Ox Bel Ha cave system

Area: Tulum South

Length: 258,791 m

Maximum depth: 57.3 m

Sistema Ox Bel Ha came from the Mayan language which means "three paths of water." It is a classic example of a coastal cave. Its main feature is a higher fresh water layer flowing on top of a near-static saltwater layer, one that intrudes from the nearby Caribbean Sea. This creates a halocline, or a mixing zone, between unequal water densities. The halocline can be found at different depths; depths gradually increase as the distance to the ocean increases. For this reason, fresh water layers will be thicker inland where the salt water is less intrusive. In Ox Bel Ha, the halocline can be found anywhere between 25 ft-50 ft deep.

A change in water level due to daily tidal change is visually apparent in the numerous cenotes. In reality, however, only a few of the area cave systems connect directly with the Caribbean Sea. Many empty into mangrove beds and wetland savannah, others in caletas (small bays), and still others eventually reach the ocean, but only through a myriad of small voids in the limestone bedrock.

Exploration

Caves

Connected systems

All the cave systems of the Yucatán