Hydrohistorian
PINERY "G"
Monitored well · 110 · Division 1 · Water District 8
Its well permit here · Well permit at DWR ↗ · DWR structure record ↗ · Its structure dossier here · Download levels (CSV)
Denver Basin bedrock
Confined sandstone aquifer; negligible human-timescale recharge — pumping is one-way storage mining.
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
52 measurements from 1974-09-06 to 2017-04-25.
Over the record the level is decreasing at -31.08 ft per decade (p = 0.0033, n = 49). Mann–Kendall with the Hamed–Rao autocorrelation correction, on water-level elevation; rising elevation means more water.
Chart: water level at this well over time, 1974-09-06 to 2017-04-25, 52 measurements. The record is decreasing at -31.08 feet per decade (p equals 0.0033), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Aquifer | DAWSON |
|---|---|
| Designated basin | DENVER BASIN |
| Total depth | 936.0 ft |
| Perforated interval | 560.0–896.0 ft |
| Ground elevation | 6245.0 ft |
| Permit | 17931 |
| Location | 39.43000, -104.73000 |
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.