Cenote Bolonchoojol is a karst sinkhole near the village of Cuzama in Yucatan, Mexico, reached through a hole in the ground fitted with a ladder built by welding together old railroad ties, opening into a chamber of crystal-clear water lined with large stalactites and stalagmites. This entity documents Cenote Bolonchoojol specifically as a geological formation, a Cuzama-area cenote reached by a repurposed railroad-tie ladder into a stalactite-lined chamber.
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Wikipedia: Cenote
WikipediaCaused By: Karstification, Lead sentenceQuote, Caused By: Karstification, Lead sentence
is a natural pit, or sinkhole, resulting when a collapse of limestone bedrock exposes groundwater.
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