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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.
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.
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.
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.
Archway of the Temple of the 7 Doll Ruins of the colonial open chapel Cenote at Dzibilchaltun. Dzibilchaltún (Yucatec: Ts'íibil Cháaltun, [d̥z̥ʼiː˧˥biɭ tɕʰɒːl˦˥tuŋ]) is a Maya archaeological site in the Mexican state of Yucatán, approximately 10 miles (16 km) north of state capital of Mérida.
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] It is larger and more open than most other ...
The ring structures are best developed to the south, west and northwest, becoming more indistinct towards the north and northeast of the structure. This is interpreted to be a result of variable water depth at the time of impact, with less well-defined rings resulting from the areas with water depths significantly deeper than 100 meters (330 ft).
Like most bodies of water in the Yucatán peninsula, the lake is fed by underground rivers, whose regular open pools are cenotes. Because of the porous limestone, the Yucatán Peninsula has almost no lakes, this is by far the largest, and fed by the 450 km underground river that is part of the worlds's largest water cave/tunnel system ...