4/23/2015 — New Findings: Earthquake potential exists in areas where there is NO normal earthquake history

New findings from the University of Colorado indicate that earthquake potential exists in areas one might not normally expect.

Earthquake potential exists in areas such as, quote:

ancient mid-continent rifts that mark the scars of earlier tectonic boundaries, or old fault scarps worn down by hundreds or thousands of years of erosion.

In other words, earthquakes occurring along areas such as the edge of the Craton.

None of my viewers should be shocked by the results of these new University of Colorado studies.  We have indeed seen earthquakes progress along the edge of the plate, along earlier tectonic boundaries, and along old fault scarps worn down over time.

As seen in this below diagram from mid-April 2015 – the craton edge and areas NOT normally known for much earthquake movement are certainly showing activity.

craton april 17 2015a


Earthquake potential where there is no earthquake history

http://phys.org/news/2015-04-earthquake-potential-history.html

“It may seem unlikely that a large earthquake would take place hundreds of kilometers away from a tectonic plate boundary, in areas with low levels of strain on the crust from tectonic motion. But major earthquakes such as the Mw 7.9 2008 Chengdu quake in China and New Zealand’s 2011 Mw 6.3 quake have shown that large earthquakes do occur and can cause significant infrastructure damage and loss of life.
So what should seismologists look for if they want to identify where an earthquake might happen despite the absence of historical seismic activity?

Roger Bilham of the University of Colorado shows that some of these regions had underlying features that could have been used to identify that the region was not as “aseismic” as previously thought. Some of these warning signs include debris deposits from past tsunamis or landslides, ancient mid-continent rifts that mark the scars of earlier tectonic boundaries, or old fault scarps worn down by hundreds or thousands of years of erosion.

Earth’s populated area where there is no written history makes for an enormous “search grid” for earthquakes. For example, the Caribbean coast of northern Colombia resembles a classic subduction zone with the potential for tsunamigenic M>8 earthquakes at millennial time scales, but the absence of a large since 1492 is cause for complacency among local populations.

These areas are not only restricted to the Americas. Bilham notes that in many parts of Asia, where huge populations now reside and critical facilities exist or are planned, a similar historical silence exists. Parts of the Himalaya and central and western India that have not had any in more than 500 years could experience shaking at levels and durations that are unprecedented in their written histories.

Bilham will present his research on April 22 at the annual meeting of the Seismological Society of America (SSA) in Pasadena, Calif.”


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