Hydrohistorian
High Plains / Ogallala
Effectively non-recharging in eastern Colorado; declines are storage depletion, a separate ledger line.
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
19 measurements from 1992-12-26 to 2010-01-25.
Over the record the level is no trend at 3.68 ft per decade (p = 0.4429, n = 17). 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, 1992-12-26 to 2010-01-25, 19 measurements. The record is no trend at 3.68 feet per decade (p equals 0.4429), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Aquifer | OGALLALA |
|---|---|
| Designated basin | NORTHERN HIGH PLAINS |
| Total depth | 330.0 ft |
| Perforated interval | 290.0–330.0 ft |
| Ground elevation | 4454.0 ft |
| Reported yield | 20.0 gpm |
| Permit | 38380 |
| Location | 40.08000, -102.96000 |
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.