Hydrohistorian
WS-36
Monitored well · 46 · Division 5 · Water District 45
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
22 measurements from 2000-09-28 to 2025-08-15. Most recent water-level elevation 6101.59 ft, 21.41 ft below ground.
Over the record the level is no trend at -1.92 ft per decade (p = 0.0907, n = 22). 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, 2000-09-28 to 2025-08-15, 22 measurements. The record is no trend at -1.92 feet per decade (p equals 0.0907), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Aquifer | WASATCH |
|---|---|
| Designated basin | WEST SLOPE |
| Total depth | 277.0 ft |
| Perforated interval | 235.0–275.0 ft |
| Ground elevation | 6123.0 ft |
| Permit | 213138 |
| Location | 39.46000, -107.65000 |
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.