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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.
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.
It is an extensive water filled cave system connected with the Caribbean Sea, fed via a coastal spring in a cenote with a variety of names, including Cenote Manati, Cenote Tankah, and Casa Cenote after a nearby restaurant. The explored cave system extends to approximately 8 kilometers (5.0 mi) inland from the coast.
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]
Camino Real, or the Royal Inland Route, was a trade route for silver extracted from the mines in Mexico and mercury imported from Europe. It was active from the mid-16th to the 19th centuries and stretched over 2,600 km (1,600 mi) from north of Mexico City to Santa Fe in today's New Mexico. This serial site comprises the Mexican part of the ...
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