Hydrohistorian
Alluvial
Stream-connected valley fill; recharges and can be depleted by nearby pumping.
Water-level record
12 measurements from 1967-10-27 to 2010-04-13. Most recent water-level elevation 3977.57 ft, 34.2 ft below ground.
Over the record the level is no trend at -0.18 ft per decade (p = 0.4507, n = 12). 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, 1967-10-27 to 2010-04-13, 12 measurements. The record is no trend at -0.18 feet per decade (p equals 0.4507), 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 | 102.0 ft |
| Ground elevation | 4011.77 ft |
| Location | 40.65000, -103.24000 |
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.