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

Costa Quebrada is a stretch of Cantabrian coastline approximately 15 kilometres long running between Covachos beach to the east and Liencres to the west, on the western coast of Cantabria. The name is precise: the rock is broken, fractured, tilted. What makes this sector of the Cantabrian coast exceptional is that the Cretaceous Flysch strata of sandstone and clay, deposited horizontally on the seafloor around 90 million years ago, were subsequently folded and tilted by tectonic forces until they stand nearly vertical, perpendicular to the coastline. The sea attacks this structure with northerly swells and over thousands of years has eroded the softer layers while leaving the harder ones standing, producing a system of ridges, sea stacks, islets and arches that is unmatched in frequency and intensity anywhere else on the Spanish Cantabrian coast. The Parque Natural de las Dunas de Liencres y Costa Quebrada has protected the area since 1986.

The best-known and most accessible viewpoint is the area around Somocuevas beach, from which a low-difficulty coastal path allows walking above the cliffs with direct views of the flysch ridges emerging from the sea. La Portilla arch — a natural rock bridge with an approximately eight-metre span, opened by wave action in a sandstone slab — is the most photographed formation on this coastline. When the sea runs strong, water strikes the interior of the arch and rises in columns visible from the path above. The bufas — water jets that shoot through vertical rock fissures during storms — are another phenomenon visitors seek out on rough-sea days between October and March.

Liencres beach and its associated dune system form the park's other major natural element. The Liencres dunes are the most extensive in Cantabria: around 150 hectares of mobile and semi-fixed sand stabilised by psammophilous vegetation including marram grass and several species of sea thistle. The estuary of the Río Pas, which flows into the Liencres inlet, adds habitat diversity that broadens the park's faunal richness: migratory waders, wintering wildfowl and grey heron as a year-round presence. The saltmarsh at the Pas mouth has been subject to halophyte vegetation restoration work in recent years.

The most-used access to the protected area is from Santander, about 16 kilometres to the east. The Cantabrian capital has good road links to the park and concentrates the accommodation offer for those using Costa Quebrada as a day destination or as a complement to a city stay. The villages of Liencres, Arce and Mortera in the municipality of Piélagos are the nearest support points to the park. The PR-S 3 trail, which follows the coast between Liencres and Covachos with constant views of the flysch, is the most complete route for exploring the entire protected area in a day's walking of low to moderate difficulty.

Practical information

Everything you need to know for your visit to Costa Quebrada

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

Find the best plans and things to do in Costa Quebrada

20

Accommodations

Best accommodation options in Costa Quebrada

Loading accommodation options...

Frequently Asked Questions

Get answers about Costa Quebrada

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.
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.
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.
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.
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.