Dzibilchaltún (Yucatec: Ts'íibil Cháaltun, d̥z̥ʼiː˧˥biɭ tɕhɒːl˦˥tuŋ) is a Maya archaeological site in the Mexican state of Yucatán, approximately north of state capital of Mérida. In the view of modern researchers, the ancient builders of Dzibilchaltún may have chosen the site of the city to be as close as possible to the coastal salt-producing region (about away), while still being located on a reasonably fertile and habitable terrain. The region between Dzibilchaltún and the sea coast is less suitable for human habitation, being either mangrove swamps or bare rock. The site has been continuously occupied for thousands of years, although it has expanded into a mid-sized city and contracted back to a small town more than once in its long history. It is about 30 minutes north of Mérida, and about the same distance south of the location of the impact site of the meteorite that killed the dinosaurs in Chicxulub. The most famous structure is the Temple of the Seven Dolls, so named because of seven small effigies found at the site when the temple was discovered under the ruins of a later temple pyramid by archaeologists in the 1950s. On the vernal equinox, the site is crowded by visitors observing the sunrise through the temple's doorways. However, there is no archaeological feature marking the observation spot, making any relationship between the orientation of the temple with the equinoxes highly unlikely. The temple is connected to the rest of the site by a sacbe, or "white road," so-called because they were originally coated with white limestone, built over stone-and-rubble fill. The other major feature of Dzibilchaltún is its cenote, Cenote Xlakah, located around the center of the city's ruins. It is thought that the availability of this source of clean drinking water influenced the builders' choice of the location. Archaeological findings retrieved from the cenote by divers indicate that it was the center of a religious cult.