4.8 Article

Near-Field Deformation from the El Mayor-Cucapah Earthquake Revealed by Differential LIDAR

Journal

SCIENCE
Volume 335, Issue 6069, Pages 702-705

Publisher

AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.1213778

Keywords

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Funding

  1. NSF RAPID [EAR-1039168, 1039147]
  2. NSF [EAR-0106924]
  3. U.S. Geological Survey [02HQAG0008]
  4. Consejo Nacional de Ciencia y Tecnologia [CB-2007-81463]
  5. NASA's Earth Surface and Interior Focus Area
  6. Division Of Earth Sciences
  7. Directorate For Geosciences [1043051, 1039147] Funding Source: National Science Foundation
  8. Office of Advanced Cyberinfrastructure (OAC)
  9. Direct For Computer & Info Scie & Enginr [0753407] Funding Source: National Science Foundation

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Large [moment magnitude (M-w) >= 7] continental earthquakes often generate complex, multifault ruptures linked by enigmatic zones of distributed deformation. Here, we report the collection and results of a high-resolution (>= nine returns per square meter) airborne light detection and ranging (LIDAR) topographic survey of the 2010 M-w 7.2 El Mayor-Cucapah earthquake that produced a 120-kilometer-long multifault rupture through northernmost Baja California, Mexico. This differential LIDAR survey completely captures an earthquake surface rupture in a sparsely vegetated region with pre-earthquake lower-resolution (5-meter-pixel) LIDAR data. The postevent survey reveals numerous surface ruptures, including previously undocumented blind faults within thick sediments of the Colorado River delta. Differential elevation changes show distributed, kilometer-scale bending strains as large as similar to 10(3) microstrains in response to slip along discontinuous faults cutting crystalline bedrock of the Sierra Cucapah.

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