Category: Geological Point
The Czech Dropstone is a rock that was trapped in glaciers, and when it broke away from the glaciers and fell into the sea, it ended up on the seabed.
Ver másIn the place known as "Hoya de la Parra" is an abandoned meander of the Tagus river, it can be visited following the route of the Taravilla lagoon.
Ver másThe fossil site of Cuevas Labradas has Jurassic marine invertebrates which, if we look closely, we will see in multitudes under our feet.
Ver másThe fossil forest is one of the jewels of the Molina-Alto Tajo Geopark, an area where there are fossil trunks of conifers from the Primary Era.
Ver másThese Jurassic layers were deposited under a tropical sea that existed in this area and then folded by the Alpine orogeny in the Tertiary.
Ver másThe Fuentelsaz Stratotype has been chosen by the IUGS as a boundary stratotype and point for the base of the Aalenian with global significance.
Ver másThe experimental area of the Tejera de Checa is dedicated to rocks and minerals and ten lithologies of the Geopark are represented there.
Ver másThe Terreras de la Virgen or "Carcava de Ribagorda" are produced by the erosion of the land due to deforestation and soil alteration.
Ver másThe ancient volcano of Orea bears witness to the fact that there were volcanoes in this area, although not in the same way as we are used to seeing them.
Ver másThe Valle de los Milagros is carved out of the limestone, sandstone and slate rocks through which the Linares river flows, it is a journey into the past.
Ver másThe Sima de Alcorón is a natural well 63 m deep which is easy to descend as it is equipped for visits.
Ver másThe river of stones of Orea is an accumulation of thousands of quartzite blocks that covers the slope of the Cerro de San Cristóbal.
Ver másThe Tornero Cave is the deepest cave of the Alto Tajo with more than 11 km and its end has not yet been reached.
Ver másThe water really does seem to turn to stone in the Aguaspeña, a waterfall active all year round that is a large tuff in formation
Ver másThe Poljé del Cubillo is a karstic depression in the form of an elongated, closed valley with a flat bottom typical of glacial landscapes.
Ver másThe Czech graptolites were small marine creatures that lived here about 430 million years ago.
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