Hydrohistorian
SHP-30 HUME, CHARLES
Monitored well · 1152 · 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
35 measurements from 1938-02-21 to 2026-02-25. Most recent water-level elevation 3693.88 ft, 229.12 ft below ground.
Over the record the level is decreasing at -29.25 ft per decade (p = 0.0001, n = 27). 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, 1938-02-21 to 2026-02-25, 35 measurements. The record is decreasing at -29.25 feet per decade (p equals 0.0001), 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 / CHEYENNE |
|---|---|
| Designated basin | SOUTHERN HIGH PLAINS |
| Total depth | 631.0 ft |
| Perforated interval | 200.0–300.0 ft |
| Ground elevation | 3923.0 ft |
| Permit | 2503 |
| Location | 37.46000, -102.27000 |
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.