Hydrohistorian
SHP-01 BLAKE, JERREL
Monitored well · 1125 · 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
23 measurements from 1993-03-11 to 2017-03-02.
Over the record the level is decreasing at -17.74 ft per decade (p = 0.0116, n = 19). 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, 1993-03-11 to 2017-03-02, 23 measurements. The record is decreasing at -17.74 feet per decade (p equals 0.0116), 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 | 600.0 ft |
| Ground elevation | 3659.0 ft |
| Permit | 10437 |
| Location | 37.89000, -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.