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Geological Formation

Santa Clara Valley

Structural and Tectonic Formations

The Santa Clara Valley is a geologic trough in Northern California that runs about 90 miles south-southeast from San Francisco Bay to Hollister, roughly 93 miles long and 15 miles wide. It is a graben, a tectonic depression, lying between the San Andreas Fault to the west and the Hayward and Calaveras faults to the east, bounded by the Santa Cruz Mountains on the west and the Diablo Range on the east, and its floor is an alluvial plain built up within that structural depression rather than an erosional feature. The valley spans San Mateo, Santa Clara, Alameda and San Benito counties and has a Mediterranean semi-arid climate; once known as the Valley of Heart's Delight for its orchards, it became the technology center Silicon Valley beginning in the 1960s. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Santa Clara Valley

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Santa Clara Valley
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Santa Clara Valley
Sources
Santa Clara Valley (Wikipedia)
Lead section
Quote, Lead section
The Santa Clara Valley (Spanish: Valle de Santa Clara) is a geologic trough in Northern California that extends 90 miles (140 km) south-southeast from San Francisco to Hollister.
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Wikidata: Santa Clara Valley
Wikidata Q1739060, class allow-list match (w-wdresolver-0926)View the Source
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