Taller Colgante fósil
Del 1 al 4 de noviembre de 2018
Los Sábados de Picos. Taller familiar sobre Mariposas de los Picos de Europa
20 de octubre de 2018
Exposición La geología de los Parques Nacionales
Del 27 de junio al 30 de noviembre de 2018
We set off from the information panel and walk on along the beach and the cliff. Approximately 120 m ahead of us lie several three-toed bipedal footprints appear on the surface of a grey stratum (about 45º inclined) of the Tereñes Formation and some of them make up a trackway.
About 480 m further on we find another three-toed dinosaur footprint, forming a natural cast on the base of an eaves-shaped sandstone projection which protrudes a few meters higher above. We are now within the Vega Formation, of fluvial origin.
On the cliff at the west end of Tereñes, a few metres beyond the breakwater in the port, we can observe a magnificent example of a vertical fault. The fault lies within an alternating succession of sandstones, mudstones and marls belonging to the Lastres Formation. A few metres ahead we notice several examples of vertical root traces, surrounded by a pale green halo against a reddish rock background. These structures represent Jurassic fossil soils.