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Cabo Espichel Dinosaur Tracks

Cabo Espichel Dinosaur Tracks

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Pedra da Mua — cliff with Jurassic sauropod trackways

📷 Image credit

Photo: Arseniop / Wikimedia Commons / CC BY-SA 4.0

The coastal cliffs around Cabo Espichel (Sesimbra municipality) preserve hundreds of dinosaur tracks from two geological ages – the Late Jurassic (~160 million years ago) and the Early Cretaceous (~130 million years ago). The complex is one of the most important palaeoichnological sites in Western Europe.

Main sites

Pedra da Mua

Parameter Value
Age Late Jurassic (~160 Ma)
Track levels At least 8
Sauropod trackways 38
Theropod trackways 2
Estimated individuals ~37
Location Coastal cliff south of the cape

Pedra da Mua is the main palaeontological site. The tracks belong predominantly to sauropods – giant quadrupedal herbivores whose rounded footprints reach 80 cm in diameter. Two three-toed trackways were left by theropods – bipedal predatory dinosaurs.

For centuries, local people interpreted the prints as “footprints of the Virgin’s mule” (pegadas da mula da Nossa Senhora), giving rise to the legend that underlies the pilgrimage sanctuary.

Lagosteiros

Parameter Value
Age Early Cretaceous (~130 Ma, Barremian)
Track levels 2
Total tracks 541 (as of 2021)
Dominant type Herbivores (336 tracks)

Lagosteiros is Portugal’s only known Cretaceous dinosaur tracksite. Three types of tracks have been identified:

  • Sauropods – large rounded prints
  • Ornithopods – three-toed herbivorous bipeds
  • Theropods – three-toed predators

In 2021, over 600 new prints were discovered here.

Boca do Chapim and Areia do Mastro

Palaeontological sites on the coast 2 km north of the cape. In addition to tracks, skeletal remains of dinosaurs have been found in the Papo-Seco and Areia do Mastro formations:

  • Megalosauridae, Baryonyx walkeri (predators)
  • Iguanodon, ornithopods (herbivores)
  • Pelorosaurus (sauropods)
  • Crocodilians, turtles, pterosaurs

In 2016, a partially exposed dinosaur skull was found on Areia do Mastro beach.

Geological context

The tracks are preserved in limestone deposited on the floor of shallow lagoons during the Mesozoic Era. Dinosaurs walked across soft muddy beds, leaving impressions that were rapidly buried under sediment and lithified.

Two different ages reflect two periods:

  • Late Jurassic (Pedra da Mua) – 160 Ma, when the area was part of extensive lagoons on the Iberian Peninsula
  • Early Cretaceous (Lagosteiros) – 130 Ma, Areia do Mastro Formation

History of research

Year Event
1884 First scientific description by geologist Nery Delgado
1950s–1970s Systematic studies by Portuguese and French researchers
2000s Inclusion in conservation programmes; geopark designation
2021 Discovery of 600+ new prints at Lagosteiros beach
2022 Publication of Areia do Mastro tracksite data (ScienceDirect)

Nery Delgado described the tracks before palaeoichnology had emerged as a formal discipline. His 1884 paper is one of the earliest scientific descriptions of dinosaur tracks in the world.

Conservation

The sites lie within the Arrábida Natural Park and are protected under palaeontological heritage legislation. Pedra da Mua is viewed from a clifftop lookout (descending to the rocks is dangerous). Lagosteiros is accessible from the beach.

Conservation challenges:

  • Natural erosion (waves, wind) is gradually destroying the prints
  • Tourist footfall
  • Sesimbra municipality restricts access in the most fragile zones

Practical information

Parameter Value
Distance from Setúbal ~40 km (via Azeitão or Sesimbra)
Best time Low tide (for Lagosteiros); any time (Pedra da Mua – viewed from above)
Access Free; car park at the Cabo Espichel sanctuary
Tips Binoculars for viewing Pedra da Mua; sturdy footwear

Cretaceous dinosaur trackway at Lagosteiros

📷 Image credit

Photo: Britoca / Wikimedia Commons / CC0

Panorama of Lagosteiros natural monument

📷 Image credit

Photo: The Cosmonaut / Wikimedia Commons / CC BY-SA 4.0

See also

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