Jump to content

Ballenas Fault

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Dawnseeker2000 (talk | contribs) at 16:13, 13 March 2020 (Reverted 1 edit by 66.172.185.2 (talk) to last revision by WallabyWombat (TW)). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

The Ballenas Fault is a transform fault located on the seabed of the Gulf of California, extending through the Canal de Ballenas which separates the Isla Ángel de la Guarda from the Baja California Peninsula. The fault is an integral part of the East Pacific Rise, linking the Delfin Basin in the north with a smaller spreading center to the south. The fault is considered the northernmost member of a grouping of four transform faults called the Guaymas Transform Fault System.

The Ballenas Fault produced a magnitude 6.9 earthquake on August 3, 2009.

References

  • Malservisi, R.; Plattner, C.; Hackl, M.; Gonzalez-Garcia, J. J.; Suarez Vidal, F.; Amelung, F.; Dixon, T. H. (2009). Earthquake cycle on the Ballenas Fault, Central Gulf of California, MX. American Geophysical Union (AGU) Fall Meeting 2009. Bibcode:2009AGUFM.G23B0689M.