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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.
Ring of cenotes of Chicxulub Crater, Yucatan Yucatán: 2012 vii (natural) This nomination comprises 99 cenotes, or sinkholes, that formed on the rim of the Chicxulub crater. The crater, with a diameter of 180 km (110 mi), formed following the meteorite impact that was the main reason for the Cretaceous–Paleogene extinction event.
Three prehistoric human remains have been found within the subsystem. The Jailhouse cenote, or Las Palmas, is the entrance to the locations of the Muknal and Las Palmas caves. The skeleton of an 18 to 20-year-old woman, Eve of Naharon, (13,454±117 cal BP) was discovered at a location around 368 m (1,207 ft) away from the Jailhouse cenote entrance.
The Deer circuit features two water landings. The Jaguar circuit features higher and longer zip lines for those seeking extra thrill. The Hammock Splash is a beginner zip-line where visitors splash into a cenote with one shorter and lower zip line. The park features an All-terrain vehicle track labeled as Amphibious Vehicles.
The Sacred Cenote at Chichen Itza. The Sacred Cenote (Spanish: cenote sagrado, Latin American Spanish: [ËŒsenote 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.
Of these cenotes, the "Cenote Sagrado" or "Sacred Cenote" (also variously known as the Sacred Well or Well of Sacrifice), is the most famous. [11] In 2015, scientists determined that there is a hidden cenote under the Temple of Kukulkan, which has never been seen by archeologists. [12]
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