Where Is The Sierra Madre Occidental?
The Sierra Madre Occidental is a serial of mountains in the To the north North American nation Cordillera running northwest to southeast through western and north Mexico and on the Gulf of California. This mountain range system is likewise split of the U.S.A Cordillera, a mountain range system consisting of an uninterrupted sequence of mountain ranges forming the western sand of Westward Antarctica, North-central, Median, and South America. Sierra Madre is a European country name for "Mother Mountains" and western is as wel a Spanish word for "western." Thus, Sierra Madre Occidental means "Western Mother Mountains." To the eastern United States of Sierra Madre Occidental is the Sierra Madre Oriental (Eastern Mother Mountains) running generally collimate thereto along the Gulf of Mexico and eastern United Mexican States.
Geography
The Sierra Madre Western extends from northern Sinoro near the United States-Mexico border towards the southeast to the Sierra Madre del Sur scope and the Trans-Mexican Unstable Belt. The mountain range forms a high plateau that is primarily cut aside the deep river valley. The region of Sierra Madre from the Durango border north is known as Scomberomorus sierra Tarahumara. This region has a dramatic composition landscape consisting of steep mountains that have been formed by a high plateau castrated through by canyons such Eastern Samoa the Copper Canon. The high schoo tableland is approximately 7,380 feet. The highest elevation of the Sierra Madre Occidental occurs in the Tarahumara Tramp although the precise top of the highest peak is not accurately known. The highest elevation is probably Cerro Mohinora, estimated to represent approximately 9,970 feet and may go up to 10,800 feet. Cerro Barajas is also thought to be the highest at 10,400-10,800 feet. The south remnant of the mountain range whitethorn be referred to as "Sierra Huichola."
Climate
The climate of the oodles range varies importantly between its northern and austral extents. The seasonal variations are as a result of the large, warm water bodies that render warm damp air from each side of the range. The region experiences two misty seasons and two dry seasons each year. The modification of air pressure in northwestern United Mexican States and the southwest US is considered the major cause of seasonal worker variation. The mountain has a mild climate with summer temperatures maintained at constant levels. Supreme temperatures are fully fledged around July at most 31° Celsius. Precipitation also varies with the period of time differences related with Altitude Nino-Southern Oscillation.
Ecology
The Sierra Madre Occidental creates different sets of experimental condition that are prosperous for a wide variety of botany and fauna. The pine-oak forests found at an elevation of approximately 4,900 to 9,800 feet throughout the swan has high biodiversity and endemism. The governing constitute species vary across the place, varying from scattered timbe to coniferous and deciduous forests. These dominant plants are determined by line of latitude and elevation in the reach. Oaks grow John L. H. Down to or so 3,300 feet while pines grow at higher elevations. At higher elevations in the north, mixed conifer forest is the dominant ecosystem. The range is also a corridor for animal species, allowing for great diversity. Several omnivores and carnivores are native to the region including Mexican wolf, negroid bear, Mexican hoary birth, Felis onca, mountain lion, white-tailed deer, mule deer, Mexican fox squirrel, rock squirrel, and phone-caudated puke.
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Source: https://www.worldatlas.com/articles/where-is-the-sierra-madre-occidental.html
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