Photograph taken during a Land Cover Trends Project field trip in California of a valley with residential housing.
Why are there no faults in the Great Valley of central California?
The Great Valley is a basin, initially forming ~100 million years ago as a low area between the subducting ocean plate on the west (diving down under the North American plate) and the volcanoes to the east (now the Sierra Nevada mountains). Since its formation, the Great Valley has continued to be low in elevation. Starting about 20 million years ago the tectonics changed in California and instead of the ocean plate diving down under the North American plate, it began to slide along it, with the ocean plate moving northward. This movement occurs along the San Andreas fault and the many other faults that are roughly parallel to it.
The faults on the east side of the Great Valley, mostly in Nevada, are the result of the North American plate pulling apart there, in a different tectonic setting that results in the linear mountain ranges and long valleys you can see there. The faults just to the east of the Great Valley are mostly old faults and may or may not still be active today. So there is movement of faults in two separate regimes: sideways motion along the San Andreas system to the west-southwest, and pull apart motion along the faults mostly in Nevada to the east-northeast of Sacramento.
Related
What is a fault and what are the different types?
What is the relationship between faults and earthquakes? What happens to a fault when an earthquake occurs?
What is a "Quaternary" fault?
Where can I find a fault map of the United States? Is one available in GIS format?
How do I find fault or hazard maps for California?
Why are there so many earthquakes and faults in the Western United States?
Why are there so many faults in the Quaternary Faults Database with the same name?

Photograph taken during a Land Cover Trends Project field trip in California of a valley with residential housing.
An agriculture field in California taken during field work for the Trends Lancover Change project.
An agriculture field in California taken during field work for the Trends Lancover Change project.

Irrigation systems in Central California Valley Ecoregion: Single-field irrigation ditch.
Irrigation systems in Central California Valley Ecoregion: Single-field irrigation ditch.
Summary of Creepmeter Data from 1980 to 2020—Measurements Spanning the Hayward, Calaveras, and San Andreas Faults in Northern and Central California
UCERF3: A new earthquake forecast for California's complex fault system
Triggering of repeating earthquakes in central California
Where's the San Andreas fault? A guidebook to tracing the fault on public lands in the San Francisco Bay region
Quaternary fault and fold database of the United States
USGS National Seismic Hazard Maps
Related
What is a fault and what are the different types?
What is the relationship between faults and earthquakes? What happens to a fault when an earthquake occurs?
What is a "Quaternary" fault?
Where can I find a fault map of the United States? Is one available in GIS format?
How do I find fault or hazard maps for California?
Why are there so many earthquakes and faults in the Western United States?
Why are there so many faults in the Quaternary Faults Database with the same name?

Photograph taken during a Land Cover Trends Project field trip in California of a valley with residential housing.
Photograph taken during a Land Cover Trends Project field trip in California of a valley with residential housing.
An agriculture field in California taken during field work for the Trends Lancover Change project.
An agriculture field in California taken during field work for the Trends Lancover Change project.

Irrigation systems in Central California Valley Ecoregion: Single-field irrigation ditch.
Irrigation systems in Central California Valley Ecoregion: Single-field irrigation ditch.