Hydrohistorian
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
31 measurements from 1991-10-07 to 2025-08-15. Most recent water-level elevation 6100.06 ft, 36.04 ft below ground.
Over the record the level is no trend at -2.42 ft per decade (p = 0.1534, n = 31). 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, 1991-10-07 to 2025-08-15, 31 measurements. The record is no trend at -2.42 feet per decade (p equals 0.1534), 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 | 134.0 ft |
| Ground elevation | 6136.1 ft |
| Location | 39.45000, -107.98000 |
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.