Cap de Creus in late autumn AI-pedia

The Cap de Creus (Spanish: Cabo de Creus) is a rocky peninsula and headland situated in the comarca of Alt Empordà, within the province of Girona in northeastern Catalonia. Located approximately 25 kilometres south of the border between Spain and France, the cape marks the easternmost point of Catalonia, mainland Spain, and the entire Iberian Peninsula. The headland represents the physical terminus of the Pyrenees, where the mountain range sinks directly into the western Mediterranean Sea. In 1998, the terrestrial and marine zones of the peninsula were granted formal environmental protection under the designation of the Parc Natural del Cap de Creus, encompassing roughly 190 square kilometres of distinct geological formations, scrubland, and deep marine waters.

In late autumn—a period spanning mid-November through late December—the peninsula undergoes an environmental and structural transformation. The heavy summer tourist traffic, which fills the arterial roads and coves around Cadaqués and El Port de la Selva, recedes completely. The region enters a period of severe climatic exposure governed by the Tramuntana, a powerful, dry northerly wind that strips the landscape of lingering warmth and generates volatile maritime conditions. As seasonal hospitality venues and cultural facilities shutter their operations, the peninsula assumes a stark, isolated character dominated by bare metamorphic rock, turbulent seas, and sharp optical clarity.

Late autumn alters both the functional access to the peninsula and its natural ecology. While lower ambient temperatures, gale-force gusts, and maritime spray make outdoor travel demanding, the absence of human congestion reveals the stark geomorphology that inspired regional artists, including Salvador Dalí. Understanding Cap de Creus during this season requires analyzing its underlying geology, its synoptic weather patterns, its botanical and zoological shifts, the demography of its winter-dormant coastal villages, and the practical demands placed on anyone attempting to navigate its terrain.

Geographical and Geological Framework

The Cap de Creus peninsula covers an area of approximately 190 square kilometres (73 square miles). It projects eastwards into the Gulf of Lion, bordered to the north by the Bay of El Port de la Selva and to the south by the Gulf of Roses. Its interior consists of steep, rugged foothills belonging to the easternmost extension of the Serra de Rodes, a sub-range of the Pyrenees. Instead of terminating in wide coastal plains or sandy beaches, these mountains drop sharply into the sea, forming high maritime cliffs fractured by dozens of narrow, sheltered, rocky inlets known locally as cales (creeks or coves).

Geologically, Cap de Creus is among the most important outcrops of the Variscan (or Hercynian) basement in the Mediterranean. The bedrock consists predominantly of Paleozoic sedimentary rocks that underwent intense regional metamorphism during the late Carboniferous and early Permian periods (roughly 300 million years ago). These metamorphic rocks are primarily mica-schists, phyllites, and migmatites. During the final stages of the Variscan orogeny, these dark, layered metamorphic basements were injected by magmatic intrusions, resulting in widespread networks of lighter-coloured pegmatite dykes and veins composed of quartz, feldspar, and tourmaline.

Differential erosion has sculpted these rock units into a jagged, hyper-textured landscape. The schists display a marked vertical or steeply dipping schistosity (parallel alignment of mineral grains under high pressure). This structure allows rain, wind, and salt crystallization to fracture the stone into thin plates and jagged spines. In contrast, the hard, crystalline pegmatites resist chemical breakdown and mechanical wear far more effectively. Over millions of years, the softer surrounding schists eroded away, leaving bright, distorted pegmatite ridges protruding like bones through the dark stone matrix.

This process of selective erosion is heavily amplified by two coastal weathering mechanisms: salt weathering (haloclasty) and aeolian (wind-driven) abrasion. As sea spray driven by autumn gales settles on exposed rock faces, moisture evaporates rapidly in the dry air, forcing salt crystals to grow inside microscopic pores and fissures. The pressure exerted by these expanding crystals fractures the rock from within. Concurrent sand- and dust-blasting by prevailing winds scours out soft layers, producing alveoli (honeycomb-like pits), tafoni (cavernous rock cavities), and zoomorphic monoliths. At the Pla de Tudela, situated on the northern flank of the cape, these processes have generated mineral figures that closely resemble animals, including shapes traditionally identified as camels, eagles, and sea lions.

Late Autumn Meteorology and the Tramuntana

The transition into late autumn over Cap de Creus is characterized by the establishment of cold-season synoptic weather systems over Western Europe. Between mid-November and the winter solstice in late December, the regional climate shifts from the moderate warmth of early Mediterranean autumn into a system dominated by intense barometric gradients and sub-polar air masses.

The Mechanism of the Tramuntana

The defining meteorological force of Cap de Creus is the Tramuntana (Catalan pronunciation: [tɾəmunˈtanə]; Spanish: Tramontana). The name derives from the Latin transmontanus, meaning "beyond the mountains" or "across the mountains." This wind originates when an Atlantic or continental high-pressure system settles over the British Isles, France, or the Bay of Biscay, while a dynamic low-pressure system (often a Genoa low) forms over the Mediterranean or the Gulf of Genoa.

This pressure distribution pulls cold, dense air masses southwards across continental Europe. As this moving air reaches the formidable topographic wall of the Pyrenees and the French Massif Central, it cannot easily cross the mountain crests. Instead, the airflow is channeled and compressed through the gap between these two ranges: the low-lying corridor of the Garonne and Aude valleys in southwestern France. This compression produces an intense Venturi effect, an aerodynamic principle where fluid or air velocity increases sharply as it is forced through a constricted space.

Upon exiting the corridor and entering the open water of the Gulf of Lion, the air accelerates unobstructed toward the Mediterranean. The Cap de Creus peninsula, projecting far out into the sea, acts as an exposed coastal breakwater that intercepts the direct path of these north-northwesterly gales. During late autumn, Tramuntana episodes frequently reach sustained gale-force speeds (above 60 km/h) with violent gusts exceeding 100 to 140 km/h (62 to 87 mph). These wind events typically endure for three, seven, or even nine consecutive days without cessation.

Atmospheric Properties and Thermal Conditions

The late autumn Tramuntana possesses distinct physical characteristics that separate it from other Mediterranean winds:

• Extreme Low Humidity: Because the air mass loses much of its moisture via precipitation on the northern, French slopes of the Pyrenees (a process known as orographic lift) and warms adiabatically as it descends the southern foothills, the Tramuntana arrives at Cap de Creus as a dry, desiccating wind. Relative humidity frequently drops below 30 percent, even while blowing directly over the coastline.
• High Atmospheric Transparency: The dry, turbulent air scours the lower troposphere of maritime haze, suspended aerosols, and airborne pollutants. As a result, late autumn days during a Tramuntana event exhibit hyper-real optical clarity. The snow-capped summits of the Canigó massif (2,784 metres) in the eastern Pyrenees become visible in sharp detail from coastal headlands, and the sea assumes a deep, saturated navy-blue colouration.
• Wind Chill and Evaporative Cooling: While the geographic position of Cap de Creus moderates baseline air temperatures—late autumn daytime highs typically range from 11°C to 15°C (52°F to 59°F), dropping to 4°C to 8°C (39°F to 46°F) at night—the high wind speeds dramatically increase convective heat loss. The wind chill factor routinely makes outdoor conditions feel sub-freezing.

Maritime Disturbance and Easterly Storms

The sea surrounding Cap de Creus reflects the seasonal atmospheric turbulence. Late autumn gales blowing against the southwestward Mediterranean surface current generate steep, short-period waves known for unpredictable swells. The interaction between gale-force offshore winds and deep water shears the tops from wave crests, filling the maritime boundary layer with aerosolized salt spray, known locally as bram or fum de mar (sea smoke).

Although the Tramuntana accounts for the majority of late autumn weather, the season is occasionally interrupted by deep easterly or southeasterly maritime depressions known as Llevantades. When moist Mediterranean air blows from the east directly against the high Pyrenean foothills, it can release torrential precipitation over the peninsula within 24 to 48 hours. These episodes cause sudden localized flash flooding through steep, usually dry ravines (rieres), trigger rockfalls along coastal cliff paths, and batter the eastern headland with massive, long-period oceanic breakers.

Flora and Fauna in Late Autumn

The environmental forces of late autumn—especially sustained desiccation, physical wind battering, and salt-laden spray—place rigorous selective pressure on the local biological communities. Most of Cap de Creus is devoid of dense forest cover, a combined result of its extreme wind exposure, shallow, rocky soils, and historical human clearing for firewood and livestock grazing.

Vegetation Patterns and Seasonal Dormancy

The peninsula's flora is dominated by Mediterranean low scrub formations: garrigue on calcareous pockets and maquis on siliceous, acidic schists. By late November, the intense reproductive phase of Mediterranean plants has concluded, and vegetation enters a semi-dormant winter state to preserve moisture against the wind.

The coastal fringes are populated by halophytic (salt-tolerant) and wind-adapted cushion plants, known in Catalan as coixinets espinosos. Species such as the sea lavender (Limonium tremolsii, endemic to this sector of the coast) and the thorny salad burnet (Sarcopoterium spinosum) form compact, hemispherical mounds that hug the bare rock. This aerodynamic shape reduces wind drag, minimizes transpiration, and traps warm air within the internal branches.

Further inland, the vegetation consists of low-growing aromatic and sclerophyllous (hard-leaved) shrubs:

• Cistus Species (Rockroses): Cistus monspeliensis (narrow-leaved rockrose) and Cistus albidus (grey rockrose) dominate open hillsides. In late autumn, their foliage darkens and hardens to withstand salt deposition and dry air.
• Lentisc and Wild Olive: Pistacia lentiscus and Olea europaea var. sylvestris grow extensively across sheltered valleys. On exposed, windward ridges, they are physically stunted and shaped by continuous wind shear into prostrate mats creeping across the stone.
• Maritime Pinewoods: Aleppo pines (Pinus halepensis) and stone pines (Pinus pinea) exist in small, fragmented pockets, primarily on south-facing or sheltered hillsides. Near the outer headlands, individual trees exhibit extreme flag-form growth, with branches developing exclusively on the leeward side away from the north wind.

In late autumn, the deciduous understory elements, such as wild fig trees (Ficus carica) growing within damp rock crevices, lose their foliage, exposing the pale grey rock architecture beneath.

Avian Presence and Winter Migration

Cap de Creus is a prominent geographical milestone for migratory birds following the western Mediterranean flyway. Because the Pyrenees present a physical barrier to east-west bird movement, many avian species follow the coastline southwards around the eastern end of the mountain range.

By late November, the main wave of trans-Saharan passerine migrants has passed, and the peninsula becomes a temporary stopover or permanent wintering territory for specialized Palearctic species:

• Pelagic Seabirds: Offshore waters, enriched by late-autumn vertical mixing of nutrient layers, support foraging populations of Balearic shearwaters (Puffinus mauretanicus), Yelkouan shearwaters (Puffinus yelkouan), northern gannets (Morus bassanus), and various species of gulls, including the Audouin's gull (Ichthyaetus audouinii). During northerly gales, these birds can often be observed close to the cliffs, utilizing turbulent updrafts for dynamic soaring.
• Raptors and Cliff Dwellers: The high, fractured cliffs of the peninsula accommodate resident peregrine falcons (Falco peregrinus) and eagle owls (Bubo bubo). In late autumn, the wallcreeper (Tichodroma muraria) occasionally descends from high Pyrenean elevations to winter on the sheer limestone and schist cliffs of Cap de Creus and the walls of the ruined monastery of Sant Pere de Rodes.
• Wintering Passerines: The open garrigue provides feeding grounds for cold-weather migrants escaping central European winters, including black redstarts (Phoenicurus ochruros), European robins (Erithacus rubecula), meadow pipits (Anthus pratensis), and various warbler species that exploit late-season berries on juniper and lentisc shrubs.

Human Settlement and Off-Season Life

The human geography of Cap de Creus changes radically between the height of summer and the late autumn months. During July and August, the urban cores of Cadaqués, El Port de la Selva, and Llançà swell with tens of thousands of seasonal residents, day-trippers, and recreational boaters. By mid-November, the peninsula enters a phase of stark demographic retraction.

Cadaqués

Cadaqués, historically the most prominent village on the peninsula, sits on an eastern bay sheltered from the direct brunt of the Tramuntana. Until the early 20th century, the village was virtually cut off from the interior of Catalonia by the rugged Serra de Rodes, relying on coastal maritime transport rather than land-based roads for commerce with Figueres and Barcelona. This historical isolation preserved its distinctive urban form: tightly packed, whitewashed masonry houses, steep slate-paved streets (rastells), and a vernacular architecture adapted to steep slopes and coastal winds.

In late autumn, the village returns to its baseline permanent population of around 2,800 residents. The vast majority of holiday apartments, souvenir shops, and seasonal seafood restaurants secure their wooden shutters against winter gales. The municipal beachfront, crowded with swimming platforms and anchored yachts during the warmer months, is emptied. Small fishing dinghies and traditional wooden craft (llauts) are hauled up onto the dry gravel beaches of the inner bay to protect their hulls from storm surges.

Daily human activity centers on the town’s primary civic axis: the municipal market, local bakeries, the pharmacy, and a handful of historic cafés along the waterfront promenade. The atmosphere shifts from an international tourist resort to an introspective, quiet coastal community where Catalan is the primary language spoken in public spaces.

El Port de la Selva and Llançà

Situated on the northern edge of the peninsula, El Port de la Selva faces directly into the path of the Tramuntana. In late autumn, the village feels exceptionally desolate. The wind often whips sea spray directly into the streets facing the harbour, forcing pedestrians indoors. The local economy relies more heavily on commercial fishing than Cadaqués does; its active fishing fleet operates throughout late autumn, heading out into the Gulf of Lion whenever wind conditions drop below dangerous storm thresholds.

Further west along the rail corridor, Llançà functions as an administrative and residential center with a more continuous year-round domestic life, serving as an access node for the northern sections of the Natural Park.

Operational Changes and Infrastructure

The late autumn visitor encounters a radically downscaled infrastructure across the entire peninsula:

Facility / Service	Summer Status (June–August)	Late Autumn Status (Nov–Dec)
Lighthouse Access Road (GI-614 / Cape Road)	Regulated; private vehicular access often restricted; mandatory shuttle buses.	Fully open to private motor vehicles, barring emergency closures during extreme gales.
Far de Cap de Creus Restaurant	Continuous daily service, high volume.	Limited weekend operations or shuttered entirely for winter maintenance.
Dalí House-Museum (Portlligat)	Open daily; tickets strictly booked weeks in advance; continuous visitor flow.	Severely reduced operating hours; advance reservation still mandatory, but visitor counts drop to a fraction of summer capacity; closed on select weekdays.
Sant Pere de Rodes Monastery	Open daily, extended hours; guided tours; heavy coach traffic.	Shortened winter hours (typically 10:00 to 17:30); closed Mondays; minimal pedestrian traffic.
Public Bus Transport (SARFA)	Frequent daily connections between Figueres/Girona and Cadaqués.	Reduced off-season timetable serving commuter and resident schedules.

Historical and Cultural Heritage

The stark conditions of Cap de Creus have informed human history, spirituality, and artistic output for millennia. Late autumn, with its barren geology and atmospheric isolation, brings these cultural connections to the fore.

Mythology and Ancient Navigation

According to ancient Greco-Roman myth, the Cap de Creus was carved directly from the Pyrenean rock by Hercules. The cape represented a critical, hazardous landmark for ancient Mediterranean navigators. Greek mariners from Rhodes and Phocaea, who founded the trading colonies of Rhode (Roses) and Emporion (Empúries) in the nearby Gulf of Roses between the 8th and 6th centuries BCE, had to round the treacherous headland to reach trading posts in southern Gaul.

The combination of sudden Tramuntana gales and submerged rocky reefs (such as the reef of En Callau) caused numerous shipwrecks throughout classical antiquity, the Middle Ages, and the early modern period. Archeological surveys have discovered numerous Greek, Roman, and medieval shipwrecks embedded in the seabed of the coves surrounding the cape, many carrying cargo such as Dressel 1 amphorae loaded with wine and garum.

Sant Pere de Rodes

Overlooking the peninsula from a granite shoulder of the Serra de Rodes, at an elevation of roughly 520 metres above sea level, stands the Benedictine monastery of Sant Pere de Rodes. While legends trace its foundation to 750 AD when monks supposedly arrived with relics of Saint Peter to protect them from invaders, the earliest documentary evidence dates to 878 AD. The monastery achieved its architectural and political peak between the 10th and 12th centuries, governing vast territorial holdings across the Empordà and Roussillon.

The monastery is a monumental example of early Romanesque architecture. Its church, consecrated in 1022, displays towering barrel vaults, asymmetric side aisles, and ornate marble capitals influenced by classical Roman architecture. High above the complex sits the ruined medieval watchtower and fortress of the Castle of Sant Salvador de Verdera, which offered visual defense across both the Gulf of Roses and the Pyrenean peaks.

In late autumn, the monastery experiences extreme environmental exposure. Dense maritime fog banks (known as boires) frequently roll up the mountain slopes from the Mediterranean, obscuring the stone ruins before being abruptly shredded by gale-force Tramuntana gusts. The sensory experience of visiting the monastic complex in November or December reveals the intense physical isolation endured by the original Benedictine community during the winter months.

Far de Cap de Creus

Standing on a headland 87 metres above the water at the eastern tip of the peninsula, the Far de Cap de Creus (Cap de Creus Lighthouse) is the most prominent maritime safety installation in the comarca. Built under the national Spanish lighthouse plan during the reign of Isabel II, it was first illuminated on May 3, 1853. The lighthouse tower stands 11 metres high, operating a catadioptric rotating lens that casts white flashes visible for up to 20 nautical miles.

The lighthouse station was historically staffed by continuous teams of keepers (faroners) who lived in the attached masonry quarters with their families. During late autumn and winter, the station was frequently cut off from Cadaqués for days at a time by violent windstorms. Today, the light operates automatically under the management of the Port Authority of Barcelona. The former keepers' quarters have housed a small educational facility and a modest hospitality space that operates intermittently outside the peak season.

Salvador Dalí and the Landscape of Surrealism

No individual is more closely identified with the topography of Cap de Creus than the Surrealist painter Salvador Dalí (1904–1989). Born in nearby Figueres, Dalí spent his childhood summers in Cadaqués, where his family owned an estate. In 1930, after breaking with his father, Dalí purchased a tiny, abandoned fisherman’s hut in Portlligat, a shallow, protected cove just north of Cadaqués. Over several decades, he acquired adjoining structures to construct an idiosyncratic, labyrinthine home and studio, which served as his primary creative base until the death of his wife Gala in 1982.

Dalí explicitly acknowledged the geomorphology of the peninsula as the foundational visual lexicon of his Surrealist paintings. In his autobiographical writings, he asserted that he had "solidified his personality" upon the rocks of the cape. The twisted, metamorphic formations of Pla de Tudela, directly shaped by salt and wind, appear repeatedly across his most celebrated works:

• The Great Masturbator (1929): The central, fleshy, profile-like head that dominates this painting is directly modeled upon a specific eroded pegmatite-schist headland in Tudela, often referred to as the "Rock of the Camel."
• The Persistence of Memory (1931): The limp, draped pocket watches rest upon an abstract landscape whose background depicts the stark, amber-toned sea cliffs and rocky headlands of the Bay of Cullaró at Cap de Creus.
• The Enigma of Desire (1929): Features a vast, perforated geological mass directly inspired by the honeycombed tafoni and wind-drilled cavities of the local stone.

In late autumn, the visual quality of the peninsula closely mirrors the lighting conditions found in Dalí’s classical period. The low seasonal solar angle casts long, distinct shadows across the schist plateaus, while the hyper-transparent atmosphere strips the landscape of aerial perspective, causing distant Pyrenean mountain ranges to appear artificially close to the viewer.

Outdoor Recreation, Navigation, and Safety

Visiting Cap de Creus in late autumn requires different preparations than a standard Mediterranean excursion. The combination of deserted trails, unpredictable meteorological shifts, and rough terrain necessitates self-sufficiency and attention to environmental conditions.

Hiking Networks

Late autumn is regarded by serious hikers as the optimal season for traversing Cap de Creus on foot, provided wind speeds remain within safe margins. The summer heat, which can easily exceed 35°C (95°F) on these shade-less, sun-baked stone plateaus, is replaced by crisp, invigorating air.

The peninsula contains several marked footpaths:

• GR 11 (Senda Pirenaica): The grand-route long-distance trail spanning the entire Pyrenees from the Atlantic Ocean (Cabo Higuer) reaches its official eastern Mediterranean terminus directly at the Far de Cap de Creus. The final stage runs from Llançà or El Port de la Selva, crossing the rugged monastic spine of Sant Pere de Rodes down to the sea.
• Camí de Ronda (GR 92): The classic coastal route connects coastal villages, rounding steep sea cliffs and descending into secluded coves. In late autumn, trails like the segment connecting Cadaqués to Portlligat, Cala Bona, and the cape lighthouse can be hiked without encountering other visitors.
• Itinerari de Tudela: A protected, formalized pedestrian circuit winding through the core of the Pla de Tudela geological reserve. The path is paved in places to prevent off-trail foot erosion on delicate lichens and fragile rock surfaces.

Environmental Hazards and Precautionary Measures

Despite its accessibility by paved road, the peninsula in late autumn presents distinct hazards:

• Wind-Induced Instability: Gusts exceeding 100 km/h can easily knock a hiker off balance. Traversing narrow, exposed cliffside sections—such as the crests around Punta dels Farallons or the ridge above Sant Salvador—is dangerous during Tramuntana episodes. Wind-driven stones and debris can also cause eye injuries.
• Exposure and Hypothermia: Because of the high wind chill factor and sudden drops in barometric pressure, hypothermia is a genuine risk for poorly equipped walkers. Hikers require windproof and waterproof outer layers (hardshell jackets), thermal base layers, and gloves, despite the southern Mediterranean latitude.
• Navigational Isolation: Away from the main paved road to the lighthouse, mobile phone reception is weak or non-existent in deep coves and behind steep schist massifs. With seasonal properties shuttered, finding assistance in an emergency can be difficult.
• Rough Surface Friction: The metamorphic rock of the cape is hard, jagged, and abrasive. Stumble injuries can cause severe lacerations on the razor-sharp schist plates. Sturdy footwear with rigid, thick-tread soles is essential.

Environmental Protection and Landscape Restoration

The modern status of Cap de Creus as an ecological reserve was hard-won. During the late Francoist era and the regional tourism boom of the 1960s and 1970s, the peninsula faced intense pressure from commercial real estate developers wishing to extend the intensive resort models of the Costa Brava northwards.

Creation of the Natural Park

In 1998, the Parliament of Catalonia passed Law 4/1998, formally establishing the Parc Natural del Cap de Creus. The park covers both terrestrial zones (roughly 13,800 hectares across eight municipalities) and marine zones (over 3,000 hectares of surrounding waters). The interior contains multiple levels of legal protection:

• Parc Natural (General Park Zone): Accommodates regulated traditional agriculture, low-impact forestry, and passive recreation.
• Paratge Natural d'Interès Nacional (PNIN): Natural sites of national interest designated for their exceptional aesthetic, botanical, and geological significance.
• Reserva Natural Integral (Strict Nature Reserve): Highest protection tier, applied to areas such as the outer cape (Pla de Tudela, Cap Gros) and select offshore islands (Illa d'En Callau, S'Encalladora). In these sectors, all extractive activities, fishing, anchoring, and off-path hiking are strictly prohibited.

The Ecological Restoration of Tudela

The most celebrated environmental achievement within the park was the deconstruction of the Club Med holiday village at Pla de Tudela. Built in 1961, before any environmental zoning existed, this private resort sprawled across 4.5 hectares of the most geologically and botanically sensitive sector of the peninsula, consisting of nearly 400 masonry bungalows, swimming pools, roads, and non-native landscaping.

Following the abandonment of the site and its expropriation by the regional government, an extensive restoration project was executed between 2009 and 2010. The project systematically dismantled every structure, ground down the masonry to use as foundation backfill for new ecological footpaths, and removed hundreds of metric tons of invasive flora, particularly the South African ice plant (Carpobrotus edulis), which had smothered endemic coastal cushions.

In late autumn, the success of this restoration is particularly evident. Without summer foot traffic, the native vegetation—such as maritime armeria, sea fennel (Crithmum maritimum), and euphorbias—thrives uninterrupted in the skeletal gravels. The landscape has reclaimed its primeval character, displaying raw, sculpted pegmatite and schist formations unobstructed by human installations.

Summary of Off-Peak Atmosphere

Cap de Creus in late autumn presents a sharp contrast to the typical image of the sunny Mediterranean coastline. When the summer crowds disperse and seasonal commerce halts, the headland re-emerges as a volatile, wind-swept maritime frontier. The interaction of deep geological time, harsh atmospheric dynamics, and solitary historic sites creates an austere environment that rewards careful, prepared observation.

See also

• Alt Empordà
• Cadaqués
• El Port de la Selva
• Garrigue
• Geology of the Pyrenees
• Gulf of Lion
• Haloclasty
• Parc Natural del Cap de Creus
• Pegmatite
• Portlligat
• Salvador Dalí
• Sant Pere de Rodes
• Schist
• Tramuntana