Hydrohistorian
SHP-36 JESSER,HARVEY
Monitored well · 1157 · 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
36 measurements from 1991-04-02 to 2026-02-25. Most recent water-level elevation 4634.63 ft, 145.37 ft below ground.
Over the record the level is no trend at 0.14 ft per decade (p = 0.2351, n = 36). 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, 1991-04-02 to 2026-02-25, 36 measurements. The record is no trend at 0.14 feet per decade (p equals 0.2351), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Aquifer | CHEYENNE |
|---|---|
| Designated basin | SOUTHERN HIGH PLAINS |
| Total depth | 350.0 ft |
| Ground elevation | 4780.0 ft |
| Permit | 16299 |
| Location | 37.45000, -102.89000 |
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.