water by Colorado and Kansas led to the creation of an interstate compact or agreement between the two states. While Congress approved the Arkansas River Compact in 1949,

2064-530: The strangers a warm welcome. La Harpe's party was honored with the calumet ceremony and spent ten days at this location. In 1988, evidence of a native village was discovered along the Arkansas River 13 miles (21 km) south of present-day Tulsa, Oklahoma . By then, the site was known as the Lasley Vore Site . French traders and trappers who had opened up trade with Indian tribes in Canada and

2112-521: The streams of the southwest and grow to large sizes. The wood is soft and easily worked with the crude tools carried by both the French and Indians. The pirogues were sturdier and could be more useful for navigating the sandbars and snags of the Southern waterways. In 1819, the Adams–Onís Treaty set the Arkansas as part of the frontier between the United States and Spanish Mexico . This continued until

2160-549: The terms "Sangre de Cristo Range" and "Sangre de Cristo Mountains" is inconsistent and may refer to the northernmost subrange, the southernmost subrange, or the mountains as a whole. The Sangre de Cristo Range, the largest and most northerly subrange of the Sangre de Cristo Mountains, runs directly along the east side of the Rio Grande rift , extending southeast from Poncha Pass for about 75 miles (120 km) through south-central Colorado to La Veta Pass , approximately 20 miles (32 km) west of Walsenburg . They form

2208-534: The traditional territory of the Osage . They resisted the new Native Americans moving in with armed conflict. The US encouraged a peace treaty made in 1828 but the territory issue was still unresolved by the time thousands of additional Cherokee refugees moved to the area during the Trail of Tears . By the time Fort Smith was established in 1817, larger capacity watercraft became available to transport goods up and down

2256-505: Was active. The Arkansas has three distinct sections in its long path through central North America. At its headwaters beginning near Leadville , Colorado , the Arkansas runs as a steep fast-flowing mountain river through the Rockies in its narrow valley, dropping 4,600 feet (1,400 m) in 120 miles (190 km). This section supports extensive whitewater rafting , including The Numbers (near Granite, Colorado ), Brown's Canyon , and

2304-463: Was to establish a trading post near the present city of Texarkana, Arkansas , but he extended his trip overland as far north as the Arkansas River (which he designated as the Alcansas ). The explorer wrote that he and nine other men, including three Caddo guides and 22 horses loaded with trade goods, had come to a native settlement overlooking the river, where there were about 6,000 natives, who gave

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