The park contains the Buseo Reservoir, which was built in 1915 and is one of the oldest in the Valencian Community.
The Chera Graben is a unique geological feature where the earth's crust has dropped significantly between two parallel fault lines.
The park houses the 'El Tio Jose' cave, which contains archaeological evidence of prehistoric human occupation.
The region is known for a high density of fossils from the Jurassic period embedded in its limestone cliffs.
It is designated as a Geopark candidate site due to its significant tectonic and geomorphological interest.
Chera-Sot de Chera Natural Park is a protected geological area spanning over 6,000 hectares in the interior of the province of Valencia. It is defined by the confluence of the Reatillo and Sot rivers, which have carved deep canyons through limestone and dolomite rock formations. The park features a complex geological structure known as the Chera Graben, characterized by significant fault lines and diverse sedimentary layers. Visitors can access various natural swimming pools and river beaches formed by natural damming. The landscape includes diverse habitats ranging from Mediterranean scrubland to dense forests of Aleppo pine and oak. Extensive trail networks link the municipalities of Chera and Sot de Chera, passing through zones of high botanical and faunal diversity.
The viewpoint overlooking the Buseo Reservoir or the limestone cliffs along the Reatillo river canyon.
Bring water-appropriate footwear with grip, as riverbeds and limestone paths can be slippery.
Check local weather forecasts for heavy rain, as flash flooding can occur in the canyons and riverbeds.
Carry your own waste away, as there are limited facilities for trash disposal within the interior hiking trails.
Attempting to swim in river sections marked as ecologically protected or having unstable, steep banks.
