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Geological Formation

Gran Cenote

Cenotes

Gran Cenote lies along the road between Tulum and Coba on Mexico's Yucatan Peninsula, a karst sinkhole formed by the collapse of limestone bedrock into an underlying flooded cave network. Its clear turquoise water and partially open, partially cavernous structure expose extensive stalactite and stalagmite formations along its submerged and semi-submerged chambers, evidence that the caves were once dry before rising sea levels and groundwater flooded them. Gran Cenote connects underground to the wider Sistema Sac Actun cave system, one of the largest surveyed underwater cave networks on the peninsula, and is a popular site for snorkeling and cave diving. This entity documents Gran Cenote specifically as a geological formation, a karst sinkhole near Tulum whose flooded chambers connect into the Sac Actun cave system.

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Source Wikipedia: Cenote
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Source GeoNames: GeoNames search results for Gran CenoteSearch result row
Quote, Search result row
20.24656 -87.46409 Mexico, Quintana Roo
Sources
GeoNames: GeoNames search results for Gran Cenote
GeoNamesIn Group: Named Cenotes, Search results
Quote, In Group: Named Cenotes, Search results
Gran cenote 20.24656 -87.46409 Mexico , Quintana Roo Tulum pond
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Wikipedia: Cenote
WikipediaCaused By: Karstification, Lead sentence
Quote, Caused By: Karstification, Lead sentence
is a natural pit, or sinkhole, resulting when a collapse of limestone bedrock exposes groundwater.
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