The “Palude del Capitano” is a small coastal cenote on the Ionian slope of Apulian Salento Peninsula in Italy. This coastal pool is of hyperkarstic origin and is characterised by inconstant hypothermal brackish water inflow. Its formation is due to the collapse of the roof that once covered a large underground cavity, leaving uncovered, in sunlight, a hitherto completely dark underground environment.
Gradually, this cenote illuminated by the sun was also colonised by photophilic species such as algae and aquatic plants. The chemical nature of this water is the results of freshwater mixed to the saltwater coming from the sea. The collapse of the vault of the ancient cavity also gave origin in some areas of the pool, to laminar walls (which was also replicated in the BAM), the result of the vertical collapse of entire portions of limestone.
The sea – at about 800m distance – is connected with the pool by submerged natural tunnels. The pool reaches a maximum depth of 3m.
- GPS
- 40.2041855, 17.9258003
- Geographical region
- Southern Europe
- Drainage Basin
- Ionian coast of Puglia Region
- River catchment
- Water body type
- Pool
- Water body name
- Palude del Capitano
- Water body part
- Pool
- Water body course
- Water body: tributary of
- Channel
- Tributary name














