Coordinates: 22°59′36.05″N 98°9′57.1″W / 22.9933472°N 98.165861°W / 22.9933472; -98.165861
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El Zacatón with free floating grass island (lower right), Municipality of Aldama, Tamaulipas, Mexico

Zacatón is a thermal water-filled sinkhole belonging to the Zacatón system - a group of unusual karst features located in Aldama Municipality near the Sierra de Tamaulipas in the northeastern state of Tamaulipas, Mexico. At a total depth of 339 meters (1,112 ft), it is one of the deepest known water-filled sinkholes in the world.[1]

Using an autonomous robot, the underwater portion of Zacatón has been measured to be 319 meters (1,047 ft) deep (a 20-meter (66 ft) difference between the rim of cliff and surface of water adds to the total depth).[2] Zacatón is the only sinkhole of the five located in Rancho La Azufrosa to have any noticeable water flow.[3]

The name Zacatón comes from the free-floating islands of zacate grass which move around on the surface with the wind.[4]

Scrapings from the rock walls beneath the surface yielded at least three new phyla of bacteria.[5]


Zacaton sinkhole, cross-section

El Zacatón's depth has made it an important dive site:


Zacatón is just one of the numerous sinkholes and other karst features in the region. Here are located more than 15 sinkholes, several cave systems and karst springs with caves. Several of these karst features have unusual characteristics like travertine lids over several of the sinkholes with isolated waterbodies below.

Since the late 1990s, Dr. Marcus Gary, a hydrogeologist at the Edwards Aquifer Authority and adjunct professor at the Jackson School of Geosciences, University of Texas at Austin has studied Sistema Zacatón to understand how the sinkholes formed and how they evolve over time.[14] During these studies, Gary made extensive use of a number of investigative tools, including those on the DEPTHX probe, geophysics, isotope geochemistry, field mapping, and geomicrobiology. Gary was a primary member and a principal investigator on the DEPTHX mission, which used an autonomous underwater robot to explore the deepest parts of Zacatón for the first time.

According to Gary, these sinkholes began to form during the Pleistocene as a result of volcanic activity from below.[15] This view differs from the classical theory of cave formation and also hypotheses about the formation of other large caves in this part of Mexico. In this view, volcanism turned deep water slightly acidic by adding dissolved carbon dioxide and hydrogen sulfide. This water slowly dissolved the limestone above, creating porous karst.[3] This is referred to as “hypogenic karstification.” From time to time, overlying rock collapsed into hollow chambers below, creating deep shafts. If his interpretation is correct, Sistema Zacatón has more in common with Mammoth Hot Springs in Yellowstone than with other deep sinkholes in this same region of Mexico.

Another interesting hydrogeologic feature is that some of the sinkholes appear to be in the process of closing up at the top as crusts of travertine (a form of calcium carbonate) form at their surfaces. Marc Airhart, a science writer at the Jackson School of Geosciences wrote:

It’s a bit like the skin on a can of paint that has been left open in the sun. For the paint, it might take a day or two. In this case, the process probably takes thousands of years. It is basically the sinkhole’s way of taking a bunch of dissolved rock floating in the water and recycling it to form new rock at the surface. At least one sinkhole (Poza Seca) appears to have closed up entirely, sealing off an underwater lake, possibly with unusual life forms. If such life forms exist, they’re likely to be bacteria that can live without oxygen and sunlight. And assuming the lake has been sealed off from the outside world for thousands and thousands of years, they might have evolved to be different from anything scientists have ever discovered and characterized before.[16]

See also[edit]


  1. ^ Gary, Marcus; Fairfield, Nathaniel; Stone, William C.; Wettergreen, David; Kantor, George; Sharp, Jr, John M. (2008). "3D Mapping and Characterization of Sistema Zacatón from DEPTHX (DEepPhreaticTHermal e Xplorer)". Sinkholes and the Engineering and Environmental Impacts of Karst. pp. 202–212. doi:10.1061/41003(327)20. ISBN 978-0-7844-1003-5. Retrieved 2011-01-07.
  2. ^ "Demystifying El Zacatón". Astrobiology Magazine. 2002-12-18. Archived from the original on 2007-06-09. Retrieved 2012-05-02.{{cite web}}: CS1 maint: unfit URL (link)
  3. ^ a b Gary, Marcus (2000). "Speleogenesis of Zacatón and cenotes of Rancho la Azufrosa". In Hallock; French (eds.). Proceedings of the 20th Annual Scientific Diving Symposium. American Academy of Underwater Sciences. Retrieved 2011-01-07.
  4. ^ "The Unusual Cenotes". Retrieved 2012-05-02.
  5. ^ Moskowitz, Clara. "Deep-diving robot finds microbial zoo in sinkhole". Retrieved 22 August 2013.
  6. ^ "Proyecto de Buceo Espeleologico México y América Central Bio: Ann Kristovich". Retrieved 2012-05-02.
  7. ^ Zacaton. A History by Dr. by Ann Kristovich
  8. ^ "A/C N10 Incident Reports". 1994-04-06. Retrieved 2012-05-02.
  9. ^ "Eulogy for an Explorer". Retrieved 2012-05-02.
  10. ^ Vlahos, James. "Robotic Mission to Zacaton". Retrieved 2012-05-02.
  11. ^ Connolly, Ceci (2007-05-14). "Mexican Sinkhole May Lead NASA to Jupiter". Retrieved 2012-05-02.
  12. ^ "The Advance DEPTHX Team Missions". Retrieved 2012-05-02.
  13. ^ "Robotic submarine reaches new depths". Retrieved 2012-05-02.
  14. ^ Sistema Zacatón
  15. ^ Volcanic karstification of Sistema Zacaton, Mexico (Gary, Sharp, 2006)
  16. ^ Airhart, Marc (2007-05-19). "Put a Lid On It". Retrieved 2011-01-07.

Further reading[edit]

  • Sistema Zacatón
  • Sistema Zacatón by Wondermondo. Separate descriptions of 17 features in system.
  • [1]. Karst hydrogeology and speleogenesis of sistema Zacatón by Marcus o. Gary. Bulletin of Association for mexican cave studies (AMCS) n°21-2010.

External links[edit]

22°59′36.05″N 98°9′57.1″W / 22.9933472°N 98.165861°W / 22.9933472; -98.165861