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Brazos Mountains
The Brazos Mountains is a range in far northern Rio Arriba County, in northern New Mexico in the southwestern United States. The range is part of the Tusas Mountains (the southern portion of the San Juan Mountains), which extended slightly into Colorado. A high crest runs from the border with Colorado for over in a south-southeasterly direction. The high point of the range at is on Grouse Mesa, at the Brazos Benchmark. Two miles (3 km) to the southeast is the more distinctive Brazos Peak, at 11,288 feet (3440 m). The range is mostly located in the privately held Tierra Amarilla Land Grant (the Carson National Forest is to the east and south). It is a distinctive part of the view from the west, including from Heron Lake. U.S. Route 64 crosses the southern end of the range at a 10,481 foot (3194 m) pass. This is the highest paved through road pass in New Mexico. Nearby are the photogenic Brazos Cliffs, headwaters of the Rio Brazos and part of the Rio Chama river sy ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Brazos (New Mexico)
The Rio Brazos is a long river flowing through northern New Mexico in the United States. It rises in the Tusas Mountains, a subrange of the San Juan Mountains, and runs generally southwest to a confluence with the Rio Chama, part of the larger Rio Grande system. The river is formed by two streams, the West Fork and the East Fork, which converge at Brazos Meadows, just outside the western boundary of the Carson National Forest. For its first few miles, it flows south as a slow-moving, meandering mountain stream. East of Brazos Peak, it swings abruptly west into the Brazos Box, one of the largest canyons in New Mexico with a maximum depth of more than . Here, it passes the Brazos Cliffs, receives Gavilan and Encinado Creeks, and picks up an unnamed tributary which feeds Brazos Falls, reputedly New Mexico's highest waterfall with a total drop of . Northeast of Tierra Amarilla, the river emerges from the mountains, receiving Chavez Creek from the right. It passes the settlement ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sangre De Cristo Mountains
) , country= United States , subdivision1_type= States , subdivision1= , parent= Rocky Mountains , geology= , orogeny= , area_mi2= 17193 , range_coordinates= , length_mi= 242 , length_orientation= north-south , width_mi= 120 , width_orientation= east-west , highest= Blanca Peak , elevation_ft= 14351 , coordinates= , highest_location= East of Alamosa, Colorado , map= , map_size= , map_caption= 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 all the peaks in New Mexico which are over twelve thousand feet. The name of the mountains may refer to the occasion ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laramide Orogeny
The Laramide orogeny was a time period of mountain building in western North America, which started in the Late Cretaceous, 70 to 80 million years ago, and ended 35 to 55 million years ago. The exact duration and ages of beginning and end of the orogeny are in dispute. The Laramide orogeny occurred in a series of pulses, with quiescent phases intervening. The major feature that was created by this orogeny was deep-seated, thick-skinned deformation, with evidence of this orogeny found from Canada to northern Mexico, with the easternmost extent of the mountain-building represented by the Black Hills of South Dakota. The phenomenon is named for the Laramie Mountains of eastern Wyoming. The Laramide orogeny is sometimes confused with the Sevier orogeny, which partially overlapped in time and space. The orogeny is commonly attributed to events off the west coast of North America, where the Kula Plate, Kula and Farallon Plates were sliding under the North American plate. Most hypothes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peneplain
390px, Sketch of a hypothetical peneplain formation after an orogeny. In geomorphology and geology, a peneplain is a low-relief plain formed by protracted erosion. This is the definition in the broadest of terms, albeit with frequency the usage of peneplain is meant to imply the representation of a near-final (or penultimate) stage of fluvial erosion during times of extended tectonic stability. Peneplains are sometimes associated with the cycle of erosion theory of William Morris Davis, but Davis and other workers have also used the term in a purely descriptive manner without any theory or particular genesis attached. The existence of some peneplains, and peneplanation as a process in nature, is not without controversy, due to a lack of contemporary examples and uncertainty in identifying relic examples. By some definitions, peneplains grade down to a base level represented by sea level, yet in other definitions such a condition is ignored. Geomorphologist Karna Lidmar-Bergstrà ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brazos Mountains New Mexico
The Brazos River ( , ), called the ''RÃo de los Brazos de Dios'' (translated as "The River of the Arms of God") by early Spanish explorers, is the 11th-longest river in the United States at from its headwater source at the head of Blackwater Draw, Roosevelt County, New Mexico to its mouth at the Gulf of Mexico with a drainage basin. Being one of Texas' largest rivers,"Brazos River." Britannica Academic, Encyclopædia Britannica, 11 Aug. 2018. academic.eb.com/levels/collegiate/article/Brazos-River/16291. Accessed 27 Nov. 2018. it is sometimes used to mark the boundary between East Texas and West Texas. The river is closely associated with Texas history, particularly the Austin settlement and Texas Revolution eras. Today major Texas institutions such as Texas Tech University, Baylor University, and Texas A&M University are located close to the river's basin, as are parts of metropolitan Houston. Geography The Brazos proper begins at the confluence of the Salt Fork an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Chama (Rio Grande)
The Rio Chama, a major tributary river of the Rio Grande, is located in the U.S. states of Colorado and New Mexico. The river is about long altogether. From its source to El Vado Dam its length is about , from El Vado Dam to Abiquiu Dam is about , and from Abiquiu Dam to its confluence with the Rio Grande is about .Calculated in Google Earth The name "Chama" is a shortened version of the Tewa term '' sąmą' ǫŋwįkeyi', meaning "wrestling pueblo-ruin". Course The Rio Chama originates in south-central Colorado, just above the New Mexico border in the San Juan Mountains and Rio Grande National Forest. The main stem Rio Chama begins at the confluence of two short headwater tributaries called West Fork and East Fork. The West Fork flows eastward from the Continental Divide. Across the divide lies the Navajo River, one of the headwater tributaries of the Colorado River. The East Fork extends a few miles into Conejos County, Colorado to a source near one of the headwater tributar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heron Lake (New Mexico)
Heron Lake is a reservoir in Rio Arriba County, New Mexico in the southwestern United States. The reservoir is part of the San Juan-Chama Project, which connects the San Juan River in Colorado to the Rio Chama, which is part of the Rio Grande watershed. Lake Heron is 80 miles northwest of Santa Fe. Water is impounded in Heron Lake by the long, high Heron Dam, which was completed in 1971. The lake is approximately long and wide, and lies at an elevation of up to . Heron Dam is owned and operated by the United States Bureau of Reclamation. The southern shore is the location of Heron Lake State Park, featuring over 200 camping and picnic sites, and two improved boat ramps. The lake is a destination for salmon and trout fishing, as well as for small boat sailing. Boat speeds are restricted by a 'no-wake' policy. A hiking trail crosses the Rio Chama Gorge via a pedestrian suspension bridge, and then runs southwest through wooded terrain to the grounds of El Vado Lake ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Arriba County, New Mexico
Rio Arriba County is a county in the U.S. state of New Mexico. As of the 2010 census, the population was 40,246. Its county seat is Tierra Amarilla. Its northern border is the Colorado state line. Rio Arriba County comprises the Española, NM Micropolitan Statistical Area, which is also included in the Albuquerque- Santa Fe-Las Vegas, NM Combined Statistical Area. History The county was one of nine originally created for the Territory of New Mexico in 1852. Originally extending west to the California line, it included the site of present-day Las Vegas, Nevada. The county seat was initially sited at San Pedro de Chamita, and shortly afterwards at Los Luceros. In 1860 the seat was moved to Plaza del Alcalde. Since 1880 Tierra Amarilla has been the county seat. The Battle of Embudo Pass took place in the southern part of the county during the Mexican–American War in January 1847. Geography According to the U.S. Census Bureau, the county has a total area of , of which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carson National Forest
Carson National Forest is a national forest in northern New Mexico, United States. It encompasses 6,070 square kilometers (1.5 million acres) and is administered by the United States Forest Service. The Forest Service's "mixed use" policy allows for its use for recreation, grazing, and resource extraction. Geography The forest is disjunct with four separate areas managed by six ranger districts. On the east side in the Sangre de Cristo Mountains are two districts that are separated by the Taos Pueblo. The west side of the forest has three are conjoined districts in the San Juan Mountains, sandwiched between the Santa Fe and Rio Grande national forests, and another in the San Juan Basin. The forest is located mainly in Rio Arriba (63.4% of acreage) and Taos (34.65%) counties, but smaller areas extend eastward into western Mora and Colfax counties. Wheeler Peak, the highest mountain in New Mexico at , is located in the National Forest. Wilderness areas Within the Carson Nation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colorado
Colorado (, other variants) is a state in the Mountain West subregion of the Western United States. It encompasses most of the Southern Rocky Mountains, as well as the northeastern portion of the Colorado Plateau and the western edge of the Great Plains. Colorado is the eighth most extensive and 21st most populous U.S. state. The 2020 United States census enumerated the population of Colorado at 5,773,714, an increase of 14.80% since the 2010 United States census. The region has been inhabited by Native Americans and their ancestors for at least 13,500 years and possibly much longer. The eastern edge of the Rocky Mountains was a major migration route for early peoples who spread throughout the Americas. "''Colorado''" is the Spanish adjective meaning "ruddy", the color of the Fountain Formation outcroppings found up and down the Front Range of the Rocky Mountains. The Territory of Colorado was organized on February 28, 1861, and on August 1, 1876, U.S. President Ulyss ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
