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79-505: Geologically, the Rio Grande Gorge is a canyon, carved out by erosion over the last several million years. The Rio Grande Gorge and its river follow a topographical low within the larger Rio Grande Rift ; a mixture of volcanic activity, shifting tectonic plates, and erosion of layers of gravels and lava yielded the recognizable narrow, deep gorge visible today. The canyon ecosystem descends 800 feet (240 m) from rim to river, creating

158-637: A channel was dug for flood control which moved the river, creating what was called Cordova Island, which became the center of the Chamizal dispute . Resolving the dispute took many years and resulted in a 1909 combined assassination attempt on the American and Mexican presidents. Following the approval of the Rio Grande Project by federal lawmakers in 1905, the waters of the Rio Grande were to be divided between

237-429: A downward hinge on the other. Which side of the basin has the major fault or the hinge alternates along the rift. The alternation between these half-grabens occurs along transfer faults, which trend across the rift to connect the major basin-bounding faults and occur between basins or, in places, within basins. The Precambrian basement changes relief sharply in this area, from 8,700 metres (28,500 ft) below sea level at

316-409: A large swing bridge , dates back to 1910 and is still in use today by automobiles connecting Brownsville with Matamoros, Tamaulipas . The swing mechanism has not been used since the early 1900s, though, when the last of the big steamboats disappeared. At one point, the bridge also had rail traffic. Railroad trains no longer use this bridge. A new rail bridge (West Rail International Crossing) connecting

395-448: A long time, because it provides a north–south route that follows a major river. The Rio Grande follows the course of the rift from southern Colorado to El Paso, where it turns southeast and flows toward the Gulf of Mexico . Important cities, including Albuquerque , Santa Fe , Taos , Española , Las Cruces , El Paso , and Ciudad Juárez , lie within the rift. The Rio Grande rift represents

474-532: A playa in the southern Albuquerque Basin where it deposited the Popotosa Formation . The upper reach of this river corresponded to the modern Rio Chama , but by 5 million years ago, an ancestral Rio Grande draining the eastern San Juan Mountains had joined the ancestral Rio Chama. The ancestral Rio Grande progressively integrated basins to the south, reaching the Mesilla Basin by 4.5 million years and

553-412: A pure-shear rifting mechanism, in which both sides of the rift pull apart evenly and slowly, with the lower crust and upper mantle (the lithosphere ) stretching like taffy . This extension is associated with very low seismic velocities in the upper mantle above approximately 400 kilometres (250 mi) depth associated with relatively hot mantle and low degrees of partial melting. This intrusion of

632-580: A royal Spanish cartographer. In the autumn of 1540, a military expedition of the Viceroyalty of New Spain led by Francisco Vásquez de Coronado , Governor of Nueva Galicia , reached the Tiwa pueblos along the Rio Grande in the future New Mexico . On July 12, 1598, Don Juan de Oñate y Salazar established the New Spain colony of Santa Fe de Nuevo Méjico at the new village of San Juan de los Caballeros adjacent to

711-638: A single river system draining into the Gulf of Mexico until relatively recent geologic time. Instead, the basins formed by the opening of the Rio Grande rift were initially bolsons , with no external drainage and a central playa . An axial river existed in the Espanola Basin as early as 13 million years ago, reaching the Santo Domingo Basin by 6.9 million years ago. However, at this time, the river drained into

790-420: A small, sandy delta at the Gulf of Mexico. During portions of 2001 and 2002, the mouth of the Rio Grande was blocked by a sandbar. In the fall of 2003, the sandbar was cleared by high river flows around 7,063 cubic feet per second (200 m /s). The Rio Grande flows through a valley with diverse animal and plants communities. Conservation of the river and the valley is a recurring theme for people who live in

869-515: A unique diversity in plant and animal life. Ancient piñon and juniper forests are home to 500-year-old trees. Wildlife include mule deer, red-tailed hawk, mountain blue-bird, prairie dog and big horn sheep. The climate is semi-arid with summer thunderstorms common in July and August, and snow possible from November through March. Summer temperatures range from 45 to 90 °F (7 to 32 °C) and in winter from −15 to 45 °F (−26 to 7 °C). In 1968,

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948-522: A year later, in October 2022, the reservoir had made only insignificant rebounds, resting at 6.4% of capacity. In late July 2022, due to extreme drought, the Rio Grande ran dry for about 50 miles in the middle Rio Grande Valley , including five miles in Albuquerque, the first time it had done so in over 40 years. The following winter, the basin experienced above-average snowfall, leading to very high flows in

1027-719: Is a north-trending continental rift zone. It separates the Colorado Plateau in the west from the interior of the North American craton on the east. The rift extends from central Colorado in the north to the state of Chihuahua , Mexico , in the south. The rift zone consists of four basins that have an average width of 50 kilometres (31 mi). The rift can be observed on location at Rio Grande National Forest , White Sands National Park , Santa Fe National Forest , and Cibola National Forest , among other locations. The Rio Grande rift has been an important site for humans for

1106-512: Is better in flanking basins of the Rio Grande Valley, where numerous Folsom sites and a much smaller number of earlier Clovis sites have been identified. Later Paleo-Indian groups included the Belen and Cody cultures, who appear to have taken advantage of the Rio Grande Valley for seasonal migrations and may have settled more permanently in the valley. The Paleo-Indian cultures gave way to

1185-400: Is fairly complex. The fundamental change in the western margin of the North American plate from one of subduction to a transform boundary occurred during Cenozoic time. The Farallon plate continued to be subducted beneath western North America for at least 100 million years during Late Mesozoic and early Cenozoic time. Compressional and transpressional deformation incurred by

1264-524: Is in the south. The crustal thickness underneath the rift is on average 30–35 kilometres (19–22 mi), thinner by 10–15 kilometres (6.2–9.3 mi) than the Colorado Plateau on the west and the Great Plains to the east. Formation of the rift began with significant deformation and faulting with offsets of many kilometers starting about 35 Ma. The largest-scale manifestation of rifting involves

1343-662: Is intersected in northern New Mexico by the NE-SW trending Jemez Lineament which extends well into Arizona . The lineament is defined by aligned volcanic fields and several calderas in the area, including the Valles Caldera National Preserve in the Jemez Mountains . The Jemez Lineament is thought to be a hydrous subduction zone scar, separating Precambrian basement rock of the Yavapai - Mazatzal transition zone from

1422-537: Is not part of the Water Authority's long-term resource management plan, dubbed WATER 2120. Dams on the Rio Grande include Rio Grande Dam , Cochiti Dam , Elephant Butte Dam , Caballo Dam , Amistad Dam , Falcon Dam , Anzalduas Dam , and Retamal Dam . In southern New Mexico and the upper portion of the Texas border segment, the river's discharge dwindles. Diversions, mainly for agricultural irrigation, have increased

1501-728: Is one of the principal rivers (along with the Colorado River ) in the Southwestern United States and in northern Mexico . The length of the Rio Grande is 1,896 miles (3,051 km), making it the 4th longest river in the United States and in North America by main stem. It originates in south-central Colorado , in the United States, and flows to the Gulf of Mexico . The Rio Grande drainage basin (watershed) has an area of 182,200 square miles (472,000 km ); however,

1580-450: Is responsible for anomalously high earthquake activity in the vicinity, including the largest rift-associated earthquakes in historic times (two events of approximately magnitude 5.8) in July and November 1906. Earth and space-based geodetic measurements indicate ongoing surface uplift above the Socorro magma body at approximately 2 mm/year. The Rio Grande rift's tectonic evolution

1659-455: Is the oldest of the three major basins, and contains 7,350 metres (24,110 ft) of Paleogene clastic sediments deposited on Precambrian basement. The southernmost Albuquerque basin contains pre-rift volcanic deposits , while the central and northern portions contain volcanics erupted during rifting. In cross-section, the geometry of the basins within the rift are asymmetrical half-grabens , with major fault boundaries on one side and

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1738-562: Is unavailable for storage, reducing system capacity by about 180,000 acre-feet. MRGCD has requested storage of "native water" downstream at Abiquiu Reservoir , which normally only stores waters imported into the Rio Grande watershed from the Colorado River watershed via the San Juan–Chama Project . Elephant Butte Reservoir , the main storage reservoir on the Rio Grande, was reported at 13.1% of capacity as of May 1, 2022, further decreasing to only 5.9% full by November 2021. Nearly

1817-755: The Apollo Astronauts at the site in March and Sept. 1971, because of the striking similarities to the Apollo 15 landing site. Astronauts who would use this training on the Moon included Apollo 15 's David Scott and James Irwin , Apollo 16 's John Young and Charlie Duke , and Apollo 17 's Jack Schmitt . Notable geologist instructors included William R. Muehlberger . 36°28′35″N 105°44′02″W  /  36.47652°N 105.73380°W  / 36.47652; -105.73380 Rio Grande Rift The Rio Grande rift

1896-675: The Archaic Oshara tradition beginning around 5450 BCE. The Oshara began cultivation of maize between 1750 and 750 BCE, and their settlements became larger and more permanent. Drought induced the collapse of the Ancestral Puebloan culture, at Chaco Canyon and elsewhere across the Four Corners region, at around 1130 CE. This led to a mass migration of the Ancestral Puebloans to the Rio Grande and other more fertile valleys of

1975-837: The Colorado River basin via the San Juan-Chama Diversion Project and from the Rio Chama . The Rio Grande then continues southwards, irrigating the farmlands in the Middle Rio Grande Valley through the desert cities of Albuquerque and Las Cruces in New Mexico, to El Paso, Texas and Ciudad Juárez, Chihuahua , in Mexico. In the Albuquerque metropolitan area , the Rio Grande flows by historic Pueblo villages, such as Sandia Pueblo and Isleta Pueblo . South of El Paso,

2054-556: The International Boundary and Water Commission (IBWC), US–Mexico. The most notable of these treaties were signed in 1906 and 1944. The IBWC traces its institutional roots to 1889, when the International Boundary Committee was established to maintain the border. The IBWC today also allocates river waters between the two nations and provides for flood control and water sanitation. Use of that water belonging to

2133-553: The Laramide Orogeny lasted until about 40  Ma in New Mexico. This deformation may have been a result of the coupling between the subducting Farallon plate and the overlying North American Plate . Crustal thickening occurred due to Laramide compression. After the Laramide Orogeny and until 20 Ma, a major period of volcanic activity occurred throughout the southwestern United States. Injection of hot magmas weakened

2212-638: The Ohio and Mississippi Rivers were requisitioned by the U.S. government and moved to the Rio Grande during the Mexican–American War in 1846. They provided transport for the U.S. Army, under General Zachary Taylor , to invade Monterrey , Nuevo León , via Camargo Municipality, Tamaulipas . Army engineers recommended that with small improvements, the river could easily be made navigable as far north as El Paso. Those recommendations were never acted upon. The Brownsville & Matamoros International Bridge ,

2291-575: The Ohkay Owingeh Pueblo at the confluence of the Rio Grande and the Río Chama . During the late 1830s and early 1840s, the river marked the disputed border between Mexico and the nascent Republic of Texas ; Mexico marked the border at the Nueces River . The disagreement provided part of the rationale for the Mexican–American War in 1846, after Texas had been admitted as a new state. Since 1848,

2370-625: The Pecos River and Devils River , both entering the Rio Grande from the north in the vicinity of Amistad Reservoir in Texas, and the Rio Salado and Rio San Juan both entering from the south with confluences in Tamaulipas , Mexico. The Rio Grande rises in high mountains and flows for much of its length at high elevation; the valley floor at Albuquerque is 5,312 feet (1,619 m), and El Paso 3,762 feet (1,147 m) above sea level . In New Mexico,

2449-630: The Pueblo and Navajo peoples also have had names for the Rio Grande/Rio Bravo: The four Pueblo names likely antedated the Spanish entrada by several centuries. Rio del Norte was most commonly used for the upper Rio Grande (roughly, within the present-day borders of New Mexico) from Spanish colonial times to the end of the Mexican period in the mid-19th century. This use was first documented by

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2528-753: The Rio Grande Gorge , and fully reintegrated the San Luis Basin into the Rio Grande watershed. Archeological sites from the earliest human presence in the Rio Grande Valley are scarce, due to traditional Indigenous nomadic culture, Pleistocene and Holocene river incision or burial under the Holocene floodplain. However, some early sites are preserved on West Mesa on the west side of the Rio Grande near Albuquerque. These include Folsom sites, possibly dating from around 10,800 to 9,700 BCE, that were probably short-term sites such as buffalo kill sites. Preservation

2607-774: The Rio Grande was among the first eight rivers the US Congress designated into the National Wild and Scenic Rivers System to protect outstanding resources values. The Wild and Scenic River flows through the Rio Grande Gorge Recreation Area. The recreation areas include the Wild Rivers area in the north and the Orilla Verde area in the south, which provide hiking, boating, fishing and camping facilities. The gorge and 242,500 acres (98,100 ha) of surrounding land

2686-472: The US Navy . It was a shallow-draft river port, with several smaller vessels that hauled cargo to and from the deeper-draft cargo ships anchored off shore. These deeper-draft ships could not cross the shallow sandbar at the mouth of the river. The port's commerce was European military supplies, in exchange for bales of cotton. The sedimentary basins forming the modern Rio Grande Valley were not integrated into

2765-607: The asthenosphere into the lithosphere and continental crust is thought to be responsible for nearly all of the volcanism associated with the Rio Grande rift. The sedimentary fill of the basins consists largely of alluvial fan and mafic volcanic flows. The most alkalic lavas erupted outside the rift. The sediments that were deposited during rifting are commonly known as the Santa Fe Group . This group contains sandstones , conglomerates , and volcanics. Aeolian deposits are also present in some basins. The Rio Grande rift

2844-411: The endorheic basins that are adjacent to and within the greater drainage basin of the Rio Grande increase the total drainage-basin area to 336,000 square miles (870,000 km ). The Rio Grande with its fertile valley , along with its tributaries, is a vital water source for seven US and Mexican states, and flows primarily through arid and semi-arid lands. After traversing the length of New Mexico ,

2923-407: The lithosphere was hot, the brittle-ductile transition was relatively shallow. There is evidence that the second period of extension began earlier in the central and northern Rio Grande rift than in the south. A third period of extension may have begun in the early Pliocene . One theory is that the Colorado Plateau acts as a semi-independent microplate and one way of explaining the creation of

3002-441: The southwestern willow flycatcher . The water of the Rio Grande is over-appropriated: that is, more users for the water exist than water in the river. Because of both drought and overuse, the section from Las Cruces downstream through Ojinaga frequently runs dry and was recently tagged "The Forgotten River" by those wishing to bring attention to the river's deteriorated condition. In 2022, due to increasing drought and water use,

3081-544: The 1890s, the Rio Grande flowed through Las Cruces from February to October each year, but this is subject to climate change. In 2020, the river flowed only from March to September. As of January 2021, the Elephant Butte Irrigation District (Ebid) expected that water shortages would mean the river only flows through Las Cruces from June through July. The water shortages are affecting the local ecosystem and endangering species including cottonwood trees and

3160-744: The Brownsville and Matamoros Bridge Company, a joint venture between the Mexican government and the Union Pacific Railroad . At the mouth of the Rio Grande, on the Mexican side, was the large commercial port of Bagdad, Tamaulipas . During the American Civil War , this was the only legitimate port of the Confederacy. European warships anchored offshore to maintain the port's neutrality, and managed to do so successfully throughout that conflict, despite occasional stare-downs with blockading ships from

3239-639: The Mazaztl Province proper. Also on the Colorado Plateau but further north lies the San Juan volcanic field in the San Juan Mountains of Colorado. The youngest eruptions in the rift region are in the Valley of Fires , New Mexico, and are approximately 5,400 years old. The Socorro, New Mexico , region of the central rift hosts an inflating mid-crustal sill-like magma body at a depth of 19 km that

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3318-595: The Palomas basin by 3.1 million years ago, forming Lake Palomas . River capture by a tributary of the Pecos River then occurred, with the Rio Grande flowing to Texas by 2.06 million years, and finally joining the Pecos River 800,000 years ago, which drained into the Gulf of Mexico. Volcanism in the Taos Plateau reduced drainage from the San Luis Basin until a spillover event 440,000 years ago that drained Lake Alamosa , forming

3397-472: The Rio Grande becomes the Mexico–United States border , between the U.S. state of Texas and the northern Mexican states of Chihuahua and Coahuila , Nuevo León and Tamaulipas ; a short segment of the Rio Grande is a partial state-boundary between the U.S. states of New Mexico and Texas. Since the mid–twentieth century, only 20 percent of the Rio Grande's water reaches the Gulf of Mexico, because of

3476-482: The Rio Grande farther north in Colorado and near Albuquerque, the 1938 Rio Grande Compact developed primarily because of the necessary repeal of the Rio Grande embargo among other issues. Though both Colorado and New Mexico were initially eager to begin negotiations, they broke down over whether Texas should be allowed to join negotiations in 1928, though it had representatives present. In an effort to avoid litigation of

3555-401: The Rio Grande has marked the boundary between Mexico and the United States from the twin cities of El Paso , Texas, and Ciudad Juárez , Chihuahua, to the Gulf of Mexico. As such, crossing the river was the escape route used by some Texan slaves to seek freedom. Mexico had liberal colonization policies and had abolished slavery in 1828. In 1899, after a gradual change to the river position,

3634-493: The Rio Grande is the national border between the U.S. and Mexico. The segment of the river that forms the international border ranges from 889 to 1,248 miles (1,431 to 2,008 km), depending on how the river is measured. The Rio Conchos is a major tributary of the Rio Grande, with its confluence 310 km. (193 straight air miles) southeast of El Paso near Ojinaga , in Chihuahua , Mexico. Downstream, other tributaries include

3713-426: The Rio Grande rift is by the simple rotation of the Colorado Plateau 1-1.5° in a clockwise direction relative to the North American craton. Other explanations that have been offered are that the extension is driven by mantle forces, such as large-scale mantle upwelling or small-scale mantle convection at the edge of the stable craton; collapse of over-thickened continental crust; initiation of transform faulting along

3792-530: The Rio Grande's discharge increases to its maximum annual average of 3,504 cubic feet per second (99 m /s) near Rio Grande City. Large diversions for irrigation below Rio Grande City reduce the river's average flow to 889 cubic feet per second (25 m /s) at Brownsville and Matamoros. The major international border crossings along the river are at Ciudad Juárez and El Paso ; Presidio and Ojinaga; Laredo and Nuevo Laredo ; McAllen and Reynosa ; and Brownsville and Matamoros. Other notable border towns are

3871-653: The San Luis is roughly 120 by 80 kilometres (75 by 50 mi). These basins may contain smaller units within them, such as the Alamosa basin within the San Luis, which is bounded by the San Juan and Tusas mountains on the west and the Sangre de Cristo Mountains in the east. The Albuquerque basin is the largest of the three basins, spanning 160 kilometres (99 mi) north–south and 86 kilometres (53 mi) east–west at its widest points. It

3950-751: The Southwest, competing with other indigenous communities such as the Apache with territory in the Rio Grande Valley. This led to decades of conflict (the Coalition Period), the eventual merging of cultures, and the establishment of most of the Tanoan and Keresan pueblos of the Rio Grande Valley. This was followed by the Classic Period, from about 1325 CE to 1600 CE and the arrival of the Spanish. The upper Rio Grande Valley

4029-424: The Spanish in 1582. Early American settlers in South Texas began to use the modern 'English' name Rio Grande. By the late 19th century, in the United States, the name Rio Grande had become standard in being applied to the entire river, from Colorado to the sea. By 1602, Río Bravo had become the standard Spanish name for the lower river, below its confluence with the Rio Conchos. The largest tributary of

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4108-458: The Taos Box and the Racecourse Run. The Taos Box, a more dramatic, deep canyon, is famous for its big, technical Class IV rapids, while the Racecourse Run is a Class III stretch better suited for first-time rafters and families. The gorge is also the site of many ancient petroglyphs . At the bottom of the gorge, the Rio Grande is flanked by hidden hot springs and many ruins. The former Chili Line also ran there. NASA geologically trained

4187-496: The Texas/Coahuila pairings of Del Rio – Ciudad Acuña and Eagle Pass – Piedras Negras . Río Grande is Spanish for "Big River" and Río Grande del Norte means "Big River of the North". In English, Rio Grande is pronounced either / ˈ r iː oʊ ˈ ɡ r æ n d / or / ˈ r iː oʊ ˈ ɡ r ɑː n d eɪ / . In Mexico, it is known as Río Bravo or Río Bravo del Norte , bravo meaning (among other things) "furious", "agitated" or "wild". Historically,

4266-417: The U.S. and Mexico was built about 15 miles west of the Brownsville & Matamoros International Bridge. It was inaugurated in August 2015. It moved all rail operations out of downtown Brownsville and Matamoros. The West Rail International Crossing is the first new international rail crossing between the U.S. and Mexico in over a century. The Brownsville & Matamoros International Bridge is now operated by

4345-431: The United States is regulated by the Rio Grande Compact , an interstate pact between Colorado, New Mexico, and Texas. 62,780 acre-feet (77,440,000 m ) of water from the upper Colorado River basin per year is allotted to municipalities in New Mexico by the Upper Colorado River Basin Compact ; Albuquerque owns 48,200. The water is delivered to the Rio Grande via the San Juan–Chama Project . The project's construction

4424-419: The agricultural interests of the Mesilla Valley and those of El Paso and Juárez . In the agreement provisions were made to construct Elephant Butte dam on public lands. This act was the first occurrence of congressionally directed allocation of an interstate river (although New Mexico would not achieve statehood till 1912). Following the admittance of New Mexico into the union, the increased settlement of

4503-440: The bottom of the Albuquerque basin to 3,300 metres (10,800 ft) above sea level in the nearby Sandia Mountains , which flanks the Albuquerque basin to the east. Flanking mountains are generally taller along the east side of the rift (although some of this relief may be Laramide in origin). The thickness of the crust increases to the north beneath the rift, where it may be as much as 5 kilometres (3.1 mi) thicker than it

4582-497: The completion of San Juan-Chama Drinking Water Project (SJCDWP) by the Albuquerque Bernalillo County Water Utility Authority. The SJCDWP uses an adjustable-height diversion dam to skim imported San Juan-Chama water from the Rio Grande, then pumps this water to a treatment plant on Albuquerque's north side. From there it is added to a municipal drinking water distribution system serving Albuquerque's metro area. Diversions are restricted during periods of low river flow in order to protect

4661-477: The easternmost manifestation of widespread extension in the western U.S. during the past 35 million years. The rift consists of three major basins and many smaller basins, less than 100 square kilometres (39 sq mi). The three major basins (from northernmost to southernmost) are the San Luis , Española , and Albuquerque basins. The rift's northern extent is delineated by the upper Arkansas River basin between Leadville and Salida, Colorado . Further south,

4740-469: The findings of which helped lead to the final agreement. The 1938 Rio Grande Compact provided for the creation of a compact commission, the creation of gaging stations along the river to ensure flow amounts by Colorado to New Mexico at the state line and by New Mexico to Elephant Butte Reservoir , the water once there would fall under the regulation of the Rio Grande Project which would guarantee provision to Texas and Mexico. A system of debits and credits

4819-422: The least amount of control over the waterway, has routinely seen an under-provision of water since 1992. In 1997, the US designated the Rio Grande as one of the American Heritage Rivers . Two portions of the Rio Grande are designated National Wild and Scenic Rivers System , one in northern New Mexico and the other in Texas, at Big Bend National Park . In mid-2001, a 328-foot (100 m)-wide sandbar formed at

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4898-439: The lithosphere and allowed for later extension of the region. Cenozoic extension started about 30 million years ago (Ma). There are two phases of extension observed: late Oligocene and middle Miocene . The first period of extension produced broad, shallow basins bounded by low-angle faults. The crust may have been extended as much as 50% during this episode. Widespread magmatism in mid- Cenozoic time suggests that

4977-430: The matter in the Supreme Court a provisional agreement was signed in 1929 which stated that negotiations would resume once a reservoir was built on the New Mexico-Colorado state line. The construction of this was delayed by the Market Crash of 1929 . With negotiations remaining stagnant, Texas sued New Mexico over the issue in 1935, prompting the intervention of the president who set up the Rio Grande Joint Investigation

5056-405: The mouth of the river, marking the first time in recorded history that the Rio Grande failed to empty into the Gulf of Mexico. The sandbar was dredged , but reformed almost immediately. Spring rains the following year flushed the reformed sandbar out to sea, but it returned in mid-2002. By late 2003, the river once again reached the Gulf. For much of the time since water rights were introduced in

5135-401: The natural decrease in flow such that by the time the river reaches Presidio , little or no water is left. Below Presidio, the Rio Conchos restores the flow of water. Near Presidio, the river's discharge is frequently zero. Its average discharge is 178 cubic feet per second (5 m /s), down from 945 cubic feet per second (27 m /s) at Elephant Butte Dam. Supplemented by other tributaries,

5214-475: The region. Although the river's greatest depth is 60 feet (18 m), the Rio Grande generally cannot be navigated by passenger riverboats or by cargo barges . Navigation is only possible near the mouth of the river, in rare circumstances up to Laredo, Texas . Navigation was active during much of the 19th century, with over 200 different steamboats operating between the river's mouth close to Brownsville and Rio Grande City, Texas . Many steamboats from

5293-420: The rift is defined by a network of smaller, less topographically distinct alternating basins and ranges. The distinction between these smaller basins and those of the Basin and Range Province becomes blurred in northern Mexico . Basin size generally decreases to the north in the rift, though the Española covers approximately 120 kilometres (75 mi) north–south and 40 kilometres (25 mi) east–west, and

5372-443: The riparian ecosystem and mitigate effects on endangered species like the Rio Grande silvery minnow . Treated effluent water is recycled into the Rio Grande south of the city. Surface water from the SJCDWP comprises a significant percentage of Albuquerque's drinking water supply, with groundwater constituting the remainder; annual percentages vary according to runoff and climate conditions. Acquisition of native pre-1907 water rights

5451-418: The river flows through the Rio Grande rift from one sediment -filled basin to another, cutting canyons between the basins and supporting a fragile bosque ecosystem on its flood plain . From Albuquerque southward, the river flows through desert. Although irrigated agriculture exists throughout most of its stretch, it is particularly extensive in the subtropical Lower Rio Grande Valley . The river ends in

5530-416: The river in spring of 2023 and flooding of some of its tributaries, including the Jemez and Pecos Rivers . By that summer, after the spring runoff had concluded and due to a failed New Mexico monsoon season and record high temperatures, the river went dry in Albuquerque for a second consecutive year. The United States and Mexico share the water of the river under a series of agreements administered by

5609-416: The states of New Mexico and Texas based on their respective amount of irrigable land. The project also accorded 60,000 acre-feet (74 million cubic meters ) of water annually to Mexico in response to the country's demands. This was meant to put an end to the many years of disagreement concerning rights to the river's flow and the construction of a dam and reservoir at various location on the river between

5688-516: The voluminous consumption of water required to irrigate farmland (e.g. the Mesilla and Lower Rio Grande Valleys ) and to continually hydrate cities (e.g. Albuquerque); such water usages are additional to the reservoirs of water retained with diversion dams . 260 miles (418 km) of the river in New Mexico and Texas are designated as the Rio Grande Wild and Scenic River . The Rio Grande rises in

5767-548: The water debt owed to Texas increased from 31,000 acre-feet to over 130,000 acre-feet since 2021, despite "very significant efforts that were done on the river this year to keep water flowing downstream." In response, New Mexico increased its program offering to subsidize farmers who fallow their fields rather than planting crops, which uses additional water; the city of Albuquerque shut off its domestic supply diversion and switched to full groundwater pumping in 2021. Additionally, in 2022, work began on El Vado Dam , during which it

5846-718: The western margin of the North American plate; or detachment of a fragment of the Farallon plate beneath the Rio Grande region that enhanced asthenospheric upwelling in the slab window. Rio Grande The Rio Grande ( / ˌ r iː oʊ ˈ ɡ r æ n d / or / ˌ r iː oʊ ˈ ɡ r ɑː n d eɪ / ) in the United States or the Río Bravo ( del Norte ) in Mexico ( Spanish pronunciation: [ˈri.o ˈβɾaβo ðel ˈnoɾte] ), also known as P’osoge in Tewa and Tó Ba’áadi in Navajo ,

5925-709: The western part of Rio Grande National Forest , in the U.S. state of Colorado , and is formed by the joining of several streams at the base of Canby Mountain , in the San Juan Mountains , due east of the Continental Divide of the Americas . From the Continental Divide, the Rio Grande flows through the San Luis Valley , then south into New Mexico , and passes through the Rio Grande Gorge , near Taos, then toward Española , afterwards collecting additional waters from

6004-406: Was characterized by occasional periods of extreme drought, and the human inhabitants make extensive use of gridded gardens and check dams to stretch the uncertain water supply. In 1519, a Spanish naval expedition along the northeastern coast of Mexico charted the mouths of several rivers including the Rio Grande. In 1536, the Rio Grande appeared for the first time on a map of New Spain produced by

6083-457: Was created to account for variations in the water provided. The compact remains in effect today, though it has been amended twice. In 1944, the US and Mexico signed a treaty regarding the river. Due to drought conditions which have prevailed throughout much of the 21st century, calls for a reexamination of this treaty have been made by locals in New Mexico, Mexico, and Texas. Texas, being the state with

6162-438: Was designated a national monument , Rio Grande del Norte National Monument , on March 25, 2013. The gorge has Class II to Class V white water rapids that are managed for recreation by The U.S. Bureau of Land Management (BLM). The BLM maintains two developed recreation areas along the river that include hiking, biking and other recreational opportunities. In New Mexico, The Rio Grande has two main sections for rafting near Taos:

6241-676: Was initiated by legislation signed by President John F. Kennedy in 1962, and was completed in 1971. This diversion project transports water under the continental divide from tributaries of the San Juan River (the Navajo, the Little Navajo, and Blanco Rivers) to Heron Reservoir, which empties into the Rio Chama before this connects to the Rio Grande. Although it held rights to San Juan-Chama water for many years, it wasn't until 2008 that Albuquerque began using it as part of its municipal supply, with

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