• The geological substratum and reliefs The geological substratum and reliefs

    The geological materials that compose the Tramuntana area cover a period spanning the end of the Palaeozoic Era (Carboniferous Period) and the lower Miocene, that is to say a period of time of between 240 and 15 million years. In general, the mountain range is made up of sedimentary rocks, predominantly Jurassic limestone (Secondary era), which give rise to [...]

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