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NameCurrent message text
 h English (en){{#category_index:M|mantle}}
The part of the Earth&#x2019;s interior between the core and the crust composed of dense silicate rocks. The upper surface of the mantle is the Moho discontinuity characterized by a sharp increase in P-wave velocity to 8.1&#x00B1;0.2&#x0020;km/s. The density of the mantle is about 3.3&#x2013;3.4 g/cm<sup>3</sup> and the mantle is essentially non-magnetic. The mantle includes the lower lithosphere and the asthenosphere. Below the mantle is the core separated from the mantle by the Gutenberg-Weichert discontinuity. See Figure [[Dictionary:Fig_E-1|E-1]].
 h Spanish (es)La parte del interior de la Tierra entre el núcleo y la corteza compuesta por densas rocas de silicato. La superficie superior del manto es la discontinuidad Moho caracterizada por un fuerte aumento en la velocidad de la onda P a 8.1&#x00B1;0.2&#x0020;km/s. La densidad del manto es de aproximadamente 3.3&#x2013;3.4 g/cm<sup>3</sup> y el manto es esencialmente no magnético. El manto incluye la litósfera inferior y la astenosfera. Debajo del manto está el núcleo, separado del manto por la discontinuidad de Gutenberg-Weichert. Ver Figura [[:File:FIG E-1.png|E-1]].