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
32 measurements from 1975-09-16 to 2014-09-30.
Over the record the level is no trend at 16.13 ft per decade (p = 0.2304, 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, 1975-09-16 to 2014-09-30, 32 measurements. The record is no trend at 16.13 feet per decade (p equals 0.2304), 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 | 853.0 ft |
| Ground elevation | 6812.6 ft |
| Location | 39.86000, -108.21000 |
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.