Hydrohistorian
DB-095 GEDDI, SAM
Monitored well · 232 · Division 2 · Water District 10
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
44 measurements from 1968-12-01 to 2026-02-06. Most recent water-level elevation 6921.71 ft, 173.29 ft below ground.
Over the record the level is no trend at -1.95 ft per decade (p = 0.0613, n = 44). 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, 1968-12-01 to 2026-02-06, 44 measurements. The record is no trend at -1.95 feet per decade (p equals 0.0613), 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 | 245.0 ft |
| Perforated interval | 180.0–245.0 ft |
| Ground elevation | 7095.0 ft |
| Permit | 36034 |
| Location | 39.01000, -104.75000 |
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.