EN

Geosite · Esplegares

Fossil ray traces of Esplegares, from the Lower Jurassic

In Pozón and Buey ravines near Esplegares, Lower Jurassic (Sinemurian) strata expose pits left by rays foraging for food on the seabed some 190 million years ago. It is the oldest known trace fossil site of this type in Spain; the only other known site, at Isona (Lleida), is Cretaceous.

Grey limestone outcrop with many irregular hollows attributed to feeding traces of Jurassic rays.
Ray traces in Barranco del Buey, Esplegares. Photo: «Huellas de batoideos en Bco. del Buey (Esplegares, SW)», Instituto Geológico y Minero de España (IGME-CSIC) · Condiciones de uso del IGME (2022)

This place across time

Which eras you can read here

A single place can preserve traces from different eras. These layers connect what you see with the stories in the atlas.

Municipality
Esplegares
Province
Guadalajara
Altitude
1,119 m
  • Lower Jurassic
  • Trace fossils
  • Oldest in Spain
  • Geosite of interest

A prehistoric seabed turned to stone

Approximately 190 million years ago, during the Lower Jurassic, this sector of the Señorío was submerged under a shallow epicontinental sea. Ancient rays grubbed through soft seabed sediments searching for food, leaving irregular feeding pits. The sediment hardened into stone, and these traces have endured to this day on the upper surface of a bed of grey dolomitic limestone.

Where to see them

They outcrop at several points in the Barranco del Pozón and its continuation, the Barranco del Buey, northeast and southeast of Esplegares. Paleontologists classify them under the ichnogenus Piscichnus, indicating fish feeding structures.

A rare geological site

Only two trace fossil sites of this specific category are known in Spain: this Jurassic locality and another in Isona (Lleida), which dates from the much younger Cretaceous period. Consequently, the Spanish Geological Survey (IGME) catalogues it as an official geosite of scientific interest. It is best observed under low-angled raking sunlight in early morning or late afternoon.

Frequently asked questions

What are the ray trace fossils of Esplegares?

They are irregular pits preserved on the bedding plane of grey dolomitic limestone, formed when Jurassic rays grubbed into the soft seabed while foraging for prey. Geologists classify them as ichnofossils (trace fossils): marks left by an organism's biological activity rather than preserved skeletal remains.

Location

Location: Fossil ray traces of Esplegares, from the Lower Jurassic EsplegaresSacecorboCanales del DucadoSaelices de la SalClimbing in Barranco de la HozCueva de las Majadillas (Sacecorbo): the caving schoolGuided visit to Saelices de la Sal saltworksSan Juan Salt Pans (Saelices de la Sal)Hoz del Río Ablanquejo: a wild, pathless canyonSaelices de la Sal Pillbox: memory of the Spanish Civil War EsplegaresSacecorboCanales del DucadoSaelices de la Sal Reference
Atlas diagram. Fossil ray traces of Esplegares, from the Lower Jurassic: large reference point. Rivers: © OpenStreetMap.

● Reference point · ● Villages · ● Places

Location diagram. Detailed map with tracks and names loads on zoom.

Reference villages: Esplegares · Sacecorbo · Canales del Ducado · Saelices de la Sal.

Open the full map and historical layers →

Directions (Google Maps) OpenStreetMap View on 1930s map

More geology and geosites nearby

View all →

Nearby routes

All routes →