La Herradura

La Herradura stacks more variety into a single dive area than most Spanish Mediterranean destinations. Boat dives depart from Marina del Este toward the Maro-Cerro Gordo cliff coast, where the seabed drops through distinct zones: calm sandy coves within the bay, rocky reefs at mid-range depths, then dramatic gorgonian-covered walls plunging past 40 metres at Punta de la Mona and Piedras Altas, where orange coral and dead man's hand colonies cover the deep rock. The bay's horseshoe shape creates natural shelter, so when wind cancels diving elsewhere, La Herradura often stays operational. The ocean sunfish is the area's aspirational sighting, lending its name to Mola Mola Point and drawing photographers in spring and summer. Marina del Este was declared a Natural Reserve in January 2025, adding protection to an area that already supports over a dozen dive operators. Each season brings different highlights: winter draws nudibranch specialists and macro photographers, spring brings sunfish closer to shore, and summer lights up the bay sites with barracuda schools and active cephalopods on night dives.

Wind direction matters more here than at most dive areas. Levante (east wind) warms the water but stirs up visibility; Poniente (west wind) clears the water but drops the temperature. Ask your center about conditions before choosing sites. Access is straightforward from Malaga airport (80 km, 75 minutes) or Granada (75 km, 50 minutes). All diving in the Maro-Cerro Gordo reserve requires an authorized center — individual divers cannot obtain permits independently. Seven or more centers operate from La Herradura and Almunecar, with permit fees included in the dive price. Winter visitors should call ahead to confirm availability, as some shops reduce operations or close between December and March. Night diving exists but requires special authorization within the marine park, so arrange it through your center well in advance.

The Maro-Cerro Gordo cliffs are composed of Mesozoic limestone and dolomite from the Subbetic Zone of the Betic Cordillera, uplifted by Alpine tectonic forces and sculpted by marine erosion into dramatic underwater walls, caves, and swim-throughs. Karstification has created an extensive network of submerged caverns within the cliff face, while the sheltered horseshoe bay collects sandy patches and Posidonia meadows between the rocky formations.