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
63 measurements from 1950-09-15 to 1973-01-12. Most recent water-level elevation 3556.21 ft, 45.3 ft below ground.
Over the record the level is increasing at 0.92 ft per decade (p = 0.0041, n = 63). 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, 1950-09-15 to 1973-01-12, 63 measurements. The record is increasing at 0.92 feet per decade (p equals 0.0041), 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 | 200.0 ft |
| Ground elevation | 3601.51 ft |
| Location | 40.54000, -102.12000 |
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.