Type igneous, metamorphic Country United States Underlies Franciscan Assemblage | Overlies basement Named for California Coast Ranges Parent range California Coast Ranges | |
Region California Coast Ranges Primary Basalt, Gabbro, Peridotite, Schist | ||
Serpentinization chemistry and life at the coast range ophiolite microbial observatory
The Coast Range Ophiolite is an ophiolite of Middle to Late Jurassic age located in the California Coast Ranges. They form the basement of the extreme western margin of central and northern California. Exposures straddle the coast from Santa Barbara County up to San Francisco. The formation then trends inland up to the southern end of the Klamath Mountains.
Contents
- Serpentinization chemistry and life at the coast range ophiolite microbial observatory
- Description
- Distribution
- Origin and Tectonics
- References
It is arguably the most extensive ophiolite terrane in the United States, and is one of the most studied ophiolites in the North America.
Description
As indicated by the name, the ophiolite is defined by the presence of ultramafic rocks in the California Coast Ranges. Pillow lavas and oceanic basalts are among the most common rocks found within the formation. There are a number of exposures that straddle the Mohorovičić discontinuity. Metamorphosed peridotite, in the form of a serpentine rock, is an indicator of the formation.
Distribution
In general, the ophiolite is exposed near the boundary between the sequences of rocks associated with the Coast Ranges, and rocks associated with the Great Valley Sequence. Where it is exposed, it generally underlies the various sedimentary rocks of the Great Valley Sequence, and may be coextensive with the contemporaneous (but slightly younger on average) Franciscan Assemblage, as would be expected by an observational application of the law of superposition. However, in many localities, the ultramafic rocks of the ophiolite can be found intruding or on top of the local country rock.
Origin and Tectonics
The Coast Range Ophiolite is characterized by obduction of oceanic crust onto land. Most of the rocks in the ophiolite were part of an accretionary wedge on the continental margin of Laurasia that was thrust onto land during the Jurassic through the influence of subduction. The exact origins of the rocks found in the ophiolite are a matter of debate; some geologists hypothesize that the rock primarily consist of mid-ocean lithosphere, while others assert different ideas related to island arc terranes associated with the Nevadan orogeny.