Hydrohistorian
SHP-15 MOORE
Monitored well · 1130 · Division 2 · Water District 67
Other bedrock
Bedrock aquifer; no assumed human-timescale recharge without local evidence.
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
34 measurements from 1961-09-22 to 2026-02-25. Most recent water-level elevation 4475.07 ft, 134.93 ft below ground.
Over the record the level is no trend at -0.1 ft per decade (p = 0.6611, n = 34). 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, 1961-09-22 to 2026-02-25, 34 measurements. The record is no trend at -0.1 feet per decade (p equals 0.6611), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Aquifer | DAKOTA |
|---|---|
| Designated basin | SOUTHERN HIGH PLAINS |
| Total depth | 316.0 ft |
| Ground elevation | 4610.0 ft |
| Permit | 9835 |
| Location | 37.56000, -102.77000 |
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.