Hydrohistorian
Alluvial
Stream-connected valley fill; recharges and can be depleted by nearby pumping.
Water-level record
33 measurements from 1962-04-16 to 2013-03-25. Most recent water-level elevation 3998.4 ft, 8.5 ft below ground.
Over the record the level is no trend at -0.03 ft per decade (p = 0.4754, n = 33). 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, 1962-04-16 to 2013-03-25, 33 measurements. The record is no trend at -0.03 feet per decade (p equals 0.4754), 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 | 90.0 ft |
| Ground elevation | 4006.9 ft |
| Location | 40.52000, -103.30000 |
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.