Farallon Trench
id:
farallon-trench-250-7944366
title:
Farallon Trench
text:
The Farallon Trench was a subduction related tectonic formation located off the coast of the western California continental margin during the late to mid Cenozoic era, around 50 miles southeast of modern-day Monterey Bay. The time duration of subduction began from around 165 Ma when the Farallon Plate replaced the Mezcalera promontory, until the San Andreas Fault straightening around 35 Ma. As data accumulated over time, a common view developed that one large oceanic plate, the Farallon Plate, a
brand slug:
wiki
category slug:
encyclopedia
description:
Tectonic formation of the Cenozoic era
original url:
https://en.wikipedia.org/wiki/Farallon_Trench
date created:
date modified:
2023-11-29T10:54:16Z
main entity:
{"identifier":"Q5434800","url":"https://www.wikidata.org/entity/Q5434800"}
image:
fields total:
13
integrity:
14