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Dorsal asísmica

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Una dorsal asísmica es una larga y lineal cordillera submarina. Las dorsales asísmica son volcánicamente inactivas y se suelen ubicar en cuencas oceánicas profundas.[1]​ Un ejemplo es la cadena Walvis en el océano Atlántico.[1]​ En la mayoría de los casos son alineamientos de relieves volcánicos, nacidos a menudo como islas sobre un punto caliente, y luego reducidos luego en volumen por su enfriamiento, y por el adelgazamiento de la litosfera oceánica que ocurre en ésta a medida que se aleja de la dorsal mediooceánica donde se ha formado.

Referencias

  1. ↑ a b Marian Frenegal, José López Gómez and Javier Martín Chivelet. 2001. Diccionario de las ciencias de la Tierra. Pág 255.
Esta página se editó por última vez el 17 mar 2020 a las 00:29.
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