Hydrohistorian
San Luis Valley (confined)
Confined aquifer beneath the valley; distinct from the shallow unconfined system.
Because this aquifer does not recharge on a human timescale, a decline here is storage being removed, not a stream being short. It is kept out of the stream-depletion math for that reason.
Water-level record
No water-level measurements are cached for this well. It is in the well inventory — permit, construction and aquifer below — but nobody has logged a level we hold.
The well itself
| Aquifer | CONFINED SAN LUIS VALLEY |
|---|---|
| Total depth | 358.0 ft |
| Perforated interval | 158.0–358.0 ft |
| Ground elevation | 7660.0 ft |
| Reported yield | 0.0 gpm |
| Permit | 185914 |
| Location | 38.02000, -106.07000 |
What this page is not
Monitoring records are irregular: measurements cluster where somebody chose to look, so a trend describes this well's record, not the aquifer as a whole. Levels are DWR's published measurements, unedited. A trend here is not a prediction, and it is not a determination about anyone's water right.