Category: Geological Point

The fossil site of Cuevas Labradas has Jurassic marine invertebrates which, if we look closely, we will see in multitudes under our feet.

The 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.

These Jurassic layers were deposited under a tropical sea that existed in this area and then folded by the Alpine orogeny in the Tertiary.

The experimental area of the Tejera de Checa is dedicated to rocks and minerals and ten lithologies of the Geopark are represented there.

The 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.

The Poljé del Cubillo is a karstic depression in the form of an elongated, closed valley with a flat bottom typical of glacial landscapes.

The Czech graptolites were small marine creatures that lived here about 430 million years ago.

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.

In 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.