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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.
A coral skeleton from the Mesoamerican Barrier Reef System, Quintana Roo, Mexico The Mesoamerican Barrier Reef System (MBRS), also popularly known as the Great Mayan Reef or Great Maya Reef, is a marine region that stretches over 1,126 kilometres (700 mi) along the coasts of four countries – Mexico, Belize, Guatemala, and Honduras – from Isla Contoy at the northern tip of the Yucatán ...
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