4 ms·
Location of maximum land subsidence in U.S. Levels at 1925 and 1977
- krunck 8mo ago"Accompanying this release of water is a largely nonrecoverable reduction in the pore volume of the compacted aquitards, and thus a reduction in the total storage capacity of the aquifer system. " We can continue to draw from the aquifer at rates higher than the recharge rate but after that the valley will be done as an agricultural area.