A tinaja[tiˈnaxa], sometimes tenaja, is a surface pocket (depression) formed in bedrock that occurs below waterfalls, that is carved out by spring flow or seepage,[1] or that is caused by sand and gravel scouring in intermittent streams (arroyos).[2][3] The term usually implies a natural or geologiccistern in rock which retains water. They are often created by erosional processes within intermittent streams.
Tinajas are an important source of surface water storage in arid environments.[2][4]
These relatively rare landforms are important ecologically, because they support unique plant communities and provide important services to terrestrial wildlife.[5]
↑ Osterkamp, W. R. 2008. Annotated Definitions of Selected Geomorphic Terms and Related Terms of Hydrology, Sedimentology, Soil Science and Ecology: Reston, Virginia, Open File Report 2008-1217, pp 49
1 2 Fox, William (2005). Desert Water. Portland, Oregon: Graphic Arts Center Publishing Company. p.12. ISBN978-1-55868-858-2.
↑ Mabbutt, J. A. (1977). Desert Landforms. Canberra: Australian National University Press. p.182. ISBN978-0-7081-0437-8.
↑ Brown, T. B. and R. R. Johnson. 1983. The distribution of bedrock depressions (tinajas) as sources of surface water in Organ Pipe Cactus National Monument, Arizona. Journal of the Arizona-Nevada Academy of Science 18: 61-68.
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