Metadata
Author: ParaCrawl Corpus
Data
English[en]
Perennially snow-capped, Mont Blanc rises at the center of a 40km long mountain range that originated in the Tertiary Era, is composed of granite, metamorphic rocks and sedimentary rocks, mainly quartz.
Spanish[es]
Perennemente nevado, el Mont Blanc se eleva en el centro de una cordillera de 40 km de largo que se originó en la Era Terciaria, comenzando hace 65 millones de años.