Hydrohistorian
Alluvial
Stream-connected valley fill; recharges and can be depleted by nearby pumping.
Water-level record
110 measurements from 1986-03-07 to 2004-07-30. Most recent water-level elevation 5130.3 ft, 7.36 ft below ground.
Over the record the level is no trend at -1.04 ft per decade (p = 0.3473, n = 110). 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, 1986-03-07 to 2004-07-30, 110 measurements. The record is no trend at -1.04 feet per decade (p equals 0.3473), 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 |
|---|---|
| Perforated interval | 7.0–28.0 ft |
| Ground elevation | 5137.66 ft |
| Location | 39.87000, -104.84000 |
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.