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
33 measurements from 1957-03-27 to 2003-01-28. Most recent water-level elevation 3710.06 ft, 129.5 ft below ground.
Over the record the level is decreasing at -1.12 ft per decade (p = 0.0031, n = 32). 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, 1957-03-27 to 2003-01-28, 33 measurements. The record is decreasing at -1.12 feet per decade (p equals 0.0031), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Designated basin | NORTHERN HIGH PLAINS |
|---|---|
| Total depth | 136.0 ft |
| Ground elevation | 3839.56 ft |
| Permit | 13728 |
| Location | 38.24000, -102.21000 |
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.