Sierra Madre Oriental

The Sierra Madre Oriental (Spanish: [ˈsjera ˈmaðɾe oɾjenˈtal] (listen)) is a mountain range in northeastern Mexico. The Sierra Madre Oriental is part of the American Cordillera, a chain of mountain ranges (cordillera) that consists of an almost continuous sequence of mountain ranges that form the western "backbone" of North America, Central America, South America and Antarctica.

Sierra Madre Oriental
Sierra Madre Oriental near Ciudad Victoria, Tamaulipas
Highest point
PeakCerro San Rafael
Elevation3,700 m (12,100 ft)
Prominence1,855 m (6,086 ft)
Coordinates25°22′N 100°33′W 
Geography
CountryMexico
StatesCoahuila, Nuevo León, Tamaulipas, San Luis Potosí, Hidalgo, Puebla and Querétaro

Setting

Spanning 1,000 kilometres (620 mi) the Sierra Madre Oriental runs from the Rio Grande on the border between Coahuila and Texas south through Nuevo León, southwest Tamaulipas, San Luis Potosí, Querétaro, and Hidalgo to northern Puebla, where it joins with the east-west running Eje Volcánico Transversal of central Mexico. The northernmost are the Sierra del Burro and the Sierra del Carmen which reach the border with the United States at the Rio Grande. North of the Rio Grande, the range continues northwestward into Texas and beyond as the Davis and Guadalupe Ranges.

Mexico's Gulf Coastal Plain lies to the east of the range, between the mountains and the Gulf of Mexico coast. The Mexican Plateau, which averages 1,100 metres (3,600 ft) in elevation, lies between the Sierra Madre Oriental and the Sierra Madre Occidental further west.

The climate of the Sierra Madre Oriental is drier than the rainforest areas further south.

The Sierra Madre Oriental in Hidalgo state.

Highest major summits

The highest point is Cerro San Rafael, at 3,700 metres (12,100 ft) above sea level, is the highest point of the Sierra Madre Oriental and the state of Coahuila and the second in Mexico in isolation.[1][2]

The Highest Major Mountain Peaks of Sierra Madre Oriental
Rank Mountain Peak State Mountain Range Elevation Prominence Isolation
1 Cerro San Rafael[3] PB  Coahuila Sierra Madre Oriental 3700 m
12,139 feet		 1855 m
6,086 feet		 628 km
390 miles
2 Sierra de la Marta[4] PB  Coahuila
 Nuevo León		 Sierra Madre Oriental 3700 m
12,139 feet		 NA 607 km
377 miles
3 Cerro el Potosí PB  Nuevo León Sierra Madre Oriental 3700 m
12,139 feet		 1380 m
4,528 feet		 570 km
354 miles

Ecology

This long range of tall mountains is noted for its abundant biodiversity and large number of endemic species of plants and wildlife, from the dry north to the wetter south. The Sierra Madre Oriental pine-oak forests are found at high elevations in the range (1,000–3,500 m or 3,300–11,500 ft above sea level).[5] To the east, the Tamaulipan matorral occupies the range's lower slopes in Nuevo León and northern Tamaulipas, while the Veracruz moist forests cover the lower slopes of the central range, and the eastern slopes at the southern end of the range are home to the Veracruz montane forests. West of the range, the Mexican Plateau is home to deserts and xeric shrublands, including the Chihuahuan Desert to the north, the Meseta Central matorral on the central part of the plateau, and the Central Mexican matorral on the southern plateau.

Much of the wildlife can also be found in the Sierra Madre Occidental, which runs parallel to these mountains along western Mexico.

  • Road into the cloud forest of El Cielo Biosphere Reserve, Municipality of Gómez Farías, Tamaulipas, Mexico (16 April 2001)
  • Gravel road through the arid interior slopes of the Sierra Madre Oriental, Municipality of Miquihuana, Tamaulipas, Mexico (10 August 2003)
  • Looking down on the Marcela valley from Sierra Peña Navada, Municipality of Miquihuana, Tamaulipas, Mexico (10 August 2003)

Flora

Pine-oak forests are dominated by several species of pine, such as Pinus nelsonii, P. cembroides, P. pseudostrobus, and P. arizonica, and oak, such as Quercus castanea and Q. affinis.[5] Matorral is characterized by woody shrubs, small trees, cacti, and succulents. Montane chaparral is found above 1,700 m (5,600 ft) and is home to species in the genera Quercus, Arbutus, Yucca, Cercocarpus and Bauhinia. Piedmont scrub occurs below 2,000 m (6,600 ft) and is composed of plants 3 to 5 m (9.8 to 16.4 ft) in height such as Helietta parvifolia, Neopringlea integrifolia and Acacia spp.[6] The canopy of moist forests is dominated by trees up to 30 m (98 ft) in height, including Brosimum alicastrum, Manilkara zapota, Celtis monoica, Bursera simaruba, Dendropanax arboreus, and Sideroxylon capiri.[7]

Fauna
See also: List of birds of the Sierra Madre Oriental

Birds of the forest include the Mexican chickadee, Montezuma quail, Strickland's woodpecker, zone-tailed hawk and several species of jay.

Pine-oak forests in Coahuila are part of the migration route of monarch butterflies (Danaus plexippus).[5]

Threats and conservation

Original habitats have been severely reduced by clearance for livestock grazing and logging over hundreds of years. Protected areas include the Cumbres de Monterrey National Park in Mexico and the Big Bend National Park in Texas. The El Cielo Biosphere in Tamaulipas preserves the northernmost tropical Veracruz moist forests in Mexico and extensive temperate cloud forests.[8]

See also
  • Mountain peaks of Mexico

References
  1. "Cerro San Rafael - Peakbagger.com". peakbagger.com. Retrieved 27 May 2016.
  2. "Sierra Madre Oriental". peakbagger.com. Retrieved 27 May 2016.
  3. The summit of Cerro San Rafael is the highest point of the Sierra Madre Oriental and the state of Coahuila.
  4. The summit of Sierra de la Marta on the border with Coahuila is the highest point of the state of Nuevo León.
  5. "Sierra Madre Oriental pine-oak forests". Terrestrial Ecoregions. World Wildlife Fund. Retrieved 2010-08-22.
  6. "Tamaulipan matorral". Terrestrial Ecoregions. World Wildlife Fund. Retrieved 2010-08-22.
  7. "Veracruz moist forests". Terrestrial Ecoregions. World Wildlife Fund. Retrieved 2010-08-22.
  8. "Gomez Farias Region and El Cielo Biosphere Reserve", "Archived copy". Archived from the original on 2015-03-05. Retrieved 2014-12-18.CS1 maint: archived copy as title (link), accessed 18 Dec 2014
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