| Well Information Table |
|---|
| Common Well ID | NA03901227ADD |
| USGS Well ID | 373512105383501 |
| USGS Station Name | NA03901227ADD |
| USGS Construction Date | 01/01/1967 |
| USGS Site Type | Well |
| USGS Site Use Information | Observation |
| USGS Groundwater Use Information | Unused |
| Data Source(s) | USGS |
| Location Data |
|---|
| TRS | NA03901227ADD |
| USGS TRS 1 | NA03901227ADD |
| USGS TRS | SESENES027T0039NR0012EN |
| Longitude/Latitude (NAD83) | -105.64362680 , 37.58667027 |
| Longitude/Latitude Data Source | GWSI decimal LAT/LONG field |
| USGS Longitude/Latitude (NAD83) | -105.6436268 , 37.58667027 |
| Easting, Northing RGDSS-NAD83 (US ft) | 208823.20 , 215060.27 |
| USGS Topography | Valley flat |
| USGS County | Alamosa County |
| Elevation and Depth Data |
|---|
| Ground Elevation (ft NAVD88) | 7565.17000000000 |
| Elevation Data Source | USGS GWSI database |
| USGS Ground Elevation (ft NGVD29) | 7561.00 |
| 1/3-Arc Second NED Ground Elevation (ft NAVD88) | 7555.07 |
| 1-Arc Second NED Ground Elevation (ft NAVD88) | 7554.82 |
| SRTM Ground Elevation (ft NAVD88) | 7558.78 |
| Total Depth (ft) | 17.00 |
| USGS Well Depth (ft) | 17.00 |
| Model Layer | 1 |
| Model Layer Source | Well Depth |
| Depth of Bottom of Layer 1 | 115 |
| Depth of Bottom of Layer 2 | 488 |
| Depth of Bottom of Layer 3 | 992 |
| Depth of Bottom of Layer 4 | 2596 |
| Additional Well Information | Geohydrology, Construction |
| Aquifer Information |
|---|
| Aquifer Type | Unconfined |
| Aquifer Type Source | TD Elevation/Model Layer |
| USGS Primary Aquifer | Cenozoic Erathem |
| USGS Hydrologic Unit | San Luis |
| USGS Data Available | Water-level (GW.LEV) |
| Water-level Database Information |
|---|
| Water-level Count | 19 |
| Water-level Date Range | 10/04/1967 thru 05/23/1984 |
| Monitored within the last 18 months | No, most recently on 05/23/1984 |
| Depth-to-Water Range (ft) | 3.23 to 4.61 |
| Water Table Elevation Range (ft NAVD88) | 7560.56 to 7561.94 |
| Water-Level-Source:Number-of-Measurements | USGS:19 |
