In the Vegas de Matute massif are represented, in a very small area, most of the metamorphic lithologies found in the central and eastern sectors of the Central System: siliciclastic metasediments (metapelites and metapsammites), carbonate metasediments (marbles and calc-silicate rocks), as well as orthogneisses of plutonic and volcanic origin, and metabasites. In this area, it is also possible to recognize the relationships existing between these lithologies, making this virtual field trip the perfect place to be acquainted with the geology of the Central-Iberian Zone basement. II.

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