To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

San Gregorio Fault

From Wikipedia, the free encyclopedia

U.S. Geological Survey map showing the trace of the San Gregorio Fault in yellow, lower center.

The San Gregorio Fault is an active, 209 km (130 mi) long fault located off the coast of Northern California. The southern end of the fault is in the Pacific Ocean just south of Monterey Bay, and the northern end is about 20 km northwest of San Francisco, near Bolinas Bay, where the San Gregorio intersects the San Andreas Fault. Most of the San Gregorio fault trace is located offshore beneath the waters of Monterey Bay, Half Moon Bay, and the Pacific Ocean, though it cuts across land near Point Año Nuevo and Pillar Point. The San Gregorio Fault is part of a system of coastal faults which run roughly parallel to the San Andreas.[1]

The movement of the San Gregorio is right-lateral strike-slip, and the slip rate is estimated to be 4–10 mm/year (0.2–0.4 inch/year). The most recent major earthquake along the fault had an estimated magnitude of 7 to 7.25 and occurred after 1270 AD—the earliest calibrated radiocarbon date for a native Californian cooking hearth at the Seal Cove site near Moss Beach that shows signs of displacement—but before 1775, when Spanish missionaries arrived in northern California and recorded history began for the region.[2]

Portions of the fault that come ashore near the cliffs between Pillar Point and Moss Beach are sometimes referred to as "Seal Cove Fault" in the geological literature.[2]

YouTube Encyclopedic

  • 1/3
    Views:
    762
    2 394
    18 233
  • The San Andreas Fault (1974) American Geological Institute
  • 7 Strike-Slip and Transform Faults
  • Is the Monterey San Gregorio Earthquake a Forshock for a M8.5 San Francisco Earthquake?

Transcription

References

  1. ^ Brown, Jr., R. D. (1990). "Quaternary deformation". The San Andreas Fault System, California – USGS Professional Paper 1515. United States Geological Survey. p. 89. ISBN 978-0607716269.
  2. ^ a b Simpson, Gary D.; Thompson, Stephen C.; Noller, J. Stratton; Lettis, William R. (October 1997). "The Northern San Gregorio Fault Zone: Evidence for the Timing of Late Holocene Earthquakes near Seal Cove, California". Bulletin of the Seismological Society of America. 87 (5): 1158–1170. Bibcode:1997BuSSA..87.1158S. doi:10.1785/BSSA0870051158. S2CID 55708626. Retrieved 18 September 2018.
This page was last edited on 29 January 2024, at 08:54
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.