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メキシコ高原

メキシコ高原(メキシコこうげん、スペイン語: Mesa del Centro)は、メキシコ中央北部の大部分を占めている起伏の激しい台地である。標高は平均で1800メートル(6000フィート)で、総じて北から南に向かって高くなっている。メキシコ高原の東には東シエラマドレ山脈が、西には西シエラマドレ山脈がある。

出典

[編集]
  •  この記事にはアメリカ合衆国内で著作権が消滅した次の百科事典本文を含む: Chisholm, Hugh, ed. (1911). "Mexico". Encyclopædia Britannica (英語). Vol. 18 (11th ed.). Cambridge University Press. p. 317-344.
  • Mexican Plateau, Mexico City Region. Image Science and Analysis Laboratory, NASA-Johnson Space Center. 18 Mar. 2005. Earth from Space - Image Information.
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メキシコ高原
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