Water level measurements in 52 shallow boreholes in the San Francisco Bay region
Water-level measurements have been read in 52 cased boreholes in the San Francisco bay region. These measurements are compared to water-table depths determined by P-wave velocity. A velocity in excess of 1200 m/s is taken as the depth of the upper surface of the water table. This method works best in saturated alluvium, and fails in dry rock because of P-wave velocities greater than 1200 m/s.
Citation Information
| Publication Year | 1978 |
|---|---|
| Title | Water level measurements in 52 shallow boreholes in the San Francisco Bay region |
| DOI | 10.3133/ofr78935 |
| Authors | Edward Roth |
| Publication Type | Report |
| Publication Subtype | USGS Numbered Series |
| Series Title | Open-File Report |
| Series Number | 78-935 |
| Index ID | ofr78935 |
| Record Source | USGS Publications Warehouse |