Hydrohistorian
Alluvial
Stream-connected valley fill; recharges and can be depleted by nearby pumping.
Water-level record
35 measurements from 1948-01-23 to 2013-03-25. Most recent water-level elevation 3533.21 ft, 18.3 ft below ground.
Over the record the level is no trend at -0.02 ft per decade (p = 0.9773, n = 35). 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, 1948-01-23 to 2013-03-25, 35 measurements. The record is no trend at -0.02 feet per decade (p equals 0.9773), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Aquifer | QUATERNARY ALLUVIUM |
|---|---|
| Designated basin | CSU SUPPLEMENTAL NETWORK |
| Total depth | 52.0 ft |
| Ground elevation | 3551.51 ft |
| Location | 40.98000, -102.40000 |
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.