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A cenote (English: / s ɪ ˈ n oʊ t i / or / s ɛ ˈ n oʊ t eɪ /; Latin American Spanish:) is a natural pit, or sinkhole, resulting when a collapse of limestone bedrock exposes groundwater. The term originated on the Yucatán Peninsula of Mexico, where the ancient Maya commonly used cenotes for water supplies, and occasionally for ...
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.
Geographical features include cenotes (sinkholes) and petenes, tree islands emerging from the swamps. [7] Pre-Hispanic City and National Park of Palenque: Chiapas: 1987 411; i, ii, iii, iv (cultural) Palenque was a Maya city, founded around the 1st century CE during the late Preclassic period.
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 main camp of exploration became Cenote "Far Point Station", located 6 kilometers (3.7 mi) from the coast, and 2.8 kilometers (1.7 mi) further inland than Main Base Camp situated at the main Nohoch Nah Chich Cenote entrance. During the Nohoch 1997 expedition, the 60 kilometers (37 mi) of total explored cave passage mark was surpassed.
The Maya block is one of a group of crustal blocks found at the edge of the Gondwana continent. Zircon ages are consistent with the presence of an underlying Grenville age crust, with large amounts of late Ediacaran arc -related igneous rocks , interpreted to have formed in the Pan-African orogeny .
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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] As the sea level was over 100 m (328 ft) lower than it is today, the cave system was dry during the Late Pleistocene. [3]
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