Geology and ground water in north-central Santa Cruz County, California
Water-Resources Investigations Report
80-26
By: Michael J. Johnson
Links
- Document: Report (pdf)
- Download citation as: RIS | Dublin Core
Abstract
North-central Santa Cruz County is underlain mainly by folded sedimentary rocks of Tertiary and Cretaceous age that have been highly fractured by movements in the San Andreas fault system. Ground water is stored in fractures within shale and mudstone formations and in intergranular pore spaces within fine- to very fine-grained sandstone and siltstone formations. Fewer than 10% of the wells yield more than 15 gallons of water per minute. The water in most wells is moderately hard to very hard, is generally of a sodium bicarbonate or calcium bicarbonate type, and commonly has excessive concentrations of iron or manganese. Of the many geologic units in the study area, only the Purisima Formation of Pliocene age has the potential to sustain well yields greater than 100 gallons per minute. (USGS)
Suggested Citation
Johnson, M.J., 1980, Geology and ground water in north-central Santa Cruz County, California: U.S. Geological Survey Water-Resources Investigations Report 80-26, iv, 33 p. , https://doi.org/10.3133/wri8026.
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Geology and ground water in north-central Santa Cruz County, California |
| Series title | Water-Resources Investigations Report |
| Series number | 80-26 |
| DOI | 10.3133/wri8026 |
| Year Published | 1980 |
| Language | English |
| Publisher | U.S. Geological Survey |
| Publisher location | Reston, VA |
| Description | iv, 33 p. |
| Country | United States |
| State | California |
| County | Santa Cruz County |