Sierra Madre Occidental in the context of "Copper Canyon"

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⭐ Core Definition: Sierra Madre Occidental

The Sierra Madre Occidental is a major mountain range system that runs northwest–southeast through northwestern and western Mexico, and along the Gulf of California. The Sierra Madre is part of the American Cordillera, an almost continuous chain of mountain ranges that forms the western "backbone" of the Americas.

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👉 Sierra Madre Occidental in the context of Copper Canyon

Copper Canyon (Spanish: Barrancas del Cobre) is a group of six distinct canyons in the Sierra Madre Occidental in the southwestern part of the state of Chihuahua in northwestern Mexico that is 65,000 square kilometres (25,000 sq mi) in size. The canyons were formed by six rivers that drain the western side of the Sierra Tarahumara (a part of the Sierra Madre Occidental). All six rivers merge into the Rio Fuerte and empty into the Gulf of California. The walls of the canyon are a copper/green color, which is the origin of the name.

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Sierra Madre Occidental in the context of Chihuahua (state)

Chihuahua, officially the Free and Sovereign State of Chihuahua, is one of the 31 states which, along with Mexico City, are the 32 federal entities of Mexico. It is located in the northwestern part of Mexico and is bordered by the states of Sonora to the west, Sinaloa to the southwest, Durango to the south, and Coahuila to the east. To the north and northeast, it shares an extensive border with the U.S. adjacent to the U.S. states of New Mexico and Texas. The state was named after its capital city, Chihuahua City; the largest city is Ciudad Juárez. In 1864 the city of Chihuahua was declared capital of Mexico by Benito Juárez during the Reform War and French intervention until 1867. The city of Parral was the largest producer of silver in the world in 1640. During the Mexican War of Independence, Miguel Hidalgo was executed on July 30, 1811, in Chihuahua city.

Although Chihuahua is primarily identified with its namesake, the Chihuahuan Desert, it has more forests than any other state in Mexico, aside from Durango. Due to its varied climate, the state has a large variety of fauna and flora. The state is mostly characterized by rugged mountainous terrain and wide river valleys. The Sierra Madre Occidental mountain range, part of the continental spine that also includes the Rocky Mountains, dominates the state's terrain, and is home to the state's greatest attraction, Las Barrancas del Cobre, or Copper Canyon, a canyon system larger and deeper than the Grand Canyon. The state also has the largest crystal cave in Mexico known as the Naica cave discovered in 2001. Chihuahua is also home to the archaeological site of Paquimé in Casas Grandes that was created by the people of the Mogollon culture of Northern Mexico and is recognized as an UNESCO World Heritage site. Chihuahua is the largest state in Mexico by area, with an area of 247,455 square kilometres (95,543 sq mi), it is slightly larger than the United Kingdom, and slightly smaller than Wyoming, the tenth largest US state by area. The state is consequently known under the nickname El Estado Grande ('The Great State' or 'The Big State').

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Sierra Madre Occidental in the context of Sinaloa

Sinaloa (Spanish pronunciation: [sinaˈloa] ), officially the Estado Libre y Soberano de Sinaloa (English: Free and Sovereign State of Sinaloa), is one of the 31 states which, along with Mexico City, compose the Federal Entities of Mexico. It is divided into 20 municipalities, and its capital and largest city is Culiacán Rosales. Other large cities include Mazatlán, Los Mochis, Guamúchil, and Guasave.

Sinaloa is located in northwest Mexico and is bordered by the states of Sonora to the northwest, Chihuahua to the north, Durango to the east, and Nayarit to the southeast. To the west, Sinaloa faces Baja California Sur, across the Gulf of California. Its natural geography is divided by the Sierra Madre Occidental, fertile river valleys, and a broad coastal plain along the Gulf of California. The state covers an area of 58,328 square kilometers (22,521 sq mi) and includes the islands of Palmito Verde, Palmito de la Virgen, Altamura, Santa María, Saliaca, Macapule, and San Ignacio.

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Sierra Madre Occidental in the context of Mexican Plateau

The Central Mexican Plateau, also known as the Mexican Altiplano (Spanish: Altiplano mexicano), is a large arid-to-semiarid plateau that occupies much of northern and central Mexico. Averaging 1,825 m (5,988 ft) above sea level, it extends from the United States border in the north to the Trans-Mexican Volcanic Belt in the south, and is bounded by the Sierra Madre Occidental and Sierra Madre Oriental to the west and east, respectively.

A low east-west mountain range in the state of Zacatecas divides the plateau into northern and southern sections. These two sections, called the Northern Plateau (Mesa del Norte) and Central Plateau (Mesa Central), are now generally regarded by geographers as sections of one plateau.

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Sierra Madre Occidental in the context of Chihuahuan Desert

The Chihuahuan Desert (Spanish: Desierto de Chihuahua, Desierto Chihuahuense) 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 501,896 km (193,783 sq mi), it is the largest hot desert in North America. The desert is fairly young, existing for only 8,000 years.

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Sierra Madre Occidental in the context of Pacific Slope

The Pacific Slope describes geographic regions in North American, Central American, and South American countries that are west of the continental divide and slope down to the Pacific Ocean. In North America, the Rocky Mountains mark the eastern border of the Pacific Slope. In Central and South America, the region is much narrower, confined by the Sierra Madre Occidental in Central America, and by the Andes in South America. The phrase is still used today mostly for scientific purposes to refer to regions inhabited by specific species.

It was and is still occasionally used to describe the region in North America during the 19th century and the expansion of the Old West. It includes the states and territories west of the continental divide that runs down the Rocky Mountains in North America. This included the territories and the states that emerged from them, including California, Oregon Territory, Washington Territory, Nevada Territory, Idaho Territory, Colorado Territory, and Utah Territory. The region is drained by the Columbia, Sacramento, San Joaquin and Colorado River systems. In the United States, the Pacific-slope flycatcher takes its name from the region it inhabits.

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Sierra Madre Occidental in the context of Huichol people

The Wixárika (Huichol pronunciation: [wiˈraɾika]) or Huichol (Spanish pronunciation: [ˈwit͡ʃo̞l]) are an Indigenous people of Mexico living in the Sierra Madre Occidental range in the states of Nayarit, Jalisco, Zacatecas, and Durango, with considerable communities in the United States, in the states of California, Arizona, New Mexico, and Texas. They are best known to the larger world as the Huichol, although they refer to themselves as Wixáritari ("the people") in their Huichol language. The adjectival form of Wixáritari and name for their own language is Wixárika.

The Wixárika speak a language of the Wixarikan group that is closely related to the Nahuatl group. Furthermore, they have received Mesoamerican influences, which is reflected by the fact that Wixarika has features typical of the Mesoamerican language area.

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Sierra Madre Occidental in the context of North American monsoon

The North American monsoon, variously known as the Southwest monsoon, the Mexican monsoon, the New Mexican monsoon, or the Arizona monsoon is a pattern of pronounced seasonal increase in thunderstorms and rainfall over large areas of the southwestern United States and northwestern Mexico.

Geographically, the weather pattern is centered over the Sierra Madre Occidental in the Mexican states of Sinaloa, Durango, Sonora and Chihuahua, and typically occurs between June and mid-September. Thunderstorms are fueled by daytime heating and build up during the late afternoon and early evening. Typically, these storms dissipate by late night, and the next day starts out fair, with the cycle repeating daily. The cycle typically loses its energy by mid-September when much drier conditions are reestablished over the region.

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