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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.
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]
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.
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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.
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.
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Looking down into the cenote. The cenote is open to the sky with the water level about 26 metres (85 ft) below ground level. It is about 60 metres (200 ft) in diameter and about 48 metres (157 ft) deep. [1] A carved stairway leads down to a swimming platform. Cenote Ik Kil is near the Maya [2] ruins of Chichen Itza, on the highway to Valladolid.