Located in the Valley of Mexico at 2,200 metres above sea level, the basin of Mexico City has no natural drainage outlet for water. As such, floods, droughts, and other water-related dynamics have always been part of the region. When the Aztecs founded their capital city Tenochtitlan here in 1325, they engineered an impressive system of water infrastructures, including dikes, locks, aqueducts, and chinampas: small, rectangular islands filled with fertile dredged soil to grow crops. This half-natural, half-artificial landscape was at once productive, environmentally sensitive, and spatially distinctive. It both provided protection against floods and allowed for the irrigation and lacustrine transport of agricultural crops. Even up until the 20th century, the region hosted several shallow lakes that fluctuated between one to three metres during the wet and dry seasons,…