Begur

Begur's coastline packs an unusual range of underwater topography into a compact area. From Aiguablava Beach, boats reach 10+ dive sites in under 10 minutes — granite walls at Cap de Begur where three rocky bars descend to 37 metres in gorgonian forests, the Furió Fitó pinnacle rising from 50 metres to a plateau at 14, parallel canyon formations at Canons de Tamariu, and the crevice-rich multilevel dive at Illa Negra where lobsters, conger eels, and morays share the dark rock. Shore dives at Aiguablava itself include Roman amphora and shipwreck remains on the seabed — one of the few spots on the Costa Brava where recreational divers encounter archaeological artefacts in situ. The area sits between the better-known Illes Medes to the north and the Ullastres pinnacles (accessed from neighbouring Calella de Palafrugell) to the south, and Begur-based centres run excursions to both. What distinguishes Begur's own sites is the exposed headland geology: Cap de Begur juts further into the Mediterranean than any other point on this stretch, drawing currents and concentrating marine life on its walls.

No permits or reserve fees — Begur's sites are open access, unlike the regulated diving at nearby Illes Medes. Two dive centres operate from the Aiguablava area: Begur Dive (SSI/SDI, rated 4.4/5) is the main operator, based directly on the beach. Boat dives run 39 EUR with own equipment. Cap de Begur and Furió Fitó are weather-dependent and exposed to currents — local sources recommend diving these with a guide who knows the conditions. For beginners, Aiguablava Beach and Sa Tuna are sheltered alternatives with easy shore access. The nearest hyperbaric chamber is in Palamós.

Paleozoic granite from the Catalan Coastal Range batholith forms the entire coastline. Marine erosion along the granite's natural joint planes has carved vertical walls, isolated pinnacles (furiós), and parallel canyon systems (canons). Cap de Begur — the most protruding headland on this stretch of coast — exposes three descending rocky bars to open-water currents, while sheltered coves collect sand and Posidonia meadows between the granite formations.