ShakeMaps provide near-real-time maps of ground motion and shaking intensity following significant earthquakes. This report overviews the hazard characteristics of the July 4 and 5, 2019 Ridgecrest, California M 6.4 and M 7.1 earthquakes, the regulatory context and emergency response, the impacts of these earthquakes, and current conditions by collocating publicly-reported information. In the Ridgecrest area these include a Seismicity in Indian Wells Valley has been characterized by swarms of thousands of earthquakes, some lasting for more than a year.More distant earthquakes provide more warning, but are less damaging, than local earthquakes.The ECSZ was originally limited to the area south of the Garlock Fault, which separates distinctly different modes of deformation, but now is considered to extend into Walker Lane. Relatively minor damage resulted from the initial foreshock, though some building fires were reported in Ridgecrest near the A significant series of additional earthquakes followed the foreshock, with the majority of magnitudes ranging approximately 2–4 MThousands more aftershocks occurred following the 7.1 MStructural damage and two building fires—one of which destroyed half of a home—occurred in Ridgecrest.Several fires broke out and five injuries were reported after the mainshock hit, most of them in Ridgecrest and Trona.Overall damage is estimated in excess of $5.3 billion.In addition, Dr. Lucy Jones said that the odds of another 7 MMany residents of Los Angeles County were not pleased when the ShakeAlertLA app on their cellphones did not alert them to either of the Ridgecrest earthquakes, which many people assumed to be failure.At the time of the Ridgecrest earthquakes the threshold for issuing an alert was an expected shaking intensity in Los Angeles County of 4 (IV) on the According to the City of Los Angeles's Twitter account, the threshold will be lowered after this event.The broad context of the Ridgecrest earthquakes is the The ECSZ extends north along the east front of the Along the eastern front of the Sierra Nevada strike-slip faulting happens on the Owens Valley Fault (OVF), part of which ruptured in the East of Rose Valley, between the nearly parallel ends of the Owens Valley and Little Lake faults, lies the Coso Range and The easterly striking left-slip Garlock Fault south of Ridgecrest is one of California's longest active faults, and marks the boundary between different styles of tectonic deformation.Geodetic measurements show that the slip-rate of Garlock Fault is currently less than half of its estimated long-term geological rate.The Scodie Lineament is a zone of microseismicity extending southwest (paralleling the Garlock Fault) from near Walker Pass (due west of Ridgecrest) to align with the White Wolf Fault, scene of the 1952 Kern County earthquake south of Bakersfield.
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