M 8.0 - 75km SSE of Lagunas, Peru

  • 2019-05-26 07:41:14 (UTC)
  • 5.796°S 75.298°W
  • 109.9 km depth
  • Felt Report - Tell Us!
    0
    0
    1
    5
    8
    5
    Responses

    Contribute to citizen science. Please tell us about your experience.

    Citizen Scientist Contributions
  • ShakeMapVIIImmi
    ShakeMap Intensity Thumbnail
    Estimated Intensity Map
    Contributed by US 4
  • PAGERORANGE
    Economic Alert Histogram
    Estimated Economic Losses
    Fatality Alert Histogram
    Estimated Fatalities
    Contributed by US 4
  • Ground Failure
    Landslides

    Limited area affected

    Little or no population exposed

    Liquefaction

    Extensive area affected

    Significant population exposed

    Contributed by US 4
  • Origin
    Review Status
    REVIEWED
    Magnitude
    8.0 mww
    Depth
    109.9 km
    Time
    2019-05-26 07:41:14 UTC
    Contributed by US 4
  • Finite Fault
    Cross-section of slip distribution
    Cross-section of slip distribution.
    Contributed by US 4

Tectonic Summary

The May 26, 2019, M 8.0 northern Peru earthquake occurred as the result of normal faulting at an intermediate depth, approximately 110 km beneath the Earth's surface within the subducted lithosphere of the Nazca plate. Focal mechanism solutions indicate that rupture occurred on either a north- or south-striking, moderately dipping normal fault. At the location of the earthquake, the Nazca plate moves to the east relative to the South America plate at a velocity of about 70 mm/yr, subducting at the Peru-Chile Trench, to the west of the Peruvian coast and the May 26th earthquake. Earthquakes of northern Peru and most of western South America are due to strains generated by this ongoing subduction; at this latitude, the Nazca plate is seismically active to depths of about 650 km. This earthquake occurred in a segment of the subducted plate that has produced frequent earthquakes with focal depths of 100 to 150 km.

Earthquakes like this event, with focal depths between 70 and 300 km, are commonly termed “intermediate-depth” earthquakes. Intermediate-depth earthquakes represent deformation within subducted slabs rather than at the shallow plate interface between subducting and overriding tectonic plates. They typically cause less damage on the ground surface above their foci than is the case with similar-magnitude shallow-focus earthquakes, but large intermediate-depth earthquakes may be felt at great distance from their epicenters.

While commonly plotted as points on maps, earthquakes of this size are more appropriately described as slip over a larger fault area. Normal events of the size of the May 26, 2019 M 8.0 earthquake are typically about 180x50 km (length x width).

Large intermediate-depth earthquakes are reasonably common in this section of the Nazca slab, and three other intermediate-depth M 7+ events have occurred within 250 km of the September 26th earthquake over the past three decades. A M 7.5 earthquake in September 2005, located at a similar depth but approximately 130 km to the west of the May 26th, 2019 earthquake, caused 5 deaths, about 70 injuries, and significant damage in the surrounding region.

For More Information