Hydrohistorian
WS-19
Monitored well · 28 · 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
27 measurements from 1972-07-27 to 2009-09-29.
Over the record the level is no trend at -1.62 ft per decade (p = 0.403, n = 26). 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, 1972-07-27 to 2009-09-29, 27 measurements. The record is no trend at -1.62 feet per decade (p equals 0.403), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Aquifer | GREEN RIVER |
|---|---|
| Designated basin | WEST SLOPE |
| Total depth | 1648.0 ft |
| Perforated interval | 1008.0–1648.0 ft |
| Ground elevation | 6622.15 ft |
| Permit | 13449 |
| Location | 39.85000, -108.28000 |
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.