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
22 measurements from 1963-05-01 to 2011-10-04.
Over the record the level is no trend at -9.49 ft per decade (p = 0.0532, n = 21). 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, 1963-05-01 to 2011-10-04, 22 measurements. The record is no trend at -9.49 feet per decade (p equals 0.0532), 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 | 294.0 ft |
| Ground elevation | 6083.8 ft |
| Permit | 15795 |
| Location | 39.46000, -107.64000 |
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.