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Jornada Del Muerto Valley
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 ac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chihuahuan Desert
The Chihuahuan Desert ( es, Desierto de Chihuahua, ) is a desert ecoregion designation covering parts of northern Mexico and the southwestern United States. It occupies much of far West Texas, the middle to lower Rio Grande Valley and the lower Pecos Valley in New Mexico, and a portion of southeastern Arizona, as well as the central and northern portions of the Mexican Plateau. It is bordered on the west by the Sonoran Desert, the Colorado Plateau, and the extensive Sierra Madre Occidental range, along with northwestern lowlands of the Sierra Madre Oriental range. Its largest, continual expanse is located in Mexico, covering a large portion of the state of Chihuahua, along with portions of Coahuila, north-eastern Durango, the extreme northern part of Zacatecas, and small western portions of Nuevo León. With an area of about , it is the largest desert in North America. The desert is fairly young, existing for only 8000 years. Geography There are several larger mountain ranges ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pueblo Revolt
The Pueblo Revolt of 1680, also known as Popé's Rebellion or Popay's Rebellion, was an uprising of most of the indigenous Pueblo people against the Spanish empire, Spanish colonizers in the province of Santa Fe de Nuevo México, larger than present-day New Mexico. The Pueblo Revolt killed 400 Spaniards and drove the remaining 2,000 settlers out of the province. The Spaniards reconquered New Mexico twelve years later. Background For more than 100 years beginning in 1540, the Pueblo people of present-day New Mexico were subjected to successive waves of soldiers, missionaries, and settlers. These encounters, referred to as ''entradas'' (incursions), were characterized by violent confrontations between Spanish colonists and Pueblo peoples. The Tiguex War, fought in the winter of 1540–41 by the expedition of Francisco Vásquez de Coronado against the twelve or thirteen pueblos of Tiwa Puebloans, Tiwa Native Americans, was particularly destructive to Pueblo and Spanish relations. In ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pueblo
In the Southwestern United States, Pueblo (capitalized) refers to the Native tribes of Puebloans having fixed-location communities with permanent buildings which also are called pueblos (lowercased). The Spanish explorers of northern New Spain used the term ''pueblo'' to refer to permanent indigenous towns they found in the region, mainly in New Mexico and parts of Arizona, in the former province of Nuevo México. This term continued to be used to describe the communities housed in apartment structures built of stone, adobe mud, and other local material. The structures were usually multi-storied buildings surrounding an open plaza, with rooms accessible only through ladders raised/lowered by the inhabitants, thus protecting them from break-ins and unwanted guests. Larger pueblos were occupied by hundreds to thousands of Puebloan people. Various federally recognized tribes have traditionally resided in pueblos of such design. Later Pueblo Deco and modern Pueblo Revival architectu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quivira And Cíbola
Quivira is a place named by Spanish conquistador Francisco Vásquez de Coronado in 1541, for the mythical Seven Cities of Gold that he never found. Quivira was a province of the ancestral Wichita people, located near the Great Bend of the Arkansas River in central Kansas, The exact site may be near present-day Lyons extending northeast to Salina. The Wichita city of Etzanoa, which flourished between 1450 and 1700, is likely part of Quivira. Expedition In 1540, Spaniard Francisco Vásquez de Coronado led a large expedition north from Mexico to search for wealth and the Seven Cities of Cibola. Instead of wealth, he found Indigenous farmers living in an array of communities and villages in what are today Arizona and New Mexico. These were the Hopi, Zuni, Rio Grande Pueblo, Apache, and Navajo peoples. As Coronado arrived at the Rio Grande, he was disappointed by the lack of wealth among the Pueblo people, but he heard from a Plains Indian informant dubbed “The Turk” of a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Field
Lava fields are large, mostly flat areas of surface or subaquatic lava flows. Such features are generally composed of highly fluid basalt lava, and can extend for tens or hundreds of miles across the underlying terrain. Morphology and structure The final morphology of a lava field can reveal properties such as internal structure, composition, and mechanics of the lava flow when it was fluid. The ridges and patterns on top of the lava field show the direction of the channels and the oftentimes active lava tubes that may be underneath the solidified "crust." It can also reveal whether the lava flow can be classified as pāhoehoe or 'a'ā. The two main types of lava field structures are defined as sheet flow lava and pillow lava. Sheet flow lava appears like a wrinkled or folded sheet, while pillow lava is bulbous, and often looks like a pile of pillows atop one another. An important aspect of lava flow morphology is a phenomenon known as lava flow inflation. This occurs in p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shield Volcano
A shield volcano is a type of volcano named for its low profile, resembling a warrior's shield lying on the ground. It is formed by the eruption of highly fluid (low viscosity) lava, which travels farther and forms thinner flows than the more viscous lava erupted from a stratovolcano. Repeated eruptions result in the steady accumulation of broad sheets of lava, building up the shield volcano's distinctive form. Shield volcanoes are found wherever fluid low-silica lava reaches the surface of a rocky planet. However, they are most characteristic of ocean island volcanism associated with hot spots or with continental rift volcanism. They include the largest volcanoes on earth, such as Tamu Massif and Mauna Loa. Giant shield volcanoes are found on other planets of the Solar System, including Olympus Mons on Mars and Sapas Mons on Venus. Etymology The term 'shield volcano' is taken from the German term ''Schildvulkan'', coined by the Austrian geologist Eduard Suess in 1888 an ... [...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, referring to the desolate colonial era trail from New Spain through this '' Malpaís'' region. Geography The volcano and lava field is located at the northern end of the Jornada del Muerto Desert 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 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 spatter cones interspersed with lava pools. On the south side the innermost spatter cone rises to nearly above the surrounding lava pools ... [...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 Basin LTER
Jornada originally an old Spanish word for a day's walk or journey, often indicating a difficult one, can refer to: Places * Jornada del Muerto, New Mexico * Jornada del Muerto Volcano Newspapers * ''Jornada'' (La Paz), a newspaper published in La Paz, Bolivia * ''La Jornada'', Mexico City newspaper * La Jornada (Managua) * '' La Jornada Latina'', Cincinnati weekly newspaper *''Jornada'', newspaper in Catalan distributed between May 5 and October 27, 2018. Computing technology *Jornada (PDA), line of Hewlett Packard PDAs, including: :* Jornada 560 series *Jornada Linux Mobility Edition or Jlime, a Linux distribution Other * Cabalgata Jornada Villista; see Cavalcade * Jornada, the longer act of a 17th-century Spanish play, interspersed with entremés Entremés, is a short, comic theatrical performance of one act, usually played during the interlude of a performance of a long dramatic work, in the 16th and 17th centuries in Spain. Later it became the sainete. Dictionary of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
