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briefing navy
USGS provides briefing to Navy about Ridgecrest Earthquake Sequence
USGS provides briefing to Navy about Ridgecrest Earthquake Sequence
USGS provides briefing to Navy about Ridgecrest Earthquake Sequence

Kate Scharer (USGS) provides CO CAPT Paul Dale (Navy) with the field mapping team’s initial product, showing the surface fault rupture at NAWSCL as well as the temporarily deployed seismic and GPS sensors that were rapidly deployed. Contributions of field data from within the base were from CGS & USGS, and from outside the base were from Univ.

Kate Scharer (USGS) provides CO CAPT Paul Dale (Navy) with the field mapping team’s initial product, showing the surface fault rupture at NAWSCL as well as the temporarily deployed seismic and GPS sensors that were rapidly deployed. Contributions of field data from within the base were from CGS & USGS, and from outside the base were from Univ.

Portable Seismic Station
Portable Seismic Station
Portable Seismic Station
Portable Seismic Station

Two portable sensors: a strong motion sensor (to record strong shaking that can be felt) and a broadband sensor (to record weak motion for detecting small earthquakes) buried into the ground to detect earthquakes. These stations can be quickly deployed and send real-time data back to the USGS via cellular telemetry immediately after they are installed. 

Two portable sensors: a strong motion sensor (to record strong shaking that can be felt) and a broadband sensor (to record weak motion for detecting small earthquakes) buried into the ground to detect earthquakes. These stations can be quickly deployed and send real-time data back to the USGS via cellular telemetry immediately after they are installed. 

briefing navy
USGS provides briefing to Navy about Ridgecrest Earthquake Sequence
USGS provides briefing to Navy about Ridgecrest Earthquake Sequence
USGS provides briefing to Navy about Ridgecrest Earthquake Sequence

Kate Scharer (USGS) provides CO CAPT Paul Dale (Navy) with the field mapping team’s initial product, showing the surface fault rupture at NAWSCL as well as the temporarily deployed seismic and GPS sensors that were rapidly deployed. Contributions of field data from within the base were from CGS & USGS, and from outside the base were from Univ.

Kate Scharer (USGS) provides CO CAPT Paul Dale (Navy) with the field mapping team’s initial product, showing the surface fault rupture at NAWSCL as well as the temporarily deployed seismic and GPS sensors that were rapidly deployed. Contributions of field data from within the base were from CGS & USGS, and from outside the base were from Univ.

rupture
Northern end of rupture resulting from the M7.1 Searles Valley quake
Northern end of rupture resulting from the M7.1 Searles Valley quake
Northern end of rupture resulting from the M7.1 Searles Valley quake

Fault rupture crosses dirt road, with California Geologial Survey vehicles for scale. Displacement at this location is primarily normal (vertical). Photograph taken near the northern end of the rupture resulting from the M7.1 Searles Valley earthquake.

Fault rupture crosses dirt road, with California Geologial Survey vehicles for scale. Displacement at this location is primarily normal (vertical). Photograph taken near the northern end of the rupture resulting from the M7.1 Searles Valley earthquake.

Surface faulting
Surface faulting from the M7.1 Searles Valley earthquake
Surface faulting from the M7.1 Searles Valley earthquake
Surface faulting from the M7.1 Searles Valley earthquake

Oblique photograph showing surface faulting from the M7.1 Searles Valley earthquake. The dirt track (center) is right-laterally offset approximately 2.5 m (~8 ft).

Measure surface displacement from Searles Valley quake #2
Measure surface displacement from Searles Valley quake #2
Measure surface displacement from Searles Valley quake #2

USGS Research Geologists Christopher DuRoss measures surface displacement resulting from the M7.1 Searles Valley earthquake.

lidar truck
Scanning surface rupture from Searles Valley earthquake
Scanning surface rupture from Searles Valley earthquake
Scanning surface rupture from Searles Valley earthquake

 

USGS Earthquake Science Center Mobile Laser Scanning truck operated by Ben Brooks and Todd Ericksen scanning the surface rupture near the zone of maximum surface displacement of the M7.1 Searles Valley earthquake.

 

USGS Earthquake Science Center Mobile Laser Scanning truck operated by Ben Brooks and Todd Ericksen scanning the surface rupture near the zone of maximum surface displacement of the M7.1 Searles Valley earthquake.

fault scarp
Inspecting the Vertical Offset Fault Scarp
Inspecting the Vertical Offset Fault Scarp
Inspecting the Vertical Offset Fault Scarp

Scientists from USGS & California Geological Survey viewing vertical fault offset of ~12 +/- 3 foot high fault scarp near the expected maximum slip locality along the primary tectonic rupture associated with the M 7.1 event.

Scientists from USGS & California Geological Survey viewing vertical fault offset of ~12 +/- 3 foot high fault scarp near the expected maximum slip locality along the primary tectonic rupture associated with the M 7.1 event.

surface displacement
Measure surface displacement from Searles Valley quake #1
Measure surface displacement from Searles Valley quake #1
Measure surface displacement from Searles Valley quake #1

USGS Research Geologists Christopher DuRoss and Jessica Thompson Jobe examine rupture resulting from the M7.1 Searles Valley earthquake.

access road offset
Helicopter Overflight Viewing Access Road Fault Offset
Helicopter Overflight Viewing Access Road Fault Offset
Helicopter Overflight Viewing Access Road Fault Offset

California Geological Survey and USGS geologists and geophysicists with National Guard and Navy personnel view road damage from 3 to 5 feet of right-lateral motion near the expected maximum slip locality along the primary tectonic rupture associated with the M 7.1 event.

California Geological Survey and USGS geologists and geophysicists with National Guard and Navy personnel view road damage from 3 to 5 feet of right-lateral motion near the expected maximum slip locality along the primary tectonic rupture associated with the M 7.1 event.

fault rupture
Searles Valley Earthquake field photo #7
Searles Valley Earthquake field photo #7
Searles Valley Earthquake field photo #7

USGS geologist Josie Nevitt and geodesist Todd Ericksen collect a sample from the fault zone of the main rupture.

fault rupture
Searles Valley Earthquake field photo #8
Searles Valley Earthquake field photo #8
fault rupture
Searles Valley Earthquake field photo #6
Searles Valley Earthquake field photo #6
Searles Valley Earthquake field photo #6

Aerial view shot from Blackhawk helicopter overflight on July 6 of the zone of high surface displacement.

fault rupture
Searles Valley Earthquake field photo #1
Searles Valley Earthquake field photo #1
Searles Valley Earthquake field photo #1

USGS Geologists Beth Haddon and Josie Nevitt measure fault displacement along the principal rupture.

fault rupture
Searles Valley Earthquake field photo #3
Searles Valley Earthquake field photo #3
fault rupture
Searles Valley Earthquake field photo #5
Searles Valley Earthquake field photo #5
Searles Valley Earthquake field photo #5

USGS geophysicist Ken Hudnut demonstrating Drop Cover and Hold Technique during the foreshock sequence to the M7.1 Searles Valley earthquake.

Image shows a road with damage from an earthquake
Damage to Access Road from Searles Valley Earthquake
Damage to Access Road from Searles Valley Earthquake
Damage to Access Road from Searles Valley Earthquake

Fault scarp at offset access road site. Center line has been offset up and to the right as one looks across the fault towards the east.

Image shows a road with cracks from an earthquake at night
Highway 178 SW of Trona
Highway 178 SW of Trona
Highway 178 SW of Trona

California State Route 178 SW of Trona, following the M7.1 earthquake. Road is now closed for repairs. 

California State Route 178 SW of Trona, following the M7.1 earthquake. Road is now closed for repairs. 

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