Trans-Mexican Volcanic Belt

Trans-Mexican Volcanic Belt
Stratigraphic range: Neogene to Quaternary
Six Mexican Volcanoes
Left to right Iztaccíhuatl, Popocatépetl, Matlalcueitl (Malinche), Nauhcampatépetl (Cofre de Perote, most distant), Citlaltépetl (Pico de Orizaba), Sierra Negra
TypeVolcanic arc[1]
OverliesSierra Madre Occidental[1][2]
Area160,000 kilometres (99,000 mi)2 [1]
ThicknessEast of 101°W 50-55 km[1] West of 101°W 35-40 km[1]
Location
Coordinates19°02′N 97°16′W / 19.03°N 97.27°W / 19.03; -97.27.
RegionCentral Mexico
CountryMexico
Extent1,000 kilometres (620 mi) [3]

The Trans-Mexican Volcanic Belt (Spanish: Eje Volcánico Transversal), also known as the Transvolcanic Belt and locally as the Sierra Nevada (Snowy Mountain Range),[4] is an active volcanic belt that covers central-southern Mexico. Several of its highest peaks have snow all year long, and during clear weather, they are visible to a large percentage of those who live on the many high plateaus from which these volcanoes rise.

  1. ^ a b c d e Cite error: The named reference FOEMM was invoked but never defined (see the help page).
  2. ^ Cite error: The named reference SQ was invoked but never defined (see the help page).
  3. ^ Cite error: The named reference FMM was invoked but never defined (see the help page).
  4. ^ Delgado de Cantú, Gloria M. (2003). México, estructuras, política, económica y social. Pearson Educación. ISBN 978-970-26-0357-3.

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