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Valladolid was later founded in 1543. [3] The cenote was once the city’s water source. [4] The cenote is in a partially collapsed cavern. [3] The cave is 150 feet across and 260 feet deep. [1] There are some stalactites on the ceiling of the cave. [3] There is a sloped passage with stairs carved from the rock that lead down to the water. [1]
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.
Valladolid (Spanish: [baʝaðoˈlið] ⓘ; Sakiʼ in Maya) is a city located in the eastern region of the Mexican state of Yucatán. It is the seat of Valladolid Municipality . As of the 2020 census the population of the city was 56,494 inhabitants (the third-largest community in the state after Kanasín ), and that of the municipality was 85,460.
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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.
The cenotes are water-filled sinkholes formed by water percolating through the soft limestone soil for thousands of years. Eighteen deep cenotes and more than 250 shallow bodies exist on the island. Many are under dense vegetation. [10] Jade Cavern Cozumel (Cenote Chempita) near El Cedral is often visited by tourists. [11]
The most jade found at a single site was at the Cenote of Sacrifice at Chichen Itza. Metal was a common offering during the Postclassic, with the largest collections coming from the Cenote of Sacrifice and "bell" caves in western Honduras. The tale of the Earth Lord having much wealth in his cave may have come from this tradition. [35]
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]