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File:San Martín de Pusa (2005) 04.jpg

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Español: Orillas del río Pusa. San Martín de Pusa (Toledo, Castilla-La Mancha, España) Los bolos cuarcíticos proceden del desmantelamiento de la raña (Plio-Pleistocena) la cual, a su vez, procede del sector Paleozoico de los Montes de Toledo
English: Banks of Pusa River. San Martín de Pusa, Toledo, Castile-La Mancha, Spain The quartzite boulders come from the dismantling of the raña formation (Plio-Pleistocene) which, in turn, comes from the Paleozoic sector of Montes de Toledo
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Author LBM1948

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current11:23, 27 March 2023Thumbnail for version as of 11:23, 27 March 20231,060 × 692 (774 KB)LBM1948 (talk | contribs)Uploaded own work with UploadWizard

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