Cenote Suytun lies near Valladolid on Mexico's Yucatan Peninsula, a karst cavern chamber formed by the collapse of limestone into an underlying flooded cave, its water sitting about five meters deep beneath a domed rock ceiling. A single natural opening in that ceiling admits a shaft of sunlight that, around midday, falls directly onto a circular stone platform built into the pool in 2009, when the landowning family opened the site to tourism, creating a dramatic spotlight effect that has made the cenote a widely photographed landmark. Its name, meaning stone center in Yucatec Maya, refers to that same platform. This entity documents Cenote Suytun specifically as a geological formation, a karst cave cenote near Valladolid whose natural ceiling skylight illuminates its built-in stone viewing platform.
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