The name 'Bolochohool' derives from Mayan roots, often translated in local context as 'nine holes' or referring to specific karst subterranean features.
The access route for the Cuzamá cenote circuit utilizes remnants of henequen-era infrastructure, specifically the narrow-gauge railway system used to transport fiber.
The water clarity is maintained by constant filtration through the surrounding porous limestone bedrock, a characteristic of the Yucatán Peninsula's aquifer.
The cenote is a semi-open type, meaning part of the ceiling has collapsed, allowing sunlight to penetrate the cavern.
Cenote Bolochohool is a semi-open karst sinkhole located in the municipality of Cuzamá, Yucatán, known for its clear, cool waters and underground cavern features. It is part of the 'Los Tres Cenotes' circuit, which traditionally requires travel between sites via horse-drawn rail carts on narrow-gauge tracks. The site features a steep wooden staircase descending into the cavern, where rock formations and natural lighting illuminate the water pool. The cenote is maintained by local ejidatarios, preserving the site's natural environment and traditional access methods. Visitors swim in a subterranean pool characterized by limestone walls and hanging roots reaching toward the surface.
The staircase landing, which offers a wide-angle view of the cavern's ceiling collapse and the reflective pool below.
Bring biodegradable sunscreen and insect repellent as they are strictly required to protect the water ecosystem.
Wear water shoes with good grip, as the wooden stairs and stone walkways can become slippery from humidity.
Pack a dry bag for your electronics, as the humidity and splashing during the horse-cart ride can damage gear.
Do not attempt to walk between the cenotes; rely on the traditional horse-drawn carts provided by the local cooperative to navigate the dense forest trails.
Shower before entering the water to remove oils and chemicals; strictly no diving from unstable rock ledges.
