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The Sacred Cenote at Chichen Itza, Mexico. Cenotes are surface connections to subterranean water bodies. [5] While the best-known cenotes are large open-water pools measuring tens of meters in diameter, such as those at Chichen Itza in Mexico, the greatest number of cenotes are smaller sheltered sites and do not necessarily have any surface exposed water.
The Sacred Cenote at Chichen Itza. The Sacred Cenote (Spanish: cenote sagrado, Latin American Spanish: [ˌsenote saˈɣɾaðo], "sacred well"; alternatively known as the "Well of Sacrifice") is a water-filled sinkhole in limestone at the pre-Columbian Maya archaeological site of Chichen Itza, in the northern Yucatán Peninsula.
Cenote Ik Kil is near the Maya [2] ruins of Chichen Itza, on the highway to Valladolid. Ik Kil was considered sacred by the Maya who used the site as a location for human sacrifice to their rain god, Chaac. Bones and pieces of jewelry have been found in the waters of the cenote by archaeologists and speleologists. [3]
A team of California researchers surveying satellite images found a cenote ring centered on the town of Chicxulub Pueblo that matched the one Penfield saw earlier; the cenotes were thought to be caused by subsidence of bolide-weakened lithostratigraphy around the impact crater wall. [18]
To the north of this arch, on the western edge of the religious pathway lies a small hole in the bedrock, similar to others that can be found throughout the ruins. These natural karst formations are called cenotes (from the Mayan word ‘’d'zonot’’) and served as water sources for the inhabitants of San Gervasio.
A large number of cenotes are located in the Tulum area such as Maya Blue, Naharon, Temple of Doom, Tortuga, Vacaha, Grand Cenote, Abejas, Nohoch Kiin, Calavera,and Zacil-Ha. Tulum has some of the best beaches in Mexico. Most popular beaches in Tulum are Playa Paraiso, Playa Ruinas, Playa Akumal, Papaya Playa and more.
The following is a list of sinkholes, blue holes, dolines, crown holes, cenotes, and pit caves. A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. Some are caused by karst processes—for example, the chemical dissolution of carbonate rocks [1] or suffosion processes. [2]
Chan Hol is derived from Mayan, meaning "little hole". [2] The Chan Hol cave system extends over 5,000 m (16,404 ft) in length. The entrance, via the cenote, is located around 15 km (9 mi) away from Tulum and around 11.5 km (7 mi) from the modern coastline. [3]