Aquifers host 30% of global freshwaters (Shiklomanov, 1993), and play an important role in addressing water needs worldwide, especially in countries with extensive arid regions (United Nations, 2022). In Mexico, 39.5% of the consumed water is supplied through ∼35,300 hm 3 /year groundwater, extracted from ∼300,000 wells and used for agriculture (71%), public supply (21%), industry and electric energy (excluding hydroelectric) (8%) (CONAGUA, 2022b). Although Mexico is not considered "water-poor", large discrepancies in recharge and consumption rates and patterns exist: only 20% of the total annual rainfall occurs where 76% population lives and 90% irrigated lands are maintained (Hernandez, 2003). In 2020, the National Waters Commission (CONAGUA) identified 157 overexploited aquifers near densely populated cities and large farmlands, and 48 threatened by salinization and/or marine intrusion (CONAGUA, 2022b). Land subsidence resulting from groundwater overexploitation has also been documented in major cities of Central Mexico (Cabral-Cano et al., 2008;Carreon-Freyre et al., 2011). Topographic lowering, tilting and deformation, apparent uplifting of deeply founded structures, surface cracking and faulting are very common impacts that aquifer-system compaction causes on Mexican urban landscapes (Carreón Freyre, 2010;Figueroa-Miranda et al., 2018), and in many other countries (Galloway &