Skip to main content
Log in

Maya utilization of karst groundwater resources

  • Published:
Environmental Geology and Water Sciences

Abstract

Much of the Maya civilization in pre-Columbian Meso-America was established on karst terrain that included parts of what are now Belize, Guatemala, northern Honduras and southern Mexico. By definition, little surface water exists in karst, so for the Maya to flourish on that terrain they had to effectively and efficiently utilize all their water resources. Access to groundwater was by means of springs and caves. Maya life, urban and rural, lay and elite, religious and secular was often a function of groundwater exploitation and surface water development. The Maya's use of groundwater was predominantly to supplement enhanced surface water supplies and was used more often in semiarid zones than in humid zones. The pattern of Maya settlements, especially in the semiarid zones, occurred in areas with greater access to the groundwater. Maya groundwater retrieval methods were primitive, inefficient, labor intensive, and uninnovative, as compared to their other technologic achievements. Groundwater contamination, from human effluent, could have resulted in widespread disease and contributed to the Maya's downfall.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Similar content being viewed by others

References Cited

  • Adams, R. E. W., 1980, Swamps, canals, and the locations of ancient Maya cities. Antiquity, v. 54, p. 206–214.

    Google Scholar 

  • Andrews, E. W., IV, 1965, Exploration in the Gruta de Chac, Yucatan, Mexico: Middle American Research Institute, Tulane University, Publication 31.

    Google Scholar 

  • Andrews, E. W., IV, 1970, Balankanche, throne of the Tiger Priest: Middle American Research Institute, Tulane University, Publication 32.

  • Andrews, E. W., IV, and A. P. Andrews, 1975, A preliminary study of the ruins of Xcaret, Quintana Roo, Mexico: Middle American Research Institute, Tulane University, Publication 40.

    Google Scholar 

  • Doehring, D. O., and J. H. Butler, 1974, Hydrogeologic constraints on Yucatan's development: Science, v. 186, no. 4164, p. 591–595.

    Google Scholar 

  • Macleod, B., and D. E. Puleston, 1978, Pathways into darkness: the search for the road to Xibalba: Third Palanque Rountable, Pre-Columbian Art Research Center, p. 71–77.

  • Mathewson, K., 1977, Maya urban genesis reconsidered: trade and intensive agriculture as primary factors: Journal of Historical Geography, v. 3, p. 203–215.

    Google Scholar 

  • Stephens, J. L., 1843, Incidents of travel in Yucatan, 2 vol.

  • Stone, A., 1987, The painted walls of Xibalba: Maya cave painting as evidence of cave ritual,in W. Hanks and D. Rice, eds., The cultural context of Mayan glyphs, language, history, and representation (in press).

  • Thompson, J. E. S., 1970, Maya history and religion: University of Oklahoma Press.

  • Wilhelmy, H., 1981, Welt und umwelt der Maya: aufstieg und untergang einer hochkultur: Zurich, R. Piper and Company.

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Veni, G. Maya utilization of karst groundwater resources. Environ. Geol. Water Sci 16, 63–66 (1990). https://doi.org/10.1007/BF01702224

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF01702224

Keywords

Navigation