Hydrohistorian
Denver Basin bedrock
Confined sandstone aquifer; negligible human-timescale recharge — pumping is one-way storage mining.
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
14 measurements from 2003-01-08 to 2005-04-09. Most recent water-level elevation 6755.2 ft, 61.8 ft below ground.
Over the record the level is insufficient data . 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, 2003-01-08 to 2005-04-09, 14 measurements. The record is insufficient data (p equals None), measured on water-level elevation. Rising elevation means more water. The values are downloadable as CSV from the link above.
The well itself
| Aquifer | DAWSON |
|---|---|
| Total depth | 110.0 ft |
| Perforated interval | 60.0–110.0 ft |
| Ground elevation | 6817.0 ft |
| Permit | 37503 |
| Location | 39.04000, -104.83000 |
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.