v4.2 had solved a problem no one had asked yet.
A 3D tomographic image materialized—not a model, but a wireframe reconstruction based on the pressure transients themselves. The software had reverse-engineered the geology from the water’s behavior. A vertical fault line, invisible to seismic surveys, plunged from the basin floor down to 2,300 meters. And at the bottom, a second aquifer. Ancient. Pressurized. Geothermal.
Some stories don’t end. They just percolate deeper.
v4.2 popped up a dialog box: "Detected secondary recharge boundary. Type: Deep crustal fracture. Estimated inflow rate: 18.7 L/s. Confidence: 97.3%. Display path?"
