Santa Fe, New Mexico in the context of "Rio Grande rift"

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👉 Santa Fe, New Mexico in the context of Rio Grande rift

The Rio Grande rift 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 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.

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Santa Fe, New Mexico in the context of New Mexico

New Mexico is a landlocked state in the Southwestern region of the United States. It is one of the Mountain States of the southern Rocky Mountains, sharing the Four Corners region with Utah, Colorado, and Arizona. It also borders the state of Texas to the east and southeast, Oklahoma to the northeast, and shares an international border with the Mexican states of Chihuahua and Sonora to the south. New Mexico's largest city is Albuquerque, and its state capital is Santa Fe, the oldest state capital in the U.S.—founded in 1610 as the government seat of Nuevo México in New Spain—and the highest in elevation, at 6,998 feet (2,133 m).

New Mexico is the fifth-largest of the fifty states by area, but with just over 2.1 million residents, ranks 36th in population and 45th in population density. Its climate and geography are highly varied, ranging from forested mountains to sparse deserts; the northern and eastern regions exhibit a colder alpine climate, while the west and south are warmer and more arid. The Rio Grande and its fertile valley runs from north-to-south, creating a riparian biome through the center of the state that supports a bosque habitat and distinct Albuquerque Basin climate. One–third of New Mexico's land is federally owned, including many protected wilderness areas, 15 national parks and monuments, and three UNESCO World Heritage Sites wholly contained within the state—the most of any U.S. state.

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Santa Fe, New Mexico in the context of Rocky Mountains

The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch 3,000 mi (4,800 km) in a straight-line distance from the northernmost part of Western Canada, to New Mexico in the Southwestern United States. Depending on differing definitions between Canada and the U.S., its northern terminus is located either in northern British Columbia's Terminal Range south of the Liard River and east of the Trench, or in the northeastern foothills of the Brooks Range/British Mountains that face the Beaufort Sea coasts between the Canning River and the Firth River across the AlaskaYukon border. Its southernmost point is near the Albuquerque metropolitan area, adjacent to the Rio Grande rift, and north of the Sandia–Manzano Mountain Range, also near Santa Fe, New Mexico. Being the easternmost portion of the North American Cordillera, the Rockies are distinct from the tectonically younger Cascade Range and Sierra Nevada, which both lie farther to its west.

The Rockies formed 55 million to 80 million years ago during the Laramide orogeny, in which a number of plates began sliding underneath the North American plate. The angle of subduction was shallow, resulting in a broad belt of mountains running down western North America. Since then, further tectonic activity and erosion by glaciers have sculpted the Rockies into dramatic peaks and valleys. At the end of the last ice age, humans began inhabiting the mountain range. After explorations of the range by Europeans, such as Sir Alexander Mackenzie, and Anglo-Americans, such as the Lewis and Clark Expedition, natural resources such as minerals and fur drove the initial economic exploitation of the mountains, although the range itself has never experienced a dense population.

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Santa Fe, New Mexico in the context of Santa Fe de Nuevo México

Santa Fe de Nuevo México (English: Holy Faith of New Mexico; shortened as Nuevo México or Nuevo Méjico, and translated as New Mexico in English) was a province of the Spanish Empire and New Spain, and later a territory of independent Mexico. The first capital was San Juan de los Caballeros from 1598 until 1610, and from 1610 onward the capital was La Villa Real de la Santa Fe de San Francisco de Asís.

The name of "New Mexico", the capital in Santa Fe, the gubernatorial office at the Palace of the Governors, vecino citizen-soldiers, and rule of law were retained as the New Mexico Territory and later state of New Mexico became part of the United States. The New Mexican citizenry, primarily consisting of Hispano, Pueblo, Navajo, Apache, and Comanche peoples, became citizens of the United States as a result of the Treaty of Guadalupe Hidalgo (1848).

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Santa Fe, New Mexico in the context of Tewa language

Tewa (/ˈtwə/ TAY-wə) is a Tanoan language spoken by several Pueblo nations in the Rio Grande valley in New Mexico north of Santa Fe, and in Arizona. It is also known as Tano, or Tée-wah (archaic). There is some disagreement among the Tewa people about whether or not Tewa should have a written form, as some Pueblo elders believe that their language should be preserved by oral tradition alone. Because of this, it was not until the 1960s that the language was written down for the first time. However, many Tewa speakers have decided that Tewa literacy is an important aspect in passing down the language and so orthographies have been created for this purpose.

The language has struggled to maintain a healthy speaker base; however, because of efforts to preserve the language starting in the 1980s—both by native speakers and linguists—this problem is not as dire as for some other indigenous languages.

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Santa Fe, New Mexico in the context of Zamość

Zamość (Polish: [ˈzamɔɕt͡ɕ] ; Yiddish: זאמאשטש, romanizedZamoshtsh; Latin: Zamoscia) is a historical city in southeastern Poland. It is situated in the southern part of Lublin Voivodeship, about 90 km (56 mi) from Lublin, 247 km (153 mi) from Warsaw. In 2021, the population of Zamość was 62,021.

Zamość was founded in 1580 by Jan Zamoyski, Grand Chancellor of Poland, who envisioned an ideal city. The historical centre of Zamość was added to the UNESCO World Heritage List in 1992, following a decision of the sixteenth ordinary session of the World Heritage Committee, held between 7 and 14 December 1992 in Santa Fe, New Mexico, United States; it was recognized for being "a unique example of a Renaissance town in Central Europe".

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Santa Fe, New Mexico in the context of Zebulon Pike

Zebulon Montgomery Pike (January 5, 1779 – April 27, 1813) was an American brigadier general and explorer for whom Pikes Peak in Colorado is named. As a U.S. Army officer he led two expeditions through the Louisiana Purchase territory, first in 1805–1806 to reconnoiter the upper northern reaches of the Mississippi River, and then in 1806–1807 to explore the southwest to the fringes of the northern Spanish-colonial settlements of New Mexico and Texas. Pike's expeditions coincided with other Jeffersonian expeditions, including the Lewis and Clark Expedition and the Red River Expedition in 1806.

Pike's second expedition crossed the Rocky Mountains into what is now southern Colorado, which resulted in his capture by the Spanish colonial authorities near Santa Fe, who then sent Pike and his men to Chihuahua (present-day Mexico) for interrogation. Later in 1807, Pike and some of his men were escorted by the Spanish through Texas and released near U.S. territory in early Louisiana.

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