The cenote is known locally as 'Dzitnup', named after the village where it is located.
The name 'Xkeken' translates from Mayan to 'pig', referencing a legend about a local farmer discovering the site while searching for a lost pig.
The water depth varies significantly, reaching up to 20 meters in certain areas.
The rock formations inside the cave include extensive drapery and flowstone structures.
The water is naturally filtered through the porous limestone bedrock, maintaining high clarity.
The skylight acts as a natural spotlight, creating shifting visual effects on the cave walls as the sun moves.
A portion of the cave ceiling collapsed long ago, creating the opening that allows light to penetrate the subterranean chamber.
Cenote Xkeken is a partially enclosed limestone cavern located near the town of Valladolid in the Yucatán Peninsula. The cave features a natural skylight in the ceiling that allows a single beam of sunlight to illuminate the turquoise water below. Visitors access the swimming area by descending a stone staircase carved into the rock. The interior is characterized by dense clusters of stalactites and stalagmites formed over centuries. Due to its enclosed nature, the water remains cool and still throughout the year. The site is part of the Dzitnup cenote complex, which also includes the nearby Cenote Samula. Artificial lighting has been installed along the rock walls to enhance visibility for swimmers.
The staircase landing, which captures the contrast between the beam of light from the ceiling and the dark water.
Bring a waterproof camera or phone pouch, as the moisture inside the cavern is constant.
Wear water shoes, as the stone stairs and cave floor can be slippery and uneven.
Shower before entering the water to help maintain the ecosystem, as is standard practice at regional cenotes.
Do not wear sunscreen before showering, as oils and chemicals contaminate the fragile cavern water.
Biodegradable sunscreen and insect repellent are required. Avoid touching the stalactites as skin oils damage the mineral deposits.
