Hydrohistorian
SHP-24 CHENOWETH,W.V.
Monitored well · 1146 · 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
38 measurements from 1983-07-01 to 2026-02-26. Most recent water-level elevation 4315.44 ft, 64.56 ft below ground.
Over the record the level is no trend at 0.16 ft per decade (p = 0.6147, n = 37). 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, 1983-07-01 to 2026-02-26, 38 measurements. The record is no trend at 0.16 feet per decade (p equals 0.6147), 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 | 100.0 ft |
| Perforated interval | 70.0–100.0 ft |
| Ground elevation | 4380.0 ft |
| Permit | 62402 |
| Location | 37.54000, -102.64000 |
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.