Hydrohistorian
WS-10A
Monitored well · 30 · Division 6 · Water District 43
Other bedrock
Bedrock aquifer; no assumed human-timescale recharge without local evidence.
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
53 measurements from 1975-09-01 to 2024-08-02. Most recent water-level elevation 6309.42 ft, 415.18 ft below ground.
Over the record the level is increasing at 1.68 ft per decade (p = 0.0004, n = 53). 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, 1975-09-01 to 2024-08-02, 53 measurements. The record is increasing at 1.68 feet per decade (p equals 0.0004), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Aquifer | UINTA |
|---|---|
| Designated basin | WEST SLOPE |
| Total depth | 1185.0 ft |
| Ground elevation | 6724.6 ft |
| Location | 39.91000, -108.38000 |
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.