Hydrohistorian
WS-23A
Monitored well · 41 · 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
36 measurements from 1975-04-17 to 2024-08-02. Most recent water-level elevation 6559.2 ft, 19.2 ft below ground.
Over the record the level is decreasing at -1.31 ft per decade (p = 0.0, n = 36). 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, 1975-04-17 to 2024-08-02, 36 measurements. The record is decreasing at -1.31 feet per decade (p equals 0.0), 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 | 744.0 ft |
| Ground elevation | 6578.4 ft |
| Permit | 95837 |
| Location | 39.80000, -108.36000 |
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.