 A map indicating the locations of shocks and aftershocks, Indian Wells, China Lake and Ridgecrest are close together and marked in the lower center of the map. The Little Lake Fault Line is northeast of Ridgecrest, running northwest to southeast. The clustered shocks run along the Fault Line and southwest, forming an upside-down V-shape. The 6.4 quake occurred near the corner of the V. Hello, my name is Jeremy Lancaster, I'm a supervising engineering geologist with the Department of Conservation and California Geological Survey. And I'm showing a map here on screen of the Ridgecrest area, and particularly an earthquake event occurred in Ridgecrest, in the Ridgecrest area on July 4th at around 10.35 in the morning. That earthquake occurred about right in this area, the magnitude 6.4. We thought that was the main shock. You can see the aftershock sequence migrated to the north and to the south a little bit on what we call the Little Lake Fault Zone, and then we also had an aftershock sequence migrate to the southwest on an unknown fault zone. There was some damage in the town of Ridgecrest, and a little bit in the town of Toronto, but generally this is a low populated or has low population density. Real views of Ridgecrest and Toronto. Subsequent to that, we had a magnitude 7.1 earthquake occur yesterday, July 5th at around 8.19 in the evening. And that earthquake produced a major aftershock sequence and surface rupturing event on the Little Lake Fault, which I'll show you on the next map. Another linear cluster extends farther northwest along the fault line from the markings of the 6.4 quake. So you can see here is the epicenter of that magnitude 7.1 earthquake and that aftershock sequence migrating up near the coastal volcanic field. So that sequence extended about 20 miles. So what we thought was the original earthquake event was now superseded by this magnitude 7.1. So the 6.4 is now what we call a foreshock, and the 7.1 is the main event. That aftershock sequence is migrated down to the southeast towards the Garlock Fault, which is the second longest fault in California. And we're just lucky that this area isn't highly populated except for the town of Ridgecrest. We have major arterial routes through here. Highway 178 extends into the Trona Valley. Highway 395 extends all the way up into the Mammoth Lakes area. So we have about nine geoprofessionals in the field mapping the surface rupture and the deformational patterns as well as documenting damages and there will be more posted on conservation.ca.gov. Thank you.