The caves were discovered by chance in 1906 during the excavation of a water well.
The interior remains at a constant temperature year-round, typically hovering around 20 degrees Celsius.
The formations are composed of calcareous rock, which continues to evolve slowly through mineral deposits from dripping water.
The total length of the cave galleries is approximately one kilometer, though only a portion is accessible to the public.
The cave is formed from Miocene-era limestone, common throughout the island of Mallorca.
Coves de Gènova are a series of subterranean limestone caverns discovered in 1906 located directly beneath a restaurant in the Palma neighborhood of Gènova. The cave system consists of a network of natural tunnels and galleries sculpted by water erosion over centuries. Visitors descend approximately 36 meters below ground level to view formations including stalactites, stalagmites, and coral-like pillars. The route follows a structured path through several interconnected chambers characterized by high humidity and consistent temperatures. The site functions as a small-scale geological exhibit rather than a vast cavern system. The cave entrance is accessed through the interior of the Cuevas de Gènova restaurant premises. It remains one of the few cave systems in Mallorca situated within an urban residential district.
The central chamber where the cavern walls narrow, offering a vertical perspective of the stalactite structures.
Wear shoes with good grip, as the limestone floor can become damp and slippery.
The caves are narrow in sections, so avoid bringing large backpacks or bulky gear.
Check the restaurant's operational status before traveling, as the cave access is dependent on the premises.
Do not expect a vast subterranean cathedral; the site is intimate and compact.
Closed on Mondays throughout the year.
Do not touch the rock formations, as oils from human skin can disrupt the calcification process.
