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Lava Gate
Lava Gate is an narrow area in the Jornada del Muerto, in the southern part of Socorro County, New Mexico. The Lava Gate creates a gap that trends north northwest to south southwest, between the malpaís (lava fields) of the Jornada del Muerto Volcano to the northeast and the foothills of the Fra Cristobal Range to the southwest. Its midpoint lies at an elevation of . The Lava Gate provided a path for the Camino Real de Tierra Adentro from the interior of the Jornada del Muerto to the Rio Grande at Paraje, Socorro County, New Mexico Paraje was a populated place along the east bank of the Rio Grande, in Socorro County, New Mexico, United States, now a ghost town. It is located north northeast of the Fra Cristobal Range. History Paraje de Fray Cristóbal The site of Paraje .... from newmexicohistory.org accessed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jornada Del Muerto
The name Jornada del Muerto translates from Spanish as "Single Day's Journey of the Dead Man" or even "Route of the Dead Man, though the modern literal translation is closer to "The Working Day of the Dead". It was the name given by the Spanish conquistadors to the Jornada del Muerto Desert basin, and the particularly dry stretch of a route through it from Las Cruces to Socorro, New Mexico. The trail led northward from central Spanish colonial New Spain, present-day Mexico, to the farthest reaches of the viceroyalty in northern Nuevo México Province (the area around the upper valley of the Rio Grande). The route later became a section of the Camino Real. Natural history The Jornada del Muerto desert is a wide and long stretch of flat desert landforms and xeric habitat about from north to south. The desert runs between the Oscura Mountains and San Andres Mountains on the east, and the Fra Cristóbal Range and Caballo Mountains on the west. The western mountains block acce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Socorro County, New Mexico
Socorro County is a county in the U.S. state of New Mexico. As of the 2010 census, the population was 17,866. The county seat is Socorro. The county was formed in 1852 as one of the original nine counties of New Mexico Territory. Socorro was originally the name given to a Native American village (''see'': Puebloan peoples) by Don Juan de Oñate in 1598. Having received vitally needed food and assistance from the native population, Oñate named the pueblo ''Socorro'' ("succor" in English). Socorro County is home to multiple scientific research institutions including New Mexico Institute of Mining and Technology, the National Radio Astronomy Observatory and its associated Very Large Array, the Magdalena Ridge Observatory, and the Langmuir Laboratory for Atmospheric Research. Federal public lands in Socorro County include parts of the Cibola National Forest, the Bosque del Apache National Wildlife Refuge, the Sevilleta National Wildlife Refuge, the Bureau of Land Mana ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Malpaís (landform)
Malpaís, in the Southwestern United States, Spain, Mexico, and other Spanish-speaking regions, are rough and barren landscapes that consist of relict and largely uneroded lava fields exhibiting recognizable lava flows, volcanic cones, and other volcanic landforms. This type of volcanic landscape is extremely rough and difficult to traverse. It is characteristic of arid environments because in more humid climates, such rough terrains are smoothed by erosion and vegetation. While the term describes many xeric places, it is strongly associated with Spanish-speaking countries and the Southwestern United States, where Spanish settlers named this landform.Strahler, A. N., 1970, ''Introduction to Physical Geography'', 2nd ed. John Wiley and Sopns. New York, New York. 486 pp. Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Badlands landform The word 'malpaís' in Spanish t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jornada Del Muerto Volcano
The Jornada del Muerto Volcano is a small shield volcano and lava field in central New Mexico, about in size and reaching an elevation of . Jornada del Muerto means "Dead Man's Route" in Spanish language, Spanish, referring to the desolate colonial era trail from New Spain through this ''Malpaís (landform), Malpaís'' region. Geography The volcano and lava field is located at the northern end of the Jornada del Muerto, Jornada del Muerto Desert Depression (geology), basin in the Basin and Range Province. The Jornada del Muerto basin runs between the Oscura Mountains and San Andres Mountains on the east, with the Caballo Mountains and the Fra Cristobal Range, Fra Cristóbal Range on the west. Geology Volcano and cones The main volcano vent is located slightly to the east of the center of the lava flows, rising about in a broad but conspicuous cone about a mile (1.6 km) in diameter. Within the outer cone are a series of nested Splatter cone, spatter cones interspersed w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fra Cristobal Range
The Fra Cristobal Range, (Fra Cristóbal Range) is a 17 mi (27 km) long, mountain range in central-north Sierra County, New Mexico. Its northern extreme above Fra Cristoblal Mountain extends into Socorro County. The range borders the eastern shore of Elephant Butte Reservoir on the Rio Grande, and the range lies towards the southwest of the Jornada del Muerto, the desert region east of the river. Description The Fra Cristobal Range is an arid, moderate elevation, north–south trending mountain range, about 17 mi long and narrow, only about 7 mi at its widest. Crater Hill, lies west of the central ridgeline, and north of Black Bluffs, Red Cliff at the Reservoir. The high peak in the northern end of the range, which gives the range its name, is Fra Cristobal Mountain, , is at the north perimeter of the range. It is located at The mountain is said to have resembled the profile of a priest, Fray Cristóbal de Salazar, a cousin of Juan de Oñate Juan de O ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Camino Real De Tierra Adentro
The Camino Real de Tierra Adentro ( en, Royal Road of the Interior Land), also known as the Silver Route, was a Spanish road between Mexico City and San Juan Pueblo (''Ohkay Owingeh''), New Mexico, USA, that was used from 1598 to 1882. It was the northernmost of the four major "royal roads" that linked Mexico City to its major tributaries during and after the Spanish colonial era. In 2010, 55 sites and five existing UNESCO World Heritage Sites along the Mexican section of the route were collectively added to the World Heritage List, including historic cities, towns, bridges, haciendas and other monuments along the route between the Historic Center of Mexico City (an independent World Heritage Site) and the town of Valle de Allende, Chihuahua. The section of the route within the United States was proclaimed the El Camino Real de Tierra Adentro National Historic Trail, a part of the National Historic Trail system, on October 13, 2000. The historic route is overseen by both ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Grande
The Rio Grande ( and ), known in Mexico as the Río Bravo del Norte or simply the Río Bravo, 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 . 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 ; however, the endorheic basins that are adjacent to and within the greater drainage basin of the Rio Grande increase the total drainage-basin area to . The Rio Grande with its fertile valley, along with its tributaries, is a vital watersource for seven US and Mexican states, and flows primarily through arid and semi-arid lands. After traversing the length of New Mexico, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paraje, Socorro County, New Mexico
Paraje was a populated place along the east bank of the Rio Grande, in Socorro County, New Mexico, United States, now a ghost town. It is located north northeast of the Fra Cristobal Range. History Paraje de Fray Cristóbal The site of Paraje was originally an area known to the first Spanish colonists of New Mexico as Paraje de Fray Cristóbal. It was a paraje, an unpopulated stopping place along the old Camino Real de Tierra Adentro from the sixteenth to the nineteenth centuries. It was the first watering and grazing place along the Rio Grande available, after the crossing of the Jornada del Muerto from the south or the last such stop before entering it from the north. Travelers passed through the north northwest/south southeast trending Lava Gate between the difficult terrain of the Jornada del Muerto Volcano ''malpaís'' (lava field) to the northeast of it and the foothills of the mountain range to the southwest which funneled travelers to the paraje on the Rio Grande. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Socorro County, New Mexico
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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