Articles | Volume 372
Proc. IAHS, 372, 285–290, 2015
https://doi.org/10.5194/piahs-372-285-2015
Proc. IAHS, 372, 285–290, 2015
https://doi.org/10.5194/piahs-372-285-2015

  12 Nov 2015

12 Nov 2015

Physical experiments of land subsidence within a maar crater: insights for porosity variations and fracture localization

M. Cerca et al.

Related authors

Analogue model of ground ruptures due to groundwater pumping in an aquifer above a bedrock ridge
Mariano Cerca, Dora Carreón-Freyre, and Pietro Teatini
Proc. IAHS, 382, 433–436, https://doi.org/10.5194/piahs-382-433-2020,https://doi.org/10.5194/piahs-382-433-2020, 2020
Short summary
Factors that condition physical vulnerability to ground fracturing in Mexico City
Dora Carreon-Freyre, Raul I. Gutierrez-Calderon, Mariano Cerca, and Carlos F. Alcantara-Duran
Proc. IAHS, 382, 571–576, https://doi.org/10.5194/piahs-382-571-2020,https://doi.org/10.5194/piahs-382-571-2020, 2020
Short summary
Mass movement processes triggered by land subsidence in Iztapalapa, the eastern part of Mexico City
M. González-Hernández, D. Carreón-Freyre, R. Gutierrez-Calderon, M. Cerca, and W. Flores-Garcia
Proc. IAHS, 372, 261–265, https://doi.org/10.5194/piahs-372-261-2015,https://doi.org/10.5194/piahs-372-261-2015, 2015
Analysis of the variation of the compressibility index (Cc) of volcanic clays and its application to estimate subsidence in lacustrine areas
D. Carreón-Freyre, M. González-Hernández, D. Martinez-Alfaro, S. Solís-Valdéz, M. Cerca, B. Millán-Malo, R. Gutiérrez-Calderón, and F. Centeno-Salas
Proc. IAHS, 372, 273–279, https://doi.org/10.5194/piahs-372-273-2015,https://doi.org/10.5194/piahs-372-273-2015, 2015
Short summary

Cited articles

Aranda-Gómez, J. J. and Carrasco-Nuñez, G.: The Valle de Santiago maars, México: the record of magma-water fluctuations during the formation of a basaltic maar (La Alberca) and active post-desiccation subsidence at the bottom of a maar lake (Rincón de Parangueo): Intra-conference field trip guidebook, 5th International Maar Conference, 17–22 November, Centro de Geociencias, Universidad Nacional Autónoma de México, Querétaro, México, 30 pp., 2014.
Aranda-Gómez, J. J., Levresse, G., Pacheco-Martínez, J., Ramos-Leal, J. A., Carrasco-Núñez, G., Chacón-Baca, E., González-Naranjo, G., Chávez-Cabello, G., Vega-González, M., Origel-Gutiérrez, G., and Noyola-Medrano, C.: Active subsidence at the bottom of a recently desiccated crater-lake and its environmental impact: Rincón de Parangueo, Guanajuato, México: Field trip guidebook, Eighth International Symposium on Land Subsidence, Universidad Nacional Autónoma de México, Centro de Geociencias, Querétaro, Qro., México, 1–48, 2010.
Aranda-Gómez, J. J., Levresse, G., Pacheco-Martínez, J., Ramos-Leal, J. A., Carrasco-Nuñez, G., Chacón-Baca, E., González-Naranjo, G. A., Chávez-Cabello, G., Vega-González, M., Origel, G., and Noyola-Medrano, C.: Active sinking at the bottom of the Rincón de Parangueo Maar (Guanajuato, México) and its probable relation with subsidence faults at Salamanca and Celaya, Boletín de la Sociedad Geológica Mexicana, 65, 169–188, 2013.
Barrientos, B., Cerca, M., García-Márquez, J., and Hernández-Bernal, C.: Three-dimensional displacement fields measured in a deforming granular-media surface by conbined frige projection and speckle photography, J. Opt. A-Pure Appl. Op., 10, 10 pp., 2008.
Cerca, M., Carreón-Freyre, D., Aranda-Gómez, J. J., and Rocha-Treviño, L.: GPR profiles for characterizing subsidence deformation in lake sediments within a mar crater, 15th International Conference on Ground Penetrating Radar GPR2014, Brussels, Belgium, 30 June–4 July, 4 pp., 2014.
Download
Short summary
We present a series of physical experiments that examine with detail the evolution of subsidence in a volcanic maar crater, located in central Mexico. The crater is thought to be connected to the adjacent aquifer, which has been extensively exploited during the last 35 years. Subsidence in the sediments filling the crater show deformation manifested as ring faults and fractures. The results may be relevant to understand the evolution of subsidence in similar volcanic settings elsewhere.