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sinkhole
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The wells at Chichén Itzá are actually large limestone sinkholes - known in Spanish as cenotes (underground pools) - and they are one of the singular aspects of the site.
The enclosed depressions are complex forms of dolines or sinkholes , which act as centripetal drainage basins.
This is the process by which rainwater erodes limestone cliffs and creates limestone caves and sinkholes .
The trip passes by waterfalls, forests, canyons, valleys, sinkholes and caves.
Karst is an area of irregular limestone in which erosion has produced fissures, sinkholes , underground streams, and caverns.
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