Costa Quebrada
The essentials of Costa Quebrada
- • La Portilla arch: natural sandstone bridge opened by wave action, visible from the coastal path
- • Near-vertical Cretaceous flysch strata: Cantabrian geology unmatched on the Spanish coast
- • Liencres dunes: 150 ha of active dune system, the largest in Cantabria
- • Blowholes during storms from October to March: water jets shooting through vertical rock fissures
- • Río Pas estuary: habitat for migratory waders and wintering wildfowl
Description
Practical information
Everything you need to know for your visit to Costa Quebrada
How to get there
How to get there
From Santander take the S-20 and local road towards Liencres: 16 km, 20-25 minutes. Local bus from Santander to Liencres on the Piélagos line. Covachos beach is accessible via the CA-231 from Santa Cruz de Bezana.
Area Information
The natural park spans the municipalities of Piélagos and Santa Cruz de Bezana on the western coast of Cantabria, 16 km from Santander. Reference villages are Liencres and Arce. The park is adjacent to the Parque Natural de las Marismas de Santoña to the east.
Geography
Cretaceous flysch strata (sandstone and clay, ~90 Ma) folded to near-vertical position. 15 km coastline with cliffs, arches and sea stacks. Liencres dune system (150 ha) and Río Pas estuary to the west.
Flora & Fauna
Dunes with marram grass and sea thistle. Pas saltmarsh with restored halophyte vegetation. Birds: little egret, grey heron, sandpipers, ringed plover and wintering wildfowl. Great cormorant and yellow-legged gull on the rocky coast.
Things to do
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20
Valle de Mena
Speleology
Desde
€380.00
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Gallery
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Frequently Asked Questions
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What exactly is flysch and why is it unusual here?
Flysch is an alternating sequence of hard sandstone and soft clay layers deposited on the seafloor. At Costa Quebrada, these layers — formed around 90 million years ago — were folded by tectonic forces until they stand nearly vertical. As the sea erodes the softer clay between the harder sandstone laminae, the rock ridges are left standing perpendicular to the coastline. This geological structure is relatively common along the Cantabrian coast, but nowhere else on the Spanish littoral does it occur with such continuous length and pronounced relief.
When is the best time to see the blowholes?
The blowholes — jets of water forced through vertical rock fissures when waves compress trapped air — occur during northerly or north-westerly storms with significant swell. October through March are the most suitable months. It is worth checking the wave forecast (Puertos del Estado website) before visiting: a significant wave height of at least 2-3 metres is needed for the phenomenon to be at its most dramatic.
Is the coastal trail suitable for families with children?
The PR-S 3 section between the Somocuevas car park and La Portilla arch (approximately 2 km one way) is accessible for families with children from around 6-7 years of age who can walk independently. The path is slightly uneven but presents no technical difficulty. Caution should be exercised near cliff edges, especially in strong wind or on wet days. Approaching the blowholes with young children during storms is not recommended.
Where is the best place to park for a park visit?
There are two main car parks: Liencres beach (western zone, access to dunes and estuary) and the Somocuevas path car park (central zone, access to the flysch and La Portilla arch). In summer the car parks fill quickly at weekends; arriving before 10:00 or after 19:00 is advisable. The Covachos car park at the eastern end of the park tends to be less crowded.
Can you swim at Liencres beach?
Yes, Liencres beach is suitable for swimming in summer. It has lifeguard service and safety flags in season. Waves can be considerable on northerly wind days; flag signals from lifeguards should always be respected. Cantabrian sea water temperature ranges between 16 and 20 °C in summer, considerably colder than the Mediterranean.






