Mexico City has sunk more than 10 meters (33 feet) since 1920, with current rates of 1–2 meters (3.3–6.6 ft) per year in the worst zones. Cause: aquifer over-extraction beneath the former Lake Texcoco. The lacustrine clay compresses irreversibly as water is pumped out. Consequences:
Mitigation: wastewater recharge, rainwater harvesting, reducing demand, but subsidence is largely permanent.